environmentclearance.nic.inenvironmentclearance.nic.in/writereaddata/Online/TOR/25_May_2018... · List of Figures Figure 1: Geology and mineral resources of Kannur. Figure 2: Geomorphology

List of Figures

Figure 1: Geology and mineral resources of Kannur.

Figure 2: Geomorphology of Kannur.

Figure 3: Landuse of Kannur.

Figure 4: Geohydrology of Kannur.

Figure 5: Geotechnical and natural hazards map of Kannur.

List of Tables

Table1: Details of revenue collection for the period 2013- - -

Table 2a: Details of Quarrying Permits granted for Granite building stone in Kannur

district

Table 2b: Details of Quarrying Permits granted for Laterite building stone in Kannur

district

Kannur (Cannanore) district is one of the northern maritime districts of Kerala. It covers

an area of 2966 sq km bounded by the North latitudes 110 0

longitudes 740 0

Kozhikode district in the south, Coorg district of Karnataka and Wayanad district in the east and the Lakshadweep Sea in the west. The Census data for the year 2011 reveals that the district has total population of 2525637 persons with 1184012 males and

Kannur district has an area of 2997 sq. kms. It is bounded by Lakshadweep sea to the

west and Karnataka state to the east. To the north of it lies Kasargod district, while to

the south is Kozhikode district and also Mahe which comes under the Pondicherry

administration. The terrain is rugged and slopes west from Western Ghats to the coast.

Kannur district is divided into 3 taluks (Taliparambu, Kannur and Thalassery), 5

municipalities (Payyanur, Taliparambu, Kannur, Azhikode and Koothuparambu), 9

blocks (Payyanur, Kannur, Thalasserry, Taliparambu, Edakkad, Irikkur, Iritty, Peravur

and Koothuparambu), 81 panchayats and 129 villages.

Kannur district is mainly drained by the Valapattanam and Anjarakandy rivers. The

other rivers are Kuppam, Mahe, Thalasserry etc. Dendritic is the common drainage

pattern. The Valapattanam river, which is the longest in the district originates from

Brahmagiri Reserve forest in Coorg district of Karnataka. The drainage area of the river

in Kerala is 1321 sq.km. The Anjarakandy river originates from the Kannoth Reserve

forest. The drainage area of the river is 412 sq.km.

Kannur district has 23,312 ha. area under irrigation, which accounts about 8.01% of the

gross irrigated area of the state. Kannur district is provided with one major irrigation

project along with some minor irrigation projects. The major irrigation scheme of the

district is Pazhassi project. The command area fixed for Pazhassi project was 11525 ha

of land. However only 8125 ha of land has been benefited through this project as on

date. Ground water is also used for irrigation purposes. In addition to this, there are

private tanks to facilitate the irrigation sector.

Kannur district receives a total annual rainfall of around 3438 mm. District experiences

heavy rainfall during the South West monsoon season followed by North East monsoon.

South West monsoon during June to September contributes 70 % of

the total rainfall of the year. The northeast monsoon contributes only about 30%. The

year to year variability of annual rainfall is around 28.2%. In general, the rainfall

increases from the coast to the eastern hilly regions. Kannur district falls under wet type

Apart from the rainfall, the meteorological parameters play an important role in

groundwater balance estimation and other types of relevant studies.

The temperature is more during the months of April to May and is less during December and January. The average mean monthly maximum temperature ranges from 28.4 to

36.90C and minimum temperature ranges from 19.7 to 23.90C.

Relative humidity is more during south west monsoon season (ie June to September).

It is more during morning hours and is less during evening hours. Humidity ranges from

77 to 88 % in the district.

Evaporation is more during summer months of March to May and low during the

months of June to November. The mean evaporation ranges from 2.6 to 5.7 mm/day.

Generally good sunshine hours are recorded in the month of November to May. January

to March records the maximum sunshine hours of more than 9.1 hours/day. The months

of June to August records the minimum sunshine due to cloudy sky.

Wind speed ranges from 2.1 to 3.3 km per hour with mean speed of 2.6 km/hr. The

wind speed is high during the period from March to June and low during the period

from September to December.

The monthly PET ranges from 124.5 to 170.6 mm. PET values are lower than the

monthly rainfall during the months of May to October indicating water surplus for

possible recharge into groundwater regime during these months.

The district can be broadly divided into seven geological belts trending NW-SE viz., (i) northern belt of Charnockite group extending further north and east to the adjacent districts, (ii) north central belt of Wayanad schist complex, (iii) Central belt of Peninsular Gneissic Complex extending to the southeast, (iv) south central belt of Vengad Group, equivalent to Dharwars, (v) southernmost belt of Migmatite Complex which extends further south to the adjacent district, (vi) Sedimentary (Warkalli Beds) in the western part near the coast and (vii) Quaternary sediments along the coast. The lithology of Kannur district is grouped under Precambrian, late Tertiary and Quaternary periods and the Precambrian rocks dominate over the other two. Charnockite Group, includes pyroxene granulite, charnockite (hypersthene granulite) and hornblende-diopside granulite. While hornblende granite and charnockite occupy large areas, pyroxene granulite occurs as linear bodies in the southeast. Hornblende-biotite gneiss constitutes the litho unit of Migmatite Complex. It has a large areal extent along the coast, south of Kannur. Towards east and southeast, discrete metasedimentary and ultramafic sequences which have been designaed as Wayanad Schist Complex and are considered equivalent of Sargur Group of Karnataka. They occur as isolated bands within charnockite and gneiss. Their contacts are generally discordant due to later folding, metamorphism and migmatisation. The group comprises quartzite, magnetite quartzite, garnet-kyanite-sillimanite gneiss, quart-mica-kyanite schist, quartz-sericite schist, amphibolite, kyanite-sillimanite-sericite quartzite, metaultramafites. Garnet-kyanite-sillimanite gneiss/schist is widespread in the east, whereas the other members of Wayanad Complex occur as linear bands, lensoidal bodies and vestiges to the West Peninsular Gneisic Complex, represented by hornblende-biotite gneiss comprise of a complex suite of gneisses and granites, representing the anatectic phase of migmatisation of schist complex. East of Kannur extending upto Tellichery in the south, a large body of quartz-mica schist is separated from the other schistose rocks by a conglomerate horizon extending over 8km. This lithounit known as Vengad Formation, characterised by lack of migmatisation, presence of primary structres and absence of high grade minerals, is correlatable with rocks of Dharwar Super Group. Large bodies of anortjosite, gabbro, granite and granophyre from the post Vengad basic and acid intrusives. Dolerite dykes trending NW-SE represent the younger basic intrusives. Late Tertiary sedimentary rocks (Warkalli beds) occur as isolated patches along the coast near Kannur, Pazhayangadi and east of Payyannur. They comprise variegated clays and friable sandstone. At Kannur and Pazhayangadi, carbonaceous clay with thin seams of lignite is reported towards bottom of the sedimentary sequence. The Tertiaries as well as the basement rocks are extensively lateritised. The pebble bed, reported near Valapatnam along the bank of Valapatanam river, is considered to be of Quaternary age. Quaternary alluvial deposit occur along the coast and in the valleys. They constitute palaeo-marine deposit (Guruvayur Formation), fluvial deposit (Periyar Formation) of Valapatnam and Dharmadom rivers, fluvio-marine deposits (Viyyam Formation) and

beach deposits (Kadappuram Formation) (Figure 1). The geology of the district given

better understanding of geological succession and stratigraphic sequence.

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Based on physiography, the district can be divided into three distinct geomorphologic

units viz i) the coastal plains and lowlands in the western part, (ii) the central

undulatory terrain comprising the midland region and (iii) eastern highland region.

The coastal plains occurs as a narrow belt of alluvial depositional landforms running

parallel to the coast with a maximum width of about 15 km. It comprises narrow

beaches interrupted by cliffs, promontories and rocky beaches. Estuaries, lagoons,

tidal flats, fllodplain and palaeo-beach ridges are the other landforms of the area. The

region has a maximum height of 7m in the east. The midland region, a relatively wide

zone repreents denudational landforms exhibiting laterite capped flats, mesasm ridges,

spurs, laterite interfluves and narrow alleviated valleys. Midland region forms a

plateau land at certain places covered by a thick cover of laterite. Elevation of this

region displays remnants of planation surfaces as well. Two former planation surfaces

with fairly extensive remnants are characterised by laterite cappings. Vestiges of still

older surfaces are identifiable at higher altitudes. The hilly region in the east is a

structural cum denudational landform, Here the elevation is generally above 500m.

Hills have very steep slopes. Landforms of intrusive origin are also noticed

nearPeralimala and Ezhimala. The hilly tract in the eastern part consists of highly

rugged terrains. The Ezhimala peak with the characteristic N-S alignment is a distinct

physiographic unit in the coastal plains. Minor cliffs of laterite generally rising to an

elevation of 50 to 60 m above mean sea level are found at Mahe, Thalasserry and

Bekal coast. The midland region presents a plateau land covered by a thick cover of

laterite. This is immediately to the east of the coastal strip, rising from 40 to 100 m

above msl. The valleys in the plateau are gorge like and V shaped cut by youthful

streams. The hilly tract along the eastern part of the district constitutes the highland

region and is highly rugged. Development of bad land topography along the margins

of the valley is a common feature observed in the district (Figure 2).

There are mainly four types of soil observed in the district. (1) Lateritic soil

(2) Brown hydromorphic soil (3) Coastal and river alluvium (4) Forest Loamy soil (5) Lateritic soil The predominant soil in the district is lateritic soil, which is the

weathered product derived under humid tropical conditions. It occurs mainly in the

midland and hilly areas characterized by rugged topography. They range from sandy

loam to red loam. (6) Brown hydromorphic soil These are confined to the valleys between

undulating topography in the midlands and in the low lying areas of the coastal strip

in the district. These soils are brown in colour and the surface texture varies from

sandy loam to clay. They have been formed as a result of transportation and deposition

of materials from adjoining hill slopes and also through deposition by rivers. (3) Coastal and river alluvium The coastal alluvium is seen in the western coastal

tract of the district. The coastal plain is characterized by secondary soils, which are

sandy and sterile with poor water holding capacity. The width of the zone is more in

the central part i.e., in the Kannur area and it is almost narrow in both north and

southern areas of the district. The marshy soil in the coastal plain supports mangrove

vegetation and is found at the estuaries and backwater extending inland along their

courses. The soil is composed of recent deposits predominantly marine with some

fluvial sediments along the coastline. These soils are immature with high sand content.

River alluvium is found along river valleys cutting across the extensive lateritic soils.

The soil is very deep with surface texture ranging from sandy loam to clay. It is fertile,

having water holding capacity and plant nutrients which are regularly replenished

during floods. (7) Forest Loamy soil These soils are found in the eastern hilly areas of the district

and are characterised by a surface layer rich in organic matter. They are generally

acidic and are dark reddish brown to black in colour with loam to silty loam texture

(Figure 5).

On the basis of landuse the district is dividedinto three units arable, forest land and waste land. Major part of the district is arable land which includes irrigated and

unirrigated land. Forest is mostly in the east, within which some areas are developed as rubber and cashew plantations. Extensive waste land formed of hard laterite, unsuitable for cultivation lies in the midland region. Most of the area is covered by lateritic soil. Forest loam soil occurs in the east and the alluvial soil is along the coast (Figure 3). The area under forest in given in the forest map given below.

The area lies in the high rainfall area of the western coast. The district is divisible into four geohydrological provinces from coast to the east based on the yield of groundwater. The coastal alluvium in the west has fairly good yield with depth to water table from 0.5 to 3m. In the laterite capped midland region, open dug wells are suitable where depth to groundwater is between 5 and 20m. Further east, the area is covered by weathered rock and lateritic soil. Here the valleys and lowlands have good yield of water from dug wells while in other areas bore wells are suitable. In the hills further east, fracture planes are potential zones of groundwater and can sustain bore wells. Groundwater occurs under phreatic conditions in weathered mantle of the crystalline

rocks, laterites and unconsolidated coastal sediments. It occurs under semi confined to

confined conditions in the deep-seated fractured aquifers of the crystalline rocks and

Tertiary sediments (Figure 4).

Kannur district is underlain by charnockites, pyroxene granulites, garnetiferous

gneisses, hornblende biotite gneisses and schistose rocks overlain by Tertiaries and

coastal alluvium along the coast ranging in age from Archaean to Recent. These rocks

have undergone weathering and lateritisation. The hydrogeological units encountered

in the district are (i) consolidated formations (weathered and fractured crystallines) (ii)

Semi consolidated sediments equivalent to Warkalies of Southern Kerala and Laterite

formations and (iii) unconsolidated formations (Recent alluvium occurring along the

coast).

Figure 2: Geomorphology Kannur District (Source: District Resource map, Kannur district, Geological Survey of India)

Figure 3: Land use of Kannur. (Source: District Resource map, Kannur district, Geological Survey of India)

Figure 4: Geohydrology of Kannur. (Source: District Resource map, Kannur district, Geological Survey of India)

Figure 5: Soil types of Kannur. (Source: District Resource map, Kannur district, Geological Survey of India)

Figure 6: Geotechnical characteristics and natural hazards map of Kannur. (Source: District Resource map, Kannur

district, Geological Survey of India)

Several places along the coast are prone to beach erosion. The district falls under seismic zone III of ISI Classification (Figure 6).

China clay, bauxite, limeshell, lignite and laterite are the major economic minerals of the district. The district has large resources of good quality china clay used for a variety of industries. Good deposits are seen at Pazhayangadi and Kannapuram. Apart from china clay, district has resource of ball clay, fire clay and tile clay. Low-grade bauxite is associated with laterite. Bauxite occurs at Madayi, Pattuvamkunnu and east of Payyannur. The sedimentary sequences of madayi has thin seams of lignite with a cumulative thickness of 5m. Lignite is also reported from Kannur, Meenkunnu and Azhikod. Talc and steatite bands are reported from Thalassery and Kuthuparamba.

Ordinary earth is the common name used for the soils. Soil is made up of three main

components minerals that come from rocks below or nearby, organic matter which is the

remains of plants and animals that use the soil, and the living organisms that reside in the

soil. The proportion of each of these is important in determining the type of soil that is

present. But other factors such as climate, vegetation, time, the surrounding terrain, and even

human activities (eg. farming, grazing, gardening, landscaping, etc.), are also important in

influencing how soil is formed and the types of soil that occur in a particular landscape. The

formation of soils can be seen as a combination of the products of weathering, structural

development of the soil, differentiation of that structure into horizons or layers, and lastly,

of its movement or translocation. In fact, there are many ways in which soil may be

transported away from the location where it was first formed. Soils represent one of the most

complex and dynamic natural systems and are one of the three major natural resources, other

than air and water. Knowledge of their chemical, physical and biological properties is a

prerequisite both for sustaining the productivity of the land, e.g. agriculture, and for

conservation purposes. Soil is an integral part of a terrestrial ecosystem and fulfills numerous

functions including the capacity to generate biomass and the filtering or buffering activities

between the atmosphere and the groundwater in the biosphere. Soils have many important

functions. Perhaps the best appreciated is the function to support the growth of agricultural

and horticultural crops. Soil is the mainstay of agriculture and horticulture, forming as it

does the medium in which growth and ultimately the yield of food producing crops occurs.

Farmers and gardeners have worked with their soils over many centuries to produce

increasing amounts of food to keep pace with the needs of a burgeoning world population.

The soil's natural cycles go a long way in ensuring that the soil can provide an adequate

physical, chemical and biological medium for crop growth. As well as being essential to

agriculture, horticulture, forestry and natural and semi-natural systems, soil also plays an

important role for our fauna. The soil itself contains millions of organisms, the exact nature

and role of which we are still trying to determine. Undoubtedly, the soil flora and fauna play

a vital role in cycles which are fundamental to the ability of the soil to support natural and

semi-natural vegetation without additions of fertilizer and other support mechanisms. They

breakdown plant debris, take in components from the atmosphere; aerate the soil together

with many other functions that make the soil such an important medium.

Classification of soils (ordinary earth) commonly found in the district

The topo-lithosequence along with variation in rainfall, temperature and alternate wet and

dry conditions particularly from the western coast to high ranges in the east and swift flowing

rivers lead to the development of different types of natural vegetation and soil. The soils can

be broadly grouped into coastal alluvium, mixed alluvium, acid saline, kari, laterite, red, hill,

black cotton and forest soils. Soil map given below may be referred to find out its

occurrences.

Coastal Alluvium

These soils of marine origin are identified along the coastal plains and basin lands as a

narrow strip. The elevation of the coastal area is generally below 5m MSL. The area has high

water table and in some areas it reaches above the surface during rainy season. The soils of

the coastal plains are very deep with sandy texture. The texture generally ranges from sand

to loamy sand with greyish brown to reddish brown and yellowish red colour. Sand content

ranges from 80% and clay up to 15%. Even though these soils have high water table, the

water holding capacity is poor due to the predominance of sand. Coconut is the major crop

in the area. Cashew and other fruit trees are also grown.

Mixed Alluvium

These soils are developed from fluvial sediments of marine, lacustrine and riverine

sediments or its combinations. They occur below 20m MSL in the lowland plains, basins,

valleys and along the banks of major rivers. The mixed alluvium is mainly noticed close to

coastal alluvium, Kuttanad and adjacent area and kole lands of Thrissur district. The soils

are frequently flooded and submerged. The soils of depressions and broad valleys are subject

to occasional flooding and stagnation. The ground water table of these soils is generally high

and it reaches above the surface during rainy season. A wide variation in texture is noticed

in these soils. Sandy clay loam to clay is the predominant texture. Sandy loam soils are also

met with. Light grey to very dark brown is the common colour of the soil. Paddy, other

annuals and seasonal crops like banana, tapioca and vegetables are grown here.

Acid Saline Soil

Acid saline soils are present throughout the coastal area in patches with very little extent.

Major area of this soil is identified in the coastal tract of Ernakulam, Thrissur and Kannur

districts. The area under these soils comprise of low-lying marshes, waterlogged and ill

drained areas near the rivers and streams, which are subject to tidal waves. Sea and

backwater tides make these soils saline. During monsoon season, when rainwater and fresh

water from rivers enter the fields, salinity is partially washed off. The area under these soils

occur mostly on plains at or below sea level. A wide variation in texture from sandy loam to

clay is noticed with dark grey to black colour. Paddy is the only crop that can be cultivated.

Laterite soil

Laterite and laterite soil are the weathering products of rock in which several course of

weathering and mineral transformations take place. This involves removal of bases and

substantial loss of combined silica of primary minerals. In laterite and laterite soils, over

acidic rocks, induration and zonation are more pronounced. This induration is greater if the

iron content is higher. These soils mainly occur in the midlands and part of lowlands at an

elevation of 10 to 100m above MSL as a strip between the coastal belt and hilly midupland.

The area comprises of mounds and low hills with gentle to steep slopes. Laterite soils are

generally suitable for most of the dryland crops. It is mainly cultivated with coconut,

arecanut, banana, tapioca, vegetables, yams, pepper, pineapple, fruit trees etc. The

percentage of gravel content in the soil and reduced soil depth limits the choice of crops. In

laterite outcropped area with shallow soils, only cashew can be grown with vegetables.

Hill Soil

The hill soils mostly occur above an elevation of 80m MSL. The area is hilly and has highly

dissected denudational hills, elongated ridges, rocky cliffs and narrow valleys. The general

slope range is above 10%. The texture of these soils generally range from loam to clay loam

with average gravel content of 10 to 50%. In addition, stones and boulders are noticed in the

subsoil. These soils have reddish brown to yellowish red/strong brown colour. Generally,

increase in clay content is noticed down the profile. The depth of the soil varies considerably

from 60 to 200 cm depending on the lie of the land, erodibility of soil and past erosion. These

soils are mostly friable and subject to heavy soil erosion. The area is suitable for all dryland

crops like rubber, coconut, arecanut and fruit trees based on the topography. Crops such as

banana, pepper, pineapple, vegetables can be grown in foot slopes.

Forest Soil

These soils are developed from crystalline rocks of archaean age under forest cover. They

occur along the eastern part of the State, generally above an elevation of 300m above MSL.

The area is hilly and mountainous with steep slopes, escarpments, elongated rocky summits

erosion and vegetative cover. The soils are generally immature due to slow weathering

process. Rock outcrops and stones are noticed on the surface. Gneissic boulders under

different stages of weathering are noticed in the subsoil. The texture of the soil ranges from

sandy clay loam to clay with reddish brown to very dark brown colour. Forest trees, shrubs

and grasses are grown here.

Mining of ordinary earth

Usually ordinary earth is mined for leveling of ground for construction of buildings. Since

ordinary earth is very important to mankind, it is not wise to mine ordinary earth for filling

purposes alone. However, for the construction of roads and other infrastructure, ordinary

earth as mined after obtaining quarrying permit from the Department of Mining and

Geology. Mining and transporting ordinary earth/soil without the permission of Department

of Mining and Geology is an offence. Department issues pass for transport of ordinary earth.

commercial purposes.

Clays and clay minerals occur under a fairly limited range of geological conditions and are

produced by weathering of silicate minerals containing calcium, magnesium, sodium, or

potassium reacting with carbonic acid, carbonates, and bicarbonates. These soluble products

are removed by ground water, while the remaining elements, aluminum, silicon, and oxygen

combine with water to produce stable clay minerals. The environment of formation include

soil horizons, continental and marine sediments, geothermal fields, volcanic deposits, and

weathering rock formations. Extensive alteration of rocks to clay minerals can produce

relatively pure clay deposits that are of economic interest. Clay formed at the site of the

parent rock is known as primary or residual clay; the one carried away or transported and

deposited elsewhere is known as secondary clay. For obvious reasons, the former is purer

with less impurity (5% 15%), while the latter may contain mica, quartz, and iron oxide as

impurities. Geological factors such as conditions at the time of deposition and post-

depositional changes have an important influence on the properties of sediment.

Buildings and utensils made of clay date back to the earliest periods of man's civilized

development, and the use of clay is intimately associated with his history. Tile and brick

continued in modern buildings as well.

In Kerala, tile/brick clay occurs in the wetlands/paddy fields in the lowlands and midlands.

The clay extracted is used for a variety of purposes such as manufacture of roofing, flooring,

and decorative tiles, wire cut (mechanically made) and ordinary bricks (manually made), and

pottery wares. Studies carried out in clay mining areas of Kerala have proved that

unprecedented increase in the development needs of the state and the subsequent increase in

the resource extraction scenarios, especially that of clay mining, have led to rapid

degradation of the wetlands (paddy fields), which is significantly reflected in the declining

agricultural productivity of the state. Mining of clays several meters below the prescribed

levels, water draining from the unaffected paddy lands into the adjacent mine pits, and

subsequent pumping of water for further mining impose severe problems on the hydrological

regime, lowering the water table and creating severe water shortage problems in the mining

areas. The additional expenditure incurred to meet the freshwater requirements of the people

living in areas adjacent to mining sites is increasing year after year, which undermines the

short-term economic benefits of resource extraction.

Tile and brick clay mining and its processing provide employment opportunities to a

considerable section of the people in the midland and lowland areas of Kerala. Adding to

this, thousands of laborers in the construction industry also indirectly depend on the products

manufactured from these clays. Under these circumstances and also with respect to the

demand incurred, complete restriction of extraction activities does not prove to be viable.

In the study report published by National Center for Earth Science Studies on the impact of

clay mining, following recommendations were given with respect to tile/brick clay mining:

ce to regulate random mining from the paddy fields/wetlands of

Kerala by allowing only location-specific resource extraction under well-conceived

guidelines. It is also crucial to limit the extraction of tile and brick clays to meet indigenous

and local demand only. This is to save the prime agricultural land and also to increase the

rice production in the area. The depth of mining should be demarcated so as to regulate

mining with respect to the water table condition in the summer season. Also, adequate

measures are to be taken to regenerate the natural ground water table using the stored water

in the clay mine pits for irrigating the agricultural crops of the hinterland areas. This will

enhance the net agricultural productivity of the area in addition to saturating the aquifer

systems in the hinterlands. Awareness creation among the public about the adversities of

clay mining and as well as the economic benefits of using clay bricks for construction

purposes will serve in the protection of our wetlands/paddy fields. Recycling of building

materials should also be considered in order to reduce mining of tile and brick clays. The

abandoned clay mine areas left behind as fallow lands or water logged areas can be used for

productive purposes such as fish farm ponds or irrigation ponds that promise some utility to

the society. Also, suitable guidelines should be framed to streamline the tile and brick clay

The Kerala Conservation of Paddy Land and Wetland Act, 2008 and Rules made thereunder

which was enacted for conservation of paddy land and wetlands of Kerala imposes

restrictions in mining of tile/brick clays in such areas. The said Act and Rules are

implemented by Revenue Department. In addition, Government have setup District Expert

Committee to monitor and control the mining activities of ordinary clay. In Kerala Minor

Mineral Concession Rules 2015, it is mandated that No Objection Certificate from the

District Collector concerned, based on the recommendation of the District Expert Committee

constituted by the Government in this regard, is to be produced by the applicant in the case

of application for extraction of ordinary clay. In addition, Bank guarantee from any

Nationalized or Scheduled Bank at the rate of Rs. 300 (Rupees three hundred only) per cubic

metre for the purpose of reclamation of pits that will be formed after quarrying in the area

permitted, in respect of application for extraction of ordinary clay. Based on the request of

the entrepreneurs working in tile/brick clay based industry, Government have instructed the

Department of Mining and Geology to carry out survey to identify the mineable tile/brick

clay deposits of Kerala and the work in this respect is progressing.

In Kerala Minor Mineral Concession Rules, 2015, the ordinary sand is defined as sand used

for non-industrial purpose. This includes both river sand and sand excavated from inland

areas like palaeo-channels. Since a separate Act has been enacted by Government of Kerala

namely, The Kerala Protection of River Banks and Regulation of Removal of Sand Act, 2001

(hereafter referred to as Sand Act, 2001) and since the mining of river sand is controlled by

Revenue Department by virtue of the powers conferred by the said Act and the Rules made

thereunder, the Department of Mining and Geology now regulates the mining of sand which

do not comes under the purview of Sand Act, 2001.

The ordinary sand (other than river sand) occurs in the palaeo-channels. The word paleo-

channel is -channel is an

old channel. Paleo-channels are deposits of unconsolidated sediments or semi-consolidated

sedimentary rocks deposited in ancient, currently inactive river and stream channel systems.

These are typical riverine geomorphic features in a location representing drainage streams,

rivers, rivulets which were flowing either ephemeral or perennial during the past time and

now stands either buried or lost or shifted due to tectonic, geomorphologic, anthropogenic

process/activities, as well as climatic changes. When a channel ceases to be part of an active

river system, it becomes a paleo-channel. In order to tap the ordinary sand occurring in

palaeo-channels, the Department entrusted the study of identification of palaeo-channels in

major river basins of Kerala to Geological Survey of India (GSI). GSI resorted to remote

sensing studies using satellite imageries and delineated some of the palaeo-channels.

However, since such deposits falls in paddy land/wetlands of Kerala, it is difficult to extract

such sand on account of restrictions imposed by various Acts and Rules.

The Kerala Conservation of Paddy Land and Wetland Act, 2008 and Rules made thereunder

which was enacted for conservation of paddy land and wetlands of Kerala imposes

restrictions in mining of ordinary sands occurring in wetlands and paddy fields. The said Act

and Rules are implemented by Revenue Department. In addition, Government have setup

District Expert Committee to monitor and control the mining activities of ordinary sand. In

Kerala Minor Mineral Concession Rules 2015, it is mandated that No Objection Certificate

from the District Collector concerned, based on the recommendation of the District Expert

Committee constituted by the Government in this regard, is to be produced by the applicant

in the case of application for extraction of ordinary sand. In addition, Bank guarantee from

any Nationalized or Scheduled Bank at the rate of Rs. 300 (Rupees three hundred only) per

cubic metre for the purpose of reclamation of pits that will be formed after quarrying in the

area permitted, in respect of application for extraction of ordinary sand.

The mining of ordinary sand from palaeo-channels also case some environmental concerns.

Since sand is a good aquifer, the mining of aquifer system poses threat to ground water

availability in surrounding areas. However in certain cases, the mining of such sand from

paddy lands increase the productivity of paddy as excess sand in the paddy lands are not

good for paddy.

In Kerala, due to shortage of river sand and ordinary sand occurring in palaeo-channels, the

construction industry now uses manufactured sand obtained by crushing of crystalline rocks.

It may be noted that since the Revenue Department is taking care of all types of mining

activities related to river sand and since sand auditing and other studies are carried

out under the aegis of the Revenue Department, this report shall not be used for the

purpose of obtaining prior environmental clearance for mining of river sand.

Laterite is a soil and rock type rich in iron and aluminium, and is commonly considered to

have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration,

because of high iron oxide content. They develop by intensive and long-lasting weathering

of the underlying parent rock. Tropical weathering is a prolonged process of chemical

weathering which produces a wide variety in the thickness, grade, chemistry and ore

mineralogy of the resulting soils. The majority of the land area containing laterites is between

the tropics of Cancer and Capricorn.

Angadipuram Laterite is a National Geological Monument identified in Angadipuram town

in Malappuram district. The special significance of Angadipuram to laterites is that it was

here that Dr. Francis Buchanan-Hamilton, a professional surgeon, gave the first account of

this rock type, in his report of 1807, as "indurated clay", ideally suited for building

construction. This formation falls outside the general classification of rocks namely, the

igneous, metamorphic, or sedimentary rocks but is an exclusively "sedimentary residual

product". It has a generally pitted and porous appearance. The name laterite was first coined

in India, by Buchanan and its etymology is traced to the Latin word "letritis" that means

bricks. This exceptional formation is found above parent rock types of various composition

namely, charnockite, leptynite, anorthosite and gabbro in Kerala. The laterite profiles in

different types of rocks varies depending on the composition of parent rock. For example in

Charnockites, the thickness of the profile ranges from 2 m to 10 m with humus zone on the

top with thin pebbly zone (with ferruginous pellets in clayey matrix), underlain by

vermicular laterite with tubular cavities of various shapes and size filled with kaolinitic clay.

This is followed by thin layer of lithomarge. Further below completely weathered, partly

weathered or fresh parent rock occur. In some places one can see hard duricrust at the top.

The mineralogical study of laterites reveals that all the silicate minerals have been

transformed to a mixture of goethite, hematite and kaolinite in laterite samples developed

over charnockite. Further studies revealed that pyroxenes have been altered to goethite while

feldspars gave rise to kaolinite. Quartz is cracked, eroded and disintegrated. Monazite and

Zircons are found as accessory minerals.

Laterite and bauxite show a tendency to occur together. Aluminous laterites and ferruginous

bauxites are quite common. The most common impurity in both is silica. Laterite gradually

passes into bauxite with decrease in iron oxide and increase in aluminium oxide.The laterite

deposits may be described on the basis of the dominant extractable minerals in it: (i)

aluminous laterite (bauxite), (ii) ferruginous laterite (iron ore), (iii) manganiferous laterite

(manganese ore), (iv) nickeliferous laterite (nickel ore) and (v) chromiferous laterite (chrome

ore). Laterite with Fe2O3:Al2O3ratio more than one, and SiO2:Fe2O3 ratio less than 1.33

is termed as ferruginous laterite,while that having Fe2O3:Al2O3 ratio less than one and

SiO2:Al2O3 ratio less than 1.33 is termed as aluminous laterite. Laterite can be considered

as polymetallic ore as it is not only the essential repository for aluminium, but also a source

of iron, manganese,nickel and chromium. Furthermore, it is the home for several trace

elements like gallium and vanadium which can be extracted as by-products.

In Kerala laterites are extracted as building stones which are used for construction of

building. Laterite as a building stone possesses one advantage that it is soft when quarried

and can be easily cut and dressed into blocks and bricks which on exposure to air become

hard. In addition, laterite (aluminous laterite) is extracted for industrial purposes (for eg.

Cement industry). In addition to aluminous laterite, bauxites are also mined in Kerala.

Hence, while granting mineral concession for laterite it is necessary to carry out the chemical

analysis to establish whether the mineral is bauxite or aluminous laterite.

Laterite, the main construction material of the area, has a very wide distribution. It is quarried

in the form of large bricks and is used in building construction. The basement rocks are also

good source of construction material.

For administrative purpose the hard crystalline rocks which do not have any economic

minerals are classified as granite dimension stones and granite (building stones). The

definition given in the Kerala Minor Mineral Concession Rules 2015 is as follows:-

other crystalline rocks of Acid, Intermediate, basic and ultra basic groups of igneous and

metamorphic origin which are suitable for cutting to pre-determined sizes, polishing, carving

and amenable for making value-added products in decorative monumental and ornamental

fields of industry as a high-value item. Granite (building stone) include all those group of

rocks specified above which are not suitable for using as dimension stones as specified

therein, but can be used as ordinary building stones, road metal, rubble and ballasts after

breaking into irregular pieces by blasting or otherwise as low value item. The Rules insists

that the rocks having the quality of granite dimension stone shall not be quarried for granite

The granite dimension stones, on the basis of geologic setting falls under

True intrusive or anatectic granites and associated migmatites of Proterozoic age from (colour: Pink, light pink, Gray, yellowish white and bluish pink with wavy patterns) and

Dolerite-Gabbro dykes, Proterozoic intrusive hypabasal dyke swarms from (colour: dark greenish blue, black and dark gray with black spots).

All Archean and Proterozoic rocks of Kerala (refer section on Geology of Kerala) which are

not listed above as granite dimension stone falls under the category of granite (building

stone) and are found below ordinary earth/laterites/and other sedimentary rocks. In some

cases such rocks are exposed as hillocks without any overburden.

In Kerala, the lime shell occurs in the backwaters/estuaries, river mouths and lagoons along

the coastal tract.

The lime shell resources next in importance to Vembanad lake are those in Kannur district

(Payyannur, Cheruvanthur, Thrikkarippur) in north Kerala. The backwaters along the coast

have good resources of lime shell. The alluvial deposit of Kandankali, south of Payyannur

is also rich in lime shell. Since all these areas falls in Coastal Regulation Zones, mechanized

mining is not permitted.

Permission for mining will be granted on case to case basis on ascertaining the availability

at the site and only if conditions stipulated in the KMMC Rules 2015 are satisfied (The

reader may refer the KMMC Rules 2015 available in the website www.dmg.kerala.gov.in for

more details in this regard) The concession will be granted only if other statutory licenses

like Environmental Clearnce, Explosive Licence, consent to operate issued by State

Pollution Control Board, NOC issued by Revenue Department (as the case may be),

Dangerous and Offensive Trade Licence issued by Local Self Government Institutions, NOC

related to Coastal Regulation Zone (as the case may be), NOC issued by Forest (as the case

may be) etc. The mineral concession will not be granted in the ecologically sensitive areas,

ecological fragile zones etc.

http://www.dmg.kerala.gov.in

10.4

Sta

tus o

f min

ing

in K

annu

r di

stri

ct

Tab

le1:

Det

ails

of r

even

ue c

olle

ctio

n fo

r th

e pe

riod

201

3--

-16

(Am

ount

in R

s.)

Rev

enue

Col

lect

ion

(Dur

ing

2013

-14)

M

ajor

Min

eral

s La

terit

e

Chi

na

Cla

y Li

me

shel

l G

rani

te

Seas

hell

Riv

er

Ord

inar

y

Bric

k

Ord

inar

y

Sa

nd

Sand

C

lay

Earth

N

o.

Parti

cule

rs

Amou

nt in

Rup

ees

1 A

pplic

atio

n fe

e fo

r Min

ing

Leas

e

2 Fe

e fo

r pro

spec

ting

licen

ce

3

Roy

alty

25

8816

0 36

0000

4 A

rrea

r Roy

alty

5 S

urfa

ce R

ent

6

Dea

d R

ent

7

Pan

el In

tere

st

8

Com

poun

ding

of o

ffenc

e

To

tal

2588

160

3600

00

Min

or M

iner

als

N

o.

Parti

cule

rs

Amou

nt in

Rup

ees

1 R

oyal

ty

1250

0 41

1200

2518

932

1695

000

48

600

2 A

rrea

r Roy

alty

1468

90

3

Sur

face

Ren

t 8,

610

5497

44

4

Arr

ear S

urfa

ce R

ent

5

Dea

d R

ent

20

0

6 A

rrea

r Dea

d R

ent

7

Fee

for Q

uarry

ing

Perm

it 1,

59,4

00

3750

0

400

800

8 Fe

e fo

r Qua

rryin

g Le

ase

10

00

9

Fee

for P

rosp

ectin

g Li

cenc

e

10

Fee

for D

eale

rs L

icen

ce

6000

12

2700

0

30

6000

11

C

onso

lidat

ed ro

yalty

(CR

PS

) 91

5500

0

48

6000

0

12

Com

poun

ding

of o

ffenc

e 16

0092

6

26

5816

84

400

13

Oth

er D

epar

tmen

ts

45

000

1906

30

14

Oth

er R

ecei

pts

22

5000

0

15

RM

CU

Com

poun

ding

To

tal

1,09

,29,

936

12

,500

91

,03,

213

25

,18,

932

2,19

,163

0 1,

46,8

90

1,33

,844

Gra

nd T

otal

1,

35,1

8,09

6 3,

60,0

00

12,5

00

91,0

3,21

3

25,1

8,93

2 21

,91,

630

1,46

,890

1,

33,8

44

Rev

enue

Col

lect

ion

(Dur

ing

2014

-15)

Maj

or M

iner

als

Late

rite

C

hina

Cla

y Li

mes

hell

Gra

nite

R

iver

O

rdin

ary

B

rick

O

rdin

ary

Sa

nd

Sand

C

lay

Earth

N

o.

Parti

cule

rs

Amou

nt in

Rup

ees

1 A

pplic

atio

n fe

e fo

r Min

ing

Leas

e

2

Fee

for p

rosp

ectin

g lic

ence

3

Roy

alty

12

0278

18

1500

00

4 A

rrea

r Roy

alty

5

Sur

face

Ren

t 36

03

6

Dea

d R

ent

4921

7 P

anel

Inte

rest

8

Com

poun

ding

of o

ffenc

e

Tota

l 12

0363

42

1500

00

M

inor

Min

eral

s

No.

Pa

rticu

lers

Am

ount

in R

upee

s 1

Roy

alty

70

00

5544

00

1965

610

8923

760

2 A

rrea

r Roy

alty

14

3255

3 S

urfa

ce R

ent

4,58

0

26

78

4 A

rrea

r Sur

face

Ren

t

5

Dea

d R

ent

6 A

rrea

r Dea

d R

ent

7 Fe

e fo

r Qua

rryin

g Pe

rmit

83,0

00

2000

0

8

Fee

for Q

uarry

ing

Leas

e

9

Fee

for P

rosp

ectin

g Li

cenc

e

10

A

pp. F

ee fo

r Dea

lers

Lic

ence

1850

0

11

C

onso

lidat

ed ro

yalty

(CR

PS

) 50

1000

0

34

3000

0

12

C

ompo

undi

ng o

f offe

nce

1429

480

9166

80

16

3846

13

O

ther

Dep

artm

ents

20

000

2500

0 14

O

ther

Rec

eipt

s

15

R

MC

U C

ompo

undi

ng

14

0000

0

16

A

rear

RM

CU

5150

000

17

App

. Fee

for R

eg.M

iner

al S

ales

Dep

ot

63

000

18

Fee

for D

eale

rs L

icen

ce

18

9600

0

1320

00

To

tal

65,4

7,06

0

7,00

0 13

4512

58

1965

610

9055

760

1432

55

1888

46

G

rand

Tot

al

1,85

,83,

402

1500

00

7,00

0 13

4512

58

1965

610

9055

760

1432

55

1888

46

Rev

enue

Col

lect

ion

(Dur

ing

2015

-16)

M

ajor

Min

eral

s La

terit

e

Chi

na

Cla

y G

rani

te

Riv

er

Ord

inar

y B

rick

Ord

inar

y O

rdin

ary

TO

TAL

Sa

nd

Sand

C

lay

Earth

C

lay

N

o.

Parti

cule

rs

Amou

nt in

Rup

ees

1 A

pplic

atio

n fe

e fo

r Min

ing

Leas

e

2 Fe

e fo

r pro

spec

ting

licen

ce

3

Roy

alty

10

7508

69

3000

0

10

7808

69

4 A

rrea

r Roy

alty

5 S

urfa

ce R

ent

6

Dea

d R

ent

7

Pan

el In

tere

st

8

Com

poun

ding

of o

ffenc

e 41

,561

41,5

61

To

tal

1079

2430

30

000

1082

2430

Min

or M

iner

als

N

o.

Parti

cule

rs

Amou

nt in

Rup

ees

1 R

oyal

ty

5648

400

6359

06

2786

4840

1612

00

34

3103

46

2 A

rrea

r Roy

alty

2500

25

00

3 S

urfa

ce R

ent

6,18

0

3031

9,21

1 4

Arr

ear S

urfa

ce R

ent

5

Dea

d R

ent

5290

5,29

0 6

Arr

ear D

ead

Ren

t

7 Fe

e fo

r Qua

rryin

g Pe

rmit

6,71

,000

1360

00

1000

8,

08,0

00

8 Fe

e fo

r Qua

rryin

g Le

ase

2600

00

2,

60,0

00

9 Fe

e fo

r Pro

spec

ting

Lice

nce

10

A

pp. F

ee fo

r Dea

lers

Lic

ence

58

500

10

00

59

500

11

Con

solid

ated

roya

lty (C

RP

S)

4660

0000

9275

000

55

8750

00

12

Com

poun

ding

of o

ffenc

e 49

1744

8

1844

660

25

000

31

5192

7102

300

13

Oth

er D

epar

tmen

ts

14

O

ther

Rec

eipt

s

15

RM

CU

Com

poun

ding

90

0000

0

9000

000

16

RM

CU

Com

poun

ding

(Are

ar)

4000

00

40

0000

17

A

pplic

atio

n fe

e fo

r RM

CU

70

00

70

00

18

CR

PS

(Are

ar)

4462

524

56

4755

9

1011

0083

19

A

pp. F

ee fo

r Reg

.Min

eral

Sal

es D

epot

60

000

13

000

73

000

20

Fee

for D

eale

rs L

icen

ce

3004

000

56

000

30

6000

0

Tota

l 5,

66,5

7,15

2

3534

9440

63

5906

27

9598

40

2500

47

6392

10

00

1210

8223

0

Gra

nd T

otal

6,

74,4

9,58

2 30

000

3534

9440

63

5906

27

9598

40

2500

47

6392

10

00

1319

0466

0

List

of v

alid

min

eral

con

cess

ions

Tab

le 2

a: L

ist o

f Qua

rryi

ng L

ease

gra

nted

for

Gra

nite

bui

ldin

g st

one

Sl.

No.

C

once

ssio

n H

olde

r's

Nam

e &

Add

ress

C

once

ssio

n N

o.

Surv

ey N

o/

Re.

Surv

ey N

o.

Vill

age

Tal

uk

Are

a

(Ha)

V

alid

from

V

alid

to

1 Ja

cob

barr

y, B

arry

Es

tate

, Kat

tuss

ery(

PO),

Ala

thur

.

269/

2007

-08

/444

8/M

3/20

07

date

d, 2

0.07

.07

Res

y.no

. 340

/2pt

A

lath

ur

Ala

thur

1

Hec

tres,

12

year

s, 25

.07.

07

24.

07.2

019

2 M

.D.A

nil k

umar

,

M/s

Mac

adam

G

rani

tes(

P)Lt

d,

Pann

ikko

de (P

O),

Pala

kkad

185/

2007

-08

/456

9/M

3/20

07/D

ate

d, 1

9.06

.07

ReS

y.N

o. 4

27 p

t, 43

5pt.

Erim

ayur

II

Ala

thur

3.

3630

he

ctre

s,

10 Y

ears

21

.07.

2007

20

.07.

2017

3 M

/s. S

ahar

a G

rani

tes,

Erim

ayur

P.O

, Pa

lakk

ad

63/2

012-

13/3

857/

M3/

2012

D

t. 28

.04.

2012

Sy.N

o. 3

5/2

& 3

5/3

Erim

ayur

-I A

lath

ur

1.84

85

Hec

tare

s 12

Yea

rs

02

/05/

2012

01

-05-

2024

4 M

/s. S

ahar

a G

rani

tes,

Erim

ayur

P.O

, Pa

lakk

ad

65/2

012-

13/3

858/

M3/

2012

D

t. 28

.04.

2012

Re.

Sy.N

o. 3

5/2

Erim

ayur

-I A

lath

ur

2.42

82

Hec

tare

s 12

Yea

rs

02

/05/

2012

01

-05-

2024

5 M

/s. S

ahar

a G

rani

tes,

Erim

ayur

P.O

, Pa

lakk

ad

66/2

012-

13/3

859/

M3/

2012

D

t. 28

.04.

2012

Re.

SyN

o. 3

5/2

Erim

ayur

-I A

lath

ur

2.61

02

Hec

tare

s 12

Yea

rs

02

/05/

2012

01

-05-

2024

6 Se

bi. P

.L.,

S/o

P.C

. Lo

nai,

Pani

kula

ngar

a H

ouse

, Fas

hion

Stre

et,

Mis

sion

Qua

rters

, Th

rissu

r - 5

389/

2011

-12

/721

9/M

3/20

11 d

t. TV

PM, 2

4.09

.201

1

Rsy

No.

33/

2 an

d 23

4/2

Kan

nam

bra

I A

lath

ur

1.45

04

Hec

t

12 y

ears

, 28

.09.

2011

2

7.09

.202

3

7 M

/s K

ottu

kapi

lly S

and

& M

etal

s (p)

Ltd

., K

alpa

thy

P.O

., Pa

lakk

ad.

298/

2011

-12

/571

4/M

3/20

11 d

t. 16

.08.

2011

Sy N

o. 3

/2

Kiz

hakk

ache

ry II

A

lath

ur

2.84

09

Hec

t 10

Yea

rs

23.0

9.20

11

22.

09.2

021

8 V

.Sas

idha

ran,

Pr

opre

itor,

M/s

. SriS

ri G

rani

tes,

Pe

echa

road

, Chi

thal

i (P

O),

Pala

kkad

240/

2008

-09

/673

9/M

3/08

/ da

ted,

14.

07.0

8

Sy.n

o.66

3/4,

8,9,

10

K

utha

nur.1

A

lath

ur

1.40

89

Hec

tres

10 y

ears

28

.07.

08

27.

07.2

018

9 Jo

hsn

Thom

son,

Pr

oprie

tor,

M/s

. Tr

opic

al G

rani

tes,

Trop

ical

Est

ate,

K

utha

nur.

P.O

, A

lath

ur, P

alak

kad

492/

2008

-09

/943

9/M

3/20

08/d

ated

, 15.

11.0

8

Res

y.no

. 651

/8

Kut

hanu

r.1

Ala

thur

1.

9320

H

ectre

s 12

yea

rs

05.0

1.09

0

4.01

.202

1

10

P.P.

Seb

astia

n,

Po

ovat

huka

ran

Hou

se,

Thal

ore

P.O

., Th

rissu

r

329/

2010

-11

/477

5/M

3/20

10 d

t. 20

.08.

2010

Res

y.N

o. 2

68/2

pt

Vad

akke

nche

ry I

A

lath

ur

0.43

18

Hec

t 12

Yea

rs

27.9

.201

0

26.0

9.20

22

11

P.T.

Dav

is, M

anag

ing

Partn

er, T

hom

son

Met

als,

Kom

bidi

njam

akka

l,PO

, Th

azek

kad

58/2

011-

12/2

870/

M3/

2011

dt

.04.

05.2

011

Re.

Sy. N

os. 2

08/1

, 20

8/3,

209/

pt.,2

10/2

,210

/3,2

10/4

,210

/5

Mut

hala

mad

a I

Chi

ttur

4.83

66

Hec

t.

12

Yea

rs

13.0

5.20

11

12.0

5.20

23

12

Bini

l K Jo

hn, M

g.

Dire

ctor

, Val

luva

nad

quar

ries a

nd

Gra

nite

s(Pv

t) L

td.,

Ang

amal

ly,

Erna

kula

m.

747/

2010

-11

/910

/M3/

2011

dt.

31.0

1.20

11

Res

y N

o. 3

30/2

pt

., 33

0/3p

t; an

d 33

1/1

pt.

Am

bala

ppar

a I

Otta

ppal

am

1.53

48

Hec

t 12

Yea

rs

11.0

2.20

11

10.0

2.20

23

13

Aja

iwils

on,

Man

agin

g Pa

rtner

,

M/s

Mal

abar

Blu

e M

etal

, Ven

gass

ery

(PO

) Am

bala

ppar

a,

Pala

kkad

.

184/

2008

-09

/782

2/M

3/20

07

date

d, 1

9.08

.08

Sy.N

os. 4

60/5

pt,

462/

9, 4

62/5

, 106

/1

pt

Am

bala

ppar

a.1.

O

ttapp

alam

1.

4164

he

ctre

s,

12 y

ears

18

.07.

08

17.

07.2

020

14

Rap

hy.P

.J.,

Pud

usse

ry

pady

Hou

se, T

hrik

kur

(PO

), Th

rissu

r.

296/

2008

-09

/689

0/M

3/20

08/d

ated

, 13.

08.2

008.

Sy.n

o. 2

26/3

C

hala

vara

O

ttapp

alam

0.

8094

H

ect.

10 y

ears

, 26

.09.

08

25

.09.

2018

15

M/s

Blu

e Ch

ips M

ines

&

Indu

strie

s, V

emba

lath

upad

am,

Kai

liyad

P.O

., O

ttapp

alam

.

Pro.

orde

r.No.

66

8/20

08-

09/7

814/

M3/

08 d

t Tv

pm, 3

1.01

.200

9 an

d

304/

09-

10/7

814/

M3/

08

dt.

14.0

9.20

09

and

Re

exec

utio

n vi

de

Pro.

No.

268

/201

1-20

12/7

814/

M3/

2008

dt

. 29.

07.2

011

of

DM

G

Sy N

o. 1

68/ 1

1 A

,

Cha

lava

ra

Otta

ppal

am

1.61

00

Hec

t

12 Y

ears

26

.08.

2011

2

5.08

.202

3

16

Geo

sons

Agg

rega

tes,

A

may

ur, P

atta

mbi

, Pa

lakk

ad.

32/2

006-

07/3

471/

M3/

06

date

d, 2

5.04

.06

59/

4 K

oppa

m

Otta

ppal

am

0.60

70

hect

res,

12 y

ears

07

.06.

2006

. 06

.06.

2018

17

M.K

.Jose

ph, M

g.

Partn

er,

M

/s.

Mal

abar

Gra

nite

s,

Am

ayur

P.O

., Pa

ttam

bi, P

alak

kad.

792/

2010

-11

/499

9/M

3/20

10 d

t. 24

.02.

2011

Res

y N

os. 3

65,3

66

367/

5 K

oppa

m

Otta

ppal

am

3.52

04

Hec

t 12

Yea

rs

09.0

3.20

11

08.0

3.20

23

18

M/s

J &

P C

onstr

uctio

n &

J & P

Gra

nite

s, C

hoor

akod

e P.

O.,

Patta

mbi

, Pal

akka

d.

Pro.

orde

r No.

53

5/20

11-

12/7

819/

M3/

2011

dt.

15.1

1.20

11.

Rsy

No.

75

78/2

V

alla

ppuz

ha

Otta

ppal

am

1.61

90

Hec

t.

10 Y

ears

30

.11.

2011

29

.11.

2021

19

M/s

. Mal

abar

Gra

nite

M

etal

, Van

iam

kula

m

Man

nann

ur (P

O)

Kav

alap

para

,Pal

akka

d

860/

2007

-08

/128

3/M

3/20

08/d

ated

, 28.

02.0

8

SyN

o. 3

9/1p

t 39

/2pt

V

ania

mku

lam

.2

Otta

ppal

am

1.57

02

Hec

tres

10 y

ears

26

.03.

08

25.

03.2

018

20

Bini

l K Jo

hn,

Man

agin

g Pa

rtner

, M/s.

V

allu

vana

d G

rani

tes,

Nel

likku

russ

i. P.

O,

Mul

anhu

r, O

ttapp

alam

, Pa

lakk

ad

418/

2014

-15

/963

9/M

3/20

14 D

t. 27

/09/

2014

Re.

Sy.N

o. 2

/2, 5

/2

Lakk

idi -

Peru

r-1

Otta

ppal

am

1.78

22

Hec

tare

s 20

-10-

2014

30

-10-

2018

21

Smt.A

nnie

Sann

ie,

Mg.

Dire

ctor

,

M/s

Mal

ayak

am

Agg

regr

ates

&

Sand

s(P)

Ltd

, ch

azhi

yatti

ri (P

O),

Pala

kkad

482/

2007

-08

/750

5/M

3/07

da

ted,

01.

11.0

7

sy.n

o. 2

74 p

t. Th

irum

ittak

kode

.2

Otta

ppal

am

1.78

00

Hec

tres

12 y

ears

13

.11.

07

12.

11.2

019

22

Saji

Mon

Abr

aham

,

S/

o A

brah

am,

Pala

kkat

tu H

ouse

, K

umm

anoo

r, K

idan

goor

P.O

., K

otta

yam

.

120/

2010

-11

/335

5/M

3/20

10 d

t. 26

.05.

2010

Res

y.N

o: 1

10/1

, 11

0/3

Aka

thet

hara

Pa

lakk

ad

2.77

21

Hec

t

(6.8

5 ac

re)

12 Y

ears

11.0

8.20

10

10.0

8.20

22

23

M/s

. Roy

al S

and

&

Gra

vels

(P) L

td.,P

laza

Ju

nctio

n, D

honi

.(P.O

), Pa

lakk

ad

281/

2014

-15

/847

3/M

3/20

14 D

t. 02

/08/

2014

Sy.N

o. 2

/P, 1

4/P,

15

/P, 1

6/1P

A

kath

etha

ra

Pala

kkad

7.

0655

H

ecta

res

12 y

ears

22/0

8/20

14

21-0

8-20

26

24

P.I.D

evas

sia,

Aru

man

i Es

tate

, Noc

hipu

lly,

Mun

dur,

Pala

kkad

.

431/

2007

-08

/647

5/M

3/20

07

DA

TED

, 05.

10.0

7

Res

y.no

. 449

/1pt

M

undu

r.2

Pala

kkad

0.

8174

H

ectre

s 12

year

s, 01

.12.

07

30

.11.

2019

25

Sabu

Tho

mas

,

Kal

apur

acka

l Hou

se,

Aya

rkun

nam

(PO

), K

otta

yam

.

200/

2007

-08

/481

9/M

3/20

07

date

d, 2

5.06

.07

Res

y.no

. 320

/2

Puth

usse

ry c

entra

l Pa

lakk

ad

1.41

65

Hec

tres,

12 y

ears

fro

m

06.0

8.07

05.

08.2

019

Tab

le 2

b: L

ist o

f Qua

rryi

ng P

erm

it gr

ante

d fo

r G

rani

te b

uild

ing

ston

e

Sl.

Con

cess

ion

hold

er's

nam

e Vi

llage

Ta

luk

Dis

tric

t Su

rvey

A

rea

M

iner

al

Con

cess

ion

no.

valid

fr

om

valid

to

No.

a

nd a

ddre

ss

N

o (h

a)

1 K

.T.M

oosa

nkut

ty

Era

mam

Ta

lipar

amba

K

annu

r 6

74/3

0.

0971

G

rani

te

36/1

5-16

/MM

/GS

/CR

PS

/ 20

.11.

15

19.1

1.16

S/o

Ada

mku

tty, K

aniy

arak

kal

Hec

tare

DO

C/M

-448

4/15

Thyk

kand

i, P

.O.N

arat

h 67

0 60

1

D

t 20.

11.2

015

2 M

anag

ing

Dire

ctor

,

Kol

ayad

Th

alas

seri

Kan

nur

70/

1 0.

5 G

rani

te

37/1

5-16

/MM

/GS

/CR

PS

/ 26

.11.

15

25.1

1.16

M

alab

ar C

onst

ruct

ion

Mat

eria

ls

Pvt

.Ltd

.

H

ecta

re

D

OC

/M-5

426/

15

E

daya

r, P

.O.K

olay

ad,

Dt 2

6.11

.201

5

3 Su

dhar

shan

Tr

ipra

ngot

tur

Thal

asse

ri K

annu

r

275/

1A

40.4

7 G

rani

te

38/1

5-16

/MM

/GS

/CR

PS

/ 02

.12.

15

01.1

2.16

S/o

Bal

an, h

eruk

unno

thpa

ram

bath

A

re

D

OC

/M-5

147/

15

H

ouse

, P.O

.Che

rupa

ram

ba 6

70

693

Dt 0

2.12

.201

5

4 V

.K.B

enni

K

olay

ad

Thal

asse

ri K

annu

r

21/1

A1

0.5

Gra

nite

39

/15-

16/M

M/G

S/C

RP

S/

18.1

2.15

17

.12.

16

S

/o K

uriy

akos

e,

Hec

tare

DO

C/M

-536

3/15

V

akka

chal

il H

ouse

, P.O

.Kol

ayad

67

0 65

0

D

t 18.

12.2

015

5 S

haju

Jos

e,

Pay

yavo

or

Talip

aram

ba

Kan

nur

1/1

0.

3 G

rani

te

40/1

5-16

/MM

/GS

/CR

PS

/ 19

.12.

15

18.1

2.16

Man

agin

g P

artn

er,

Hec

tare

DO

C/M

-548

0/15

P

ayya

voor

Cru

sher

s, P

ayya

voor

67

0 63

3

D

t 19.

12.2

015

6 B

ashe

er.K

.P.

Ayy

anku

nnu

Iritty

K

annu

r 12

93

0.5

Gra

nite

41

/15-

16/M

M/G

S/C

RP

S/

11.0

1.16

10

.01.

17

M

anag

ing

Par

tner

, Roc

k S

tar,

Hec

tare

DO

C/M

-556

6/15

Pul

lanp

arat

hattu

, P.O

.Cha

ral

Dt 1

1.01

.201

6

7 S

onia

Bin

oy,

Ayy

anku

nnu

Iritty

K

annu

r 12

93

12

Gra

nite

42

/15-

16/M

M/G

S/C

RP

S/

14.0

1.16

13

.01.

17

D

/o S

ebas

tian,

K

izha

kkep

pada

vath

,

C

ent

D

OC

/M-2

571/

15

P

.O.P

ayam

670

704

D

t 14.

01.2

016

8 K

adek

kara

Ali

Kun

hi

Vel

lad

Talip

aram

ba

Kan

nur

292/

1A

0.14

57

Gra

nite

43

/15-

16/M

M/G

S/C

RP

S/

15.0

1.16

14

.01.

17

S

/o H

ussa

in, K

adek

kara

Hou

se,

Hec

tare

DO

C/M

-261

8/15

P.O

.Eria

m, E

dakk

ome

Dt 1

5.01

.201

6

9 C

.H.A

skar

V

ayat

hur

Iritty

K

annu

r

28/1

A2

0.19

43

Gra

nite

44

/15-

16/M

M/G

S/C

RP

S/

15.0

1.16

14

.01.

17

M

anag

ing

Par

tner

, Hin

dust

an

Sto

ne

Hec

tare

DO

C/M

-358

3/15

Cru

sher

and

Hol

low

Bric

ks U

nit,

Dt 1

5.01

.201

6

P.O

.Kal

lang

i 670

706

10

K.C

.Jam

es,

Eru

vess

i Ta

lipar

amba

K

annu

r 4

0.40

47

Gra

nite

45

/15-

16/M

M/G

S/C

RP

S/

16.0

1.16

15

.01.

17

M

anag

ing

Par

tner

, Eve

rest

Sto

ne

Hec

tare

DO

C/M

-234

3/15

Cru

sher

and

Gra

nite

s, M

.T. 8

9 V

D

t 16.

01.2

016

H

ighw

ay A

rcad

e, K

annu

r

11

Vas

undh

aran

.K.

Per

ingo

me

Talip

aram

ba

Kan

nur

308

/3

0.09

71

Gra

nite

46

/15-

16/M

M/G

S/C

RP

S/

08.0

2.16

07

.02.

17

S

/o K

arun

akar

an,

Hec

tare

DO

C/M

-546

8/15

M

adhu

man

dhira

m, P

.O.P

erin

gom

e 67

0 30

7

D

t 08.

02.2

016

12

K.P

.Yun

as

Thiru

men

i Ta

lipar

amba

K

annu

r 2

84/1

0.

0486

G

rani

te

47/1

5-16

/MM

/GS

/CR

PS

/ 15

.02.

16

14.0

2.17

S/o

E.P

.Mam

mad

Haj

i

286/

1 H

ecta

re

D

OC

/M-5

616/

15

A

kkar

amm

al H

ouse

, P.O

.May

yil

670

602

Dt 1

5.02

.201

6

13

Jabi

r.M.A

. A

lakk

ode

Talip

aram

ba

Kan

nur

17/

1A

4.04

G

rani

te

48/1

5-16

/MM

/GS

/CR

PS

/ 18

.02.

16

17.0

2.17

S/o

Ass

u H

aji,

Mal

likka

ntak

ath,

1 A

re

D

OC

/M-2

503/

15

P

.O.R

ayar

om

Dt 1

8.02

.201

6

14

T.P.

Sha

msu

deen

K

olar

i Iri

tty

Kan

nur

47/

1 0.

0486

G

rani

te

49/1

5-16

/MM

/GS

/CR

PS

/ 24

.02.

16

23.0

2.17

S/o

Aha

mm

ad K

utty

,Gre

en V

illa,

H

ecta

re

D

OC

/M-4

902/

15

K

alar

oad,

P.O

.Kee

cher

i 670

702

D

t 24.

02.2

016

15

V.P

.Pra

bhak

aran

K

anna

vam

Th

alas

seri

Kan

nur

10

8/1A

0.

0971

G

rani

te

50/1

5-16

/MM

/GS

/CR

PS

/ 24

.02.

16

23.0

2.17

Hol

y G

rani

te a

nd B

ricks

(P) L

td.

Hec

tare

DO

C/M

-353

1/15

Eda

yar,

P.O

.Kol

ayad

,

D

t 24.

02.2

016

16

Mav

ilakk

andi

Bal

akris

hnan

, K

ooda

li Th

alas

seri

Kan

nur

3/1

A

0.09

71

Gra

nite

51

/15-

16/M

M/G

S/C

RP

S/

24.0

2.16

23

.02.

17

S

hajin

a N

ivas

, Ves

sala

H

ecta

re

D

OC

/M-2

439/

15

P

.O.C

hattu

kapa

ra 6

70 5

92

Dt 2

4.02

.201

6

17

Man

agin

g D

irect

or,

Ayy

anku

nnu

Iritty

K

annu

r 12

93

0.38

44

Gra

nite

52

/15-

16/M

M/G

S/C

RP

S/

03.0

3.16

02

.03.

17

K

annu

r Jill

a B

lack

Roc

k C

rush

ers

and

Hec

tare

DO

C/M

-548

8/15

San

d M

akin

g In

dust

ries

(P) L

td.,

D

t 03.

03.2

016

K

ouse

r Com

plex

, Kal

tex

Junc

tion

18

A.M

anoh

aran

K

eezh

oor

Iritty

K

annu

r 1

67/2

0.

0444

G

rani

te

53/1

5-16

/MM

/GS

/CR

PS

/ 16

.03.

16

15.0

3.17

S

/o K

unhi

ram

an, S

aras

wat

hi

Nila

yam

H

ecta

re

D

OC

/M-2

567/

15

P

.O.M

anga

ttido

m 6

70 6

43

Dt 1

6.03

.201

6

19

Sun

ny J

ose,

P

ayya

voor

Ta

lipar

amba

K

annu

r 1

/1

0.1

Gra

nite

54

/15-

16/M

M/G

S/C

RP

S/

28.0

3.16

27

.03.

17

M

anag

ing

Par

tner

, Pay

yavo

or

Gra

nite

s

H

ecta

re

D

OC

/M-5

481/

15

P

ayya

voor

D

t 28.

03.2

016

20

Pro

ject

Man

ange

r, K

utto

or

Talip

aram

ba

Kan

nur

74/

1D

0.40

47

Gra

nite

55

/15-

16/M

M/G

S/C

RP

S/

31.0

3.16

30

.03.

17

R

.D.S

.Pro

ject

Ltd

., O

rana

dath

chal

H

ecta

re

D

OC

/M-5

615/

15

P

.O.V

ilaya

nkod

e 67

0 50

4

D

t 31.

03.2

016

21

C.G

.Geo

rge

Trip

rang

ottu

r Th

alas

seri

Kan

nur

27

5/1A

29

.95

Gra

nite

01

/16-

17/M

M/G

S/C

RP

S/

06.0

4.16

05

.04.

17

Jo

int M

anag

ing

Dire

ctor

,

A

re

D

OC

/M-3

96/1

6

C

hend

ayad

Gra

nite

s (P

) Ltd

., K

SID

C

Dt 0

6.04

.201

6

In

dust

rial G

row

th C

entre

, V

aliy

avel

icha

m

22

C.K

.Abd

urah

iman

, P

erin

gom

e Ta

lipar

amba

K

annu

r 30

4/3

0.09

72

Gra

nite

02

/16-

17/M

M/G

S/C

RP

S/

06.0

4.16

05

.04.

17

M

anag

ing

Par

tner

, Per

ingo

me

Sto

ne C

rush

er,

Hec

tare

DO

C/M

-219

9/15

B

aith

ulas

her,

Man

iyoo

r, P

.O.C

hekk

ikul

am

Dt 0

6.04

.201

6

23

Ane

esh

Kum

ar.K

. Th

olam

bra

Thal

asse

ri K

annu

r 1/

1A

0.04

25

Gra

nite

03

/16-

17/M

M/G

S/C

RP

S/

11.0

4.16

10

.04.

17

S

/o M

adha

van,

Mad

hav

Niv

as,

Hec

tare

DO

C/M

-122

7/16

P.O

.Vel

larv

ally

670

673

D

t 11.

04.2

016

24

Man

agin

g D

irect

or,

Nid

iyen

ga

Talip

aram

ba

Kan

nur

3 0.

24

Gra

nite

04

/16-

17/M

M/G

S/C

RP

S/

21.0

4.16

20

.04.

17

S

ampa

th C

rush

ers

Pvt

.Ltd

.

A

cre

D

OC

/M-1

228/

16

C

hepp

aram

b, P

.O.C

hem

beri,

670

63

2

D

t 21.

04.2

016

25

Rav

i Pal

eri

Kol

aval

lur

Thal

asse

ri K

annu

r 58

/1A

1 0.

0971

G

rani

te

05/1

6-17

/MM

/GS

/CR

PS

/ 25

.04.

16

24.0

4.17

Soo

rya

Ston

e C

rush

er

Hec

tare

DO

C/M

-388

0/15

K

allu

vala

ppu,

P.O

.Che

rupa

ram

b 67

0 69

3

D

t 25.

04.2

016

26

K.G

anga

dhar

an

Kut

hupa

ram

ba

Thal

asse

ri K

annu

r 89

0.

0971

G

rani

te

06/1

6-17

/MM

/GS

/CR

PS

/ 04

.05.

16

03.0

5.17

S/o

Kum

aran

, K.G

.Hou

se,

Hec

tare

DO

C/M

-555

6/15

P.O

.Mut

hiye

nga

670

691

Dt 0

4.05

.201

6

27

K.K

hade

r S

ivap

uram

Th

alas

seri

Kan

nur

13

1/1B

0.

0971

G

rani

te

07/1

6-17

/MM

/GS

/CR

PS

/ 04

.05.

16

03.0

5.17

S/o

Moi

deen

, Saj

itha

Man

zil,

Hec

tare

DO

C/M

-466

3/15

P.O

.Siv

apur

am 6

70 7

02

Dt 0

4.05

.201

6

28

Ani

l Jos

eph

Nid

iyen

ga

Talip

aram

ba

Kan

nur

25/

1A

12

Gra

nite

08

/16-

17/M

M/G

S/C

RP

S/

11.0

5.16

10

.05.

17

S

/o J

osep

h, K

uzhi

thot

tu H

ouse

,

C

ent

D

OC

/M-2

710/

15

P

.O.C

hem

bant

hotty

670

631

D

t 11.

05.2

016

29

U.S

aeed

V

ella

d Ta

lipar

amba

K

annu

r

292/

1A

0.09

72

Gra

nite

09

/16-

17/M

M/G

S/C

RP

S/

18.0

5.16

17

.05.

17

S

aj M

ahal

,

H

ecta

re

D

OC

/M-5

799/

15

P

ushp

agiri

, Tal

ipar

amba

670

141

D

t 18.

05.2

016

30

C.G

.Geo

rge

Kan

nava

m

Thal

asse

ri K

annu

r

108/

1C

0.09

71

Gra

nite

10

/16-

17/M

M/G

S/C

RP

S/

25.0

5.16

24

.05.

17

Jo

int M

anag

ing

Dire

ctor

,

H

ecta

re

D

OC

/M-1

567/

16

C

hend

ayad

Gra

nite

s (P

) Ltd

., K

SID

C

Dt 2

5.05

.201

6

In

dust

rial G

row

th C

entre

, V

aliy

avel

icha

m

K

ooth

upar

amb,

P.O

.Mur

iyad

643

67

0

31

P.M

.Ibra

him

P

erin

gom

e Ta

lipar

amba

K

annu

r 3

28/5

0.

0971

G

rani

te

11/1

6-17

/MM

/GS

/CR

PS

/ 01

.06.

16

31.0

5.17

M

anag

ing

Par

tner

, Sou

ther

n G

rani

tes,

H

ecta

re

D

OC

/M-6

006/

15

M

adak

kam

poyi

l, P

erin

gom

e

D

t 01.

06.2

016

32

Jils

on J

osep

h.V

. N

idiy

enga

Ta

lipar

amba

K

annu

r 28

40

G

rani

te

12/1

6-17

/MM

/GS

/CR

PS

/ 15

.06.

16

14.0

6.17

S/o

V.M

.Jos

eph,

Vel

iyat

hil H

ouse

,

A

re

D

OC

/M-1

759/

16

P

.O.P

ulik

kuru

mba

670

582

D

t 15.

06.2

016

33

Jils

on J

osep

h.V

. N

idiy

enga

Ta

lipar

amba

K

annu

r 28

40

G

rani

te

13/1

6-17

/MM

/GS

/CR

PS

/ 15

.06.

16

14.0

6.17

S/o

V.M

.Jos

eph,

Vel

iyat

hil H

ouse

,

A

re

D

OC

/M-1

760/

16

P

.O.P

ulik

kuru

mba

670

582

D

t 15.

06.2

016

34

Sha

ju J

ose,

P

ayya

voor

Ta

lipar

amba

K

annu

r 1

/1

0.19

98

Gra

nite

14

/16-

17/M

M/G

S/C

RP

S/

16.0

6.16

15

.06.

17

M

anag

ing

Par

tner

,

H

ecta

re

D

OC

/M-1

678/

16

P

ayya

voor

Cru

sher

s, P

ayya

voor

67

0 63

3

D

t 16.

06.2

016

35

Siri

l Jos

e,

Nid

iyen

ga

Talip

aram

ba

Kan

nur

3 73

G

rani

te

15/1

6-17

/MM

/GS

/CR

PS

/ 22

.06.

16

21.0

6.17

M

anag

ing

Dire

ctor

, Sam

path

C

rush

ers

C

ent

D

OC

/M-5

576/

16

(P

) Ltd

., N

idiy

enga

, P.O

.Che

mbe

ri 67

0 63

2

D

t 22.

06.2

016

36

Aby

Abr

aham

Tr

ipra

ngot

tur

Thal

asse

ri K

annu

r

275/

1A

0.49

9 G

rani

te

16/1

6-17

/MM

/GS

/CR

PS

/ 22

.09.

16

21.0

9.17

S

/o M

.A.A

brah

am, A

nugr

ah, K

isan

R

oad

Hec

tare

DO

C/M

-200

7/16

P.O

.Ala

vil 6

70 0

08

Dt 2

2.09

.201

6

37

San

ny C

yria

c V

ayat

hur

Iritty

K

annu

r

28/1

A2

0.3

Gra

nite

17

/16-

17/M

M/G

S/C

RP

S/

26.0

9.16

25

.09.

17

S

/o C

yria

c M

athe

w, P

otta

ngal

H

ouse

,

H

ecta

re

D

OC

/M-8

03/1

6

Thon

diyi

l.P.O

. 670

673

D

t 26.

09.2

016

38

Javi

d.E

.P.,

Nid

iyen

ga

Talip

aram

ba

Kan

nur

1/1

24

G

rani

te

18/1

6-17

/MM

/GS

/CR

PS

/ 26

.09.

16

25.0

9.17

S/o

Moi

deen

.V.P

., S

anth

i Mah

al

Cen

t

DO

C/M

-521

2/15

Che

kkik

ulam

.P.O

. 670

592

D

t 26.

09.2

016

39

Mah

esh.

C.M

. K

anic

har

Iritty

K

annu

r 1

56/1

0.

0971

G

rani

te

19/1

6-17

/MM

/GS

/CR

PS

/ 29

.09.

16

28.0

9.17

M

anag

ing

Par

tner

, Sre

elak

shm

i S

tone

H

ecta

re

D

OC

/M-3

612/

15

C

rush

er, 2

7th

Mile

, P

.O.P

oola

kkut

ty 6

70 6

50

Dt 2

9.09

.201

6

40

Raj

esh.

T.S

. E

ruve

ssi

Talip

aram

ba

Kan

nur

5 36

G

rani

te

20/1

6-17

/MM

/GS

/CR

PS

/ 31

.10.

16

30.1

0.17

S

/o T

.R.S

ukum

aran

, Th

amar

asse

riyil

Hou

se,

Cen

t

DO

C/M

-397

2/16

P.O

.Kud

iyan

mal

a 67

0 58

2

D

t 31.

10.2

016

41

Rav

i Pal

eri

Kol

aval

lur

Thal

asse

ri K

annu

r 1

50/3

0.

0971

G

rani

te

21/1

6-17

/MM

/GS

/CR

PS

/ 07

.11.

16

06.1

1.17

S

urya

Sto

ne C

rush

er a

nd H

ollo

w

Bric

ks,

H

ecta

re

D

OC

/M-5

330/

15

P

.O.C

heru

para

mb,

670

693

D

t 07.

11.2

016

Tab

le 2

c: L

ist o

f Qua

rryi

ng P

erm

it gr

ante

d fo

r L

ater

ite b

uild

ing

ston

e Sl

. C

once

ssio

n ho

lder

's n

ame

Vi

llage

Ta

luk

Surv

ey

Are

a

Con

cess

ion

no.

valid

to

No

and

addr

ess

no

(ha)

1

Raj

u Th

atto

ttu

Thille

nker

i Iri

tty

28/

4 0.

0972

41

0/15

-16/

MM

/LT/

CR

PS/

18.1

1.16

S/o

Kun

hira

man

, Jis

ha N

ivas

,

2

7/2

Hec

tare

D

OC

/M-5

357/

15

P.O

.Eru

vatti

670

647

D

t 19.

11.2

015

2

Sun

il

Muz

hakk

unnu

Iri

tty

1/1

0.

0971

41

1/15

-16/

MM

/LT/

CR

PS/

18.1

1.16

S/o

Gop

alan

, Kee

rthan

a,

H

ecta

re

DO

C/M

-244

6/15

P

.O.S

ivap

uram

670

702

D

t 19.

11.2

015

3

Bab

u.P

. P

erin

that

ta

Talip

aram

ba

16

0.09

71

412/

15-1

6/M

M/L

T/C

RPS

/ 18

.11.

16

S

/o K

unhi

kann

an, P

alan

gattu

Hou

se,

H

ecta

re

DO

C/M

-521

1/15

P

erin

that

ta 6

70 3

07

Dt 1

9.11

.201

5

4 P

anne

ri R

ames

han

Ram

anth

ali

Talip

aram

ba

183

/2

0.09

71

413/

15-1

6/M

M/L

T/C

RPS

/ 22

.11.

16

S

/o K

oran

Mou

vann

al

H

ecta

re

DO

C/M

-434

0/15

P

anne

ri H

ouse

, P.O

.Kar

anth

att 6

70 3

08

Dt 2

3.11

.201

5

5 V

ijaya

n.N

.K.

Ram

anth

ali

Talip

aram

ba

185

/1

0.09

71

414/

15-1

6/M

M/L

T/C

RPS

/ 22

.11.

16

S

/o P

.V.K

rishn

an

H

ecta

re

DO

C/M

-434

6/15

N

aran

gaku

lang

ara

Hou

se,

P.O

.Kar

anth

attu

67

0 30

8

D

t 23.

11.2

015

6

Muk

ri M

aham

ood

Kan

kol

Talip

aram

ba

335

/1

0.09

71

415/

15-1

6/M

M/L

T/C

RPS

/ 22

.11.

16

M

ukri

Hou

se, T

hayi

neri,

3

35/2

H

ecta

re

DO

C/M

-519

3/15

P

.O.P

ayya

nnur

670

307

D

t 23.

11.2

015

7

Tham

ban.

P.P

. A

lapp

adam

b Ta

lipar

amba

4

78/1

0.

0972

41

6/15

-16/

MM

/LT/

CR

PS/

22.1

1.16

S/o

Ram

an, P

uthi

ya P

uray

il H

ouse

,

Hec

tare

D

OC

/M-5

193/

15

P.O

.Pot

havo

or 6

70 3

13

Dt 2

3.11

.201

5

8 K

unhi

ram

an.P

.V.

Pan

niyo

or

Talip

aram

ba

1/1

B

0.09

72

417/

15-1

6/M

M/L

T/C

RPS

/ 24

.11.

16

S

/o K

unha

ppa,

Put

hiya

Val

appi

l Hou

se,

H

ecta

re

DO

C/M

-536

1/15

P

.O.K

urum

atho

or 6

70 1

42

Dt 2

5.11

.201

5

9 H

aris

chan

dran

.M.V

. P

anni

yoor

Ta

lipar

amba

1

/1B

0.

0972

41

8/15

-16/

MM

/LT/

CR

PS/

24.1

1.16

S/o

San

kara

n N

air,

Hec

tare

D

OC

/M-5

362/

15

Mel

edat

h H

ouse

, P.O

.Pan

niyo

or

Dt 2

5.11

.201

5

10

Pav

ithra

n.K.

Ta

lipar

amba

Ta

lipar

amba

1

/1

24

419/

15-1

6/M

M/L

T/C

RPS

/ 24

.11.

16

S

/o K

unhi

kora

n

Cen

t D

OC

/M-4

300/

15

Kiz

hakk

eppa

dath

Hou

se, P

.O.T

alip

aram

ba

Dt 2

5.11

.201

5

11

Kan

nur K

allu

koth

u Th

ozhi

lali

Ksh

ema

C

huzh

ali

Talip

aram

ba

222

0.09

72

420/

15-1

6/M

M/L

T/C

RPS

/ 24

.11.

16

S

ahak

aran

a S

anga

m L

t.,D

herm

asal

a,

H

ecta

re

DO

C/M

-514

5/15

P

.O.P

aras

sini

kkad

avu

670

563

Dt 2

5.11

.201

5

12

Sun

eesh

P

anni

yoor

Ta

lipar

amba

13

7 0.

0972

42

1/15

-16/

MM

/LT/

CR

PS/

24.1

1.16

S/o

Bha

skar

an, A

niya

nkot

tu H

ouse

,

Hec

tare

D

OC

/M-5

354/

15

P.O

.Koy

yam

670

142

D

t 25.

11.2

015

13

B

alak

rishn

an.K

. Th

imiri

Ta

lipar

amba

1

00/2

A

24

422/

15-1

6/M

M/L

T/C

RPS

/ 24

.11.

16

K

ayak

kil H

ouse

,

Cen

t D

OC

/M-4

019/

15

P.O

.Chu

zhal

i 670

142

D

t 25.

11.2

015

14

M

anik

anda

n E

ram

am

Talip

aram

ba

469

0.09

71

423/

15-1

6/M

M/L

T/C

RPS

/ 29

.11.

16

S

/o G

ovin

da P

oduv

al

H

ecta

re

DO

C/M

-405

2/15

K

anuv

atiy

il, P

.O.K

ando

th

Dt 3

0.11

.201

5

15

M.R

ajan

A

lapp

adam

b Ta

lipar

amba

4

78/1

0.

0972

42

4/15

-16/

MM

/LT/

CR

PS/

29.1

1.16

S/o

Ram

an, C

halu

vala

ppil

Hou

se,

H

ecta

re

DO

C/M

-528

3/15

P

.O.T

him

iri 6

70 3

14

Dt 3

0.11

.201

5

16

Rag

hava

n.D

. P

anap

uzha

K

annu

r 1

/1

0.09

71

425/

15-1

6/M

M/L

T/C

RPS

/ 29

.11.

16

S

/o K

unhi

ram

an,

H

ecta

re

DO

C/M

-438

5/15

D

herm

al H

ouse

, P.O

.Pila

thar

a

D

t 30.

11.2

015

17

G

anga

dhar

an.

Per

inth

atta

Ta

lipar

amba

1

32/1

A

0.09

71

426/

15-1

6/M

M/L

T/C

RPS

/ 01

.12.

16

S

/o K

unhi

ram

an, P

uthi

ya V

eetti

l Hou

se,

H

ecta

re

DO

C/M

-476

7/15

P

.O.K

utto

or 6

70 3

06

Dt 0

2.12

.201

5

18

Moh

anan

.P.T

. A

lapp

adam

b Ta

lipar

amba

4

88/2

0.

0972

42

7/15

-16/

MM

/LT/

CR

PS/

01.1

2.16

Pal

eri T

haiv

alap

pil,

P.O

.Ola

tt

Hec

tare

D

OC

/M-5

265/

15

Via

Thr

ikka

ripur

, Kar

sarg

od 6

71 3

10

Dt 0

2.12

.201

5

19

Kun

hika

nnan

Tr

ipra

ngot

tur

Thal

asse

ri 1

58/2

9.

71

428/

15-1

6/M

M/L

T/C

RPS

/ 01

.12.

16

S

/o K

oran

,

A

re

DO

C/M

-557

5/15

S

ivam

Bha

van,

P.O

.Put

hoor

D

t 02.

12.2

015

20

R

ajee

van.

A.

Kut

tiatto

or

Talip

aram

ba

76/

3 0.

0971

42

9/15

-16/

MM

/LT/

CR

PS/

01.1

2.16

S/o

Ach

utha

n, A

riyam

batt

Hou

se,

H

ecta

re

DO

C/M

-398

9/15

P

.O.N

arat

h 67

0 60

3

D

t 02.

12.2

015

21

Sur

esha

n.V

.P.

Ala

ppad

amb

Talip

aram

ba

478

/1

0.09

71

430/

15-1

6/M

M/L

T/C

RPS

/ 06

.12.

16

S

/o A

mbr

onte

Am

bu, V

adak

kepo

yil H

ouse

,

Hec

tare

D

OC

/M-5

284/

15

P.O

.Kot

akka

d, K

asar

god

671

310

Dt 0

7.12

.201

5

22

Pur

usho

tham

an.M

. K

allia

d Iri

tty

23/

1 0.

24

431/

15-1

6/M

M/L

T/C

RPS

/ 06

.12.

16

S

/o K

unhi

kann

an,

Mad

appu

ra H

ouse

,

Acr

e D

OC

/M-5

543/

15

Ura

thur

, P.O

.Kos

avan

vaya

l 670

593

D

t 07.

12.2

015

23

S

anth

osh

Kum

ar.K

. C

hava

sser

i Iri

tty

105

0.09

71

432/

15-1

6/M

M/L

T/C

RPS

/ 06

.12.

16

S

/o K

utta

n, P

adm

alay

am, P

.O. V

enga

Hec

tare

D

OC

/M-4

475/

15

Sha

stha

mko

tta, K

olla

m

Dt 0

7.12

.201

5

24

Raj

esh.

P.

Per

inth

atta

Ta

lipar

amba

4

5/1

0.09

71

433/

15-1

6/M

M/L

T/C

RPS

/ 06

.12.

16

S

/o N

aray

anan

, Par

ukka

ran

Hou

se,

H

ecta

re

DO

C/M

-557

3/15

P

.O.P

urak

kunn

u 67

0 30

6

D

t 07.

12.2

015

25

S

anth

osh

Kum

ar.T

. K

utto

or

Talip

aram

ba

131

/1A

1 0.

0971

43

4/15

-16/

MM

/LT/

CR

PS/

06.1

2.16

S/o

Pat

hman

abha

n, T

hant

hray

i Hou

se,

H

ecta

re

DO

C/M

-466

2/15

M

aila

nche

ri, P

.O.K

utto

or

Dt 0

7.12

.201

5

26

Ash

okan

.K.

Per

inth

atta

Ta

lipar

amba

4

6/1A

0.

0971

43

5/15

-16/

MM

/LT/

CR

PS/

06.1

2.16

S/o

Kun

hika

nnan

Hec

tare

D

OC

/M-3

992/

15

Kat

toor

Hou

se, P

.O.P

orak

kunn

u 67

0 30

6

D

t 07.

12.2

015

27

H

arid

as.N

.P.

Ram

anth

ali

Talip

aram

ba

22

0.09

71

436/

15-1

6/M

M/L

T/C

RPS

/ 06

.12.

16

S

/o M

.Dam

odha

ran,

Hec

tare

D

OC

/M-4

235/

15

Nad

uvile

Pur

ayil,

P.O

.Pal

akko

de 6

70 3

05

Dt 0

7.12

.201

5

28

Rag

hava

n.P.

V.

Kan

kol

Talip

aram

ba

258

/3

0.09

71

437/

15-1

6/M

M/L

T/C

RPS

/ 08

.12.

16

S

/o A

mbu

, Put

hen

Veet

til,

H

ecta

re

DO

C/M

-561

2/15

P

.O.C

hala

kkod

e 67

0 30

7

D

t 09.

12.2

015

29

Jo

hn

Kel

akom

Iri

tty

kpd

260

/1

0.09

7 43

8/15

-16/

MM

/LT/

CR

PS/

08.1

2.16

S/o

Joh

n, C

heru

sser

i Hou

se,

H

ecta

re

DO

C/M

-546

9/15

P

.O.C

hetti

yam

para

mb

670

674

Dt 0

9.12

.201

5

30

Suv

arna

n.P

.V.

Per

inth

atta

Ta

lipar

amba

76

/2

0.09

71

439/

15-1

6/M

M/L

T/C

RPS

/ 08

.12.

16

S

/o K

unha

ppan

, Put

hiya

Vee

ttil H

ouse

,

Hec

tare

D

OC

/M-4

638/

15

P.O

.Kut

toor

670

306

D

t 09.

12.2

015

31

Th

omas

.K.K

. E

ruve

ssi

Talip

aram

ba

64/

2 0.

0931

44

0/15

-16/

MM

/LT/

CR

PS/

08.1

2.16

S/o

Kur

iyan

, Kuz

him

ullil

Hou

se,

H

ecta

re

DO

C/M

-448

0/15

E

ruve

ssi,

P.O

.Chu

ndak

unnu

670

632

D

t 09.

12.2

015

32

A

bdul

Naz

ar.C

.K.

Nid

iyen

ga

Talip

aram

ba

4 0.

0971

44

1/15

-16/

MM

/LT/

CR

PS/

08.1

2.16

S

/o M

uham

med

, C

.K.H

ouse

,

Hec

tare

D

OC

/M-4

946/

15

P.O

.Mal

appa

ttam

670

631

D

t 09.

12.2

015

33

R

athe

esh

Phi

lip

Eru

vess

i Ta

lipar

amba

57

24

44

2/15

-16/

MM

/LT/

CR

PS/

13.1

2.16

S/o

Pai

li, V

anjip

uray

il H

ouse

,

Cen

t D

OC

/M-4

564/

15

P.O

.Nel

likut

ty 6

70 6

32

Dt 1

4.12

.201

5

34

Ane

esh

Kum

ar.C

. S

reek

anda

pura

m

Talip

aram

ba

252

/5

0.09

71

443/

15-1

6/M

M/L

T/C

RPS

/ 13

.12.

16

S

/o K

.Kun

ham

bu,

H

ecta

re

DO

C/M

-494

5/15

C

hath

oth

Hou

se, P

.O.M

alap

patta

m 6

70 6

31

Dt 1

4.12

.201

5

35

San

thos

h.V.

V.

Eru

vess

i Ta

lipar

amba

10

9/1A

48

44

4/15

-16/

MM

/LT/

CR

PS/

13.1

2.16

S/o

Kris

hnan

Nam

biar

,

Cen

t D

OC

/M-4

944/

15

Vel

luva

Vee

ttil,

P.O

.Kai

thap

ram

670

631

D

t 14.

12.2

015

36

S

uren

dran

.V.V

. N

idiy

enga

Ta

lipar

amba

30

24

44

5/15

-16/

MM

/LT/

CR

PS/

13.1

2.16

S/o

Nar

ayan

an

C

ent

DO

C/M

-574

9/15

V

aliy

a V

alap

pil

Hou

se,

P.O

.Nid

iyen

ga 6

70

631

Dt 1

4.12

.201

5

37

Jose

V.S

. P

adiy

oor

Iritty

5

1/1

0.09

71

446/

15-1

6/M

M/L

T/C

RPS

/ 13

.12.

16

S

/o S

teep

hen,

Val

lark

attil

Hou

se,

H

ecta

re

DO

C/M

-541

6/15

K

allu

vaya

l, P

.O.P

adiy

oor 6

70 7

03

Dt 1

4.12

.201

5

38

Sun

il K

umar

Pad

inha

kkar

a Th

imiri

Ta

lipar

amba

1

00/2

A

24

447/

15-1

6/M

M/L

T/C

RPS

/ 13

.12.

16

P

adin

hakk

ara

Hou

se,

C

ent

DO

C/M

-328

8/15

P

.O.K

arip

pal 6

70 5

81

Dt 1

4.12

.201

5

39

San

esh

Chu

zhal

i Ta

lipar

amba

72

/1A

1 0.

0972

44

8/15

-16/

MM

/LT/

CR

PS/

13.1

2.16

S/o

Jan

ardh

anan

, Vay

a V

eetti

l,

Hec

tare

D

OC

/M-3

149/

15

Kol

atho

or, C

huzh

ali.P

.O. 6

70 1

41

Dt 1

4.12

.201

5

40

Jana

rdha

nan.

P.V

. Th

illenk

eri

Iritty

64

0.

0678

44

9/15

-16/

MM

/LT/

CR

PS/

15.1

2.16

S/o

Kam

mar

an N

air,

H

ecta

re

DO

C/M

-574

5/15

S

reen

ilaya

m, P

.O.T

hille

nger

i 670

702

D

t 16.

12.2

015

41

M

eri K

uriy

an

Eru

vess

i Ta

lipar

amba

1

09/1

A

0.09

71

450/

15-1

6/M

M/L

T/C

RPS

/ 15

.12.

16

D

/o K

uriy

an

H

ecta

re

DO

C/M

-500

1/15

K

uzhi

mul

lil H

ouse

, P

.O.C

hund

akun

nu 6

70

632

Dt 1

6.12

.201

5

42

Unn

ikris

hnan

.K.K

. N

idiy

enga

Ta

lipar

amba

42

24

45

1/15

-16/

MM

/LT/

CR

PS/

15.1

2.16

S/o

App

u N

ambi

ar, K

rishn

a K

ripa,

Cen

t D

OC

/M-5

651/

15

Vel

am, P

.O.M

ayyi

l 670

602

D

t 16.

12.2

015

43

E

.P.S

hara

fudh

een

Kal

liad

Iritty

4

6/4

0.09

71

452/

15-1

6/M

M/L

T/C

RPS

/ 20

.12.

16

S

/o A

bdul

Rah

iman

, Sub

aida

Man

zil,

H

ecta

re

DO

C/M

-562

4/15

P

.O.M

ayyi

l 670

602

D

t 21.

12.2

015

44

R

eji.V

.J.

Pay

yavo

or

Talip

aram

ba

1/1

0.

1943

45

3/15

-16/

MM

/LT/

CR

PS/

20.1

2.16

S/o

Jos

eph,

Vat

hil K

unne

l Hou

se,

H

ecta

re

DO

C/M

-528

8/15

P

.O.T

hond

ayil,

Via

. Per

avoo

r 670

673

D

t 21.

12.2

015

45

R

avee

ndra

.K.P

. A

lapp

adam

b Ta

lipar

amba

11

0.

0971

45

4/15

-16/

MM

/LT/

CR

PS/

20.1

2.16

S/o

Kun

happ

an, K

uttip

urat

h H

ouse

,

Hec

tare

D

OC

/M-5

209/

15

P.O

.Pad

iyot

tuch

al 6

70 3

07

Dt 2

1.12

.201

5

46

P.P

ram

od

Per

inth

atta

Ta

lipar

amba

1

32/1

A

0.48

56

455/

15-1

6/M

M/L

T/C

RP

S/

21.1

2.16

S/o

Bal

an, K

.K.P

aram

b H

ouse

,

Hec

tare

D

OC

/M-5

533/

15

P.O

.Man

gatti

dam

670

643

D

t 22.

12.2

015

47

R

athe

esh.

K.V

. K

orom

Ta

lipar

amba

1

06/3

24

45

6/15

-16/

MM

/LT/

CR

PS/

22.1

2.16

S/o

K.T

.Kar

unak

aran

Cen

t D

OC

/M-5

867/

15

Ala

kkat

t, P

.O.K

anko

l 670

307

D

t 23.

12.2

015

48

M

anoj

Kum

ar.K

. P

ayam

Iri

tty

84

0.09

71

457/

15-1

6/M

M/L

T/C

RPS

/ 22

.12.

16

S

/o D

amu,

Kar

uvat

h H

ouse

,

Hec

tare

D

OC

/M-5

742/

15

P.O

.Man

anth

eri 6

70 6

43

Dt 2

3.12

.201

5

49

Mah

esh.

K.P

. K

anko

l Ta

lipar

amba

1

83/3

0.

0575

45

8/15

-16/

MM

/LT/

CR

PS/

22.1

2.16

S/o

V.V

.Kris

hna

Podu

val,K

unna

th M

anay

il

H

ecta

re

DO

C/M

-579

5/15

P

ayya

daka

th H

ouse

, P.O

.Kan

kol 6

70 3

07

Dt 2

3.12

.201

5

50

Sas

heen

dran

.V.C

. K

allia

d Iri

tty

46/

4 0.

24

459/

15-1

6/M

M/L

T/C

RPS

/ 22

.12.

16

S

/o

V.V

elay

udha

n,

Val

iyar

amba

thch

alil

Hou

se,

A

cre

DO

C/M

-465

9/15

P

.O.P

avan

door

, Koz

hiko

de 6

73 6

13

Dt 2

3.12

.201

5

51

Jasi

m.K

.K.

Kal

liad

Iritty

2

3/1

0.19

42

460/

15-1

6/M

M/L

T/C

RPS

/ 22

.12.

16

S

/o

Kunh

abdu

lla

Haj

i, K

unnd

ukan

dath

il H

ouse

,

Hec

tare

D

OC

/M-5

492/

15

P.O

.Pen

mer

ipar

amba

il, K

ozhi

kode

673

542

D

t 23.

12.2

015

52

M

ajee

d P

atta

r Kad

aval

K

allia

d Iri

tty

46/

4 0.

0971

46

1/15

-16/

MM

/LT/

CR

PS/

22.1

2.16

S/o

Kun

hiko

ya, P

atta

rkad

avan

Hou

se,

H

ecta

re

DO

C/M

-542

9/15

P

.O.P

atta

rkad

av, M

alap

pura

m 6

76 5

19

Dt 2

3.12

.201

5

53

Ham

za K

utty

.P.P

. K

allia

d Iri

tty

46/

4 0.

0971

46

2/15

-16/

MM

/LT/

CR

PS/

22.1

2.16

S/o

Moi

du, P

anni

yam

kand

i Put

hiya

Pur

ayil

H

ecta

re

DO

C/M

-585

7/15

H

ouse

, P.O

.Kol

ache

ri 67

0 60

1

D

t 23.

12.2

015

54

R

iyas

.K.

Kal

liad

Iritty

1

0.09

71

463/

15-1

6/M

M/L

T/C

RPS

/ 22

.12.

16

S

/o M

uham

med

, Riy

as M

anzi

l

Hec

tare

D

OC

/M-5

824/

15

P.O

.Eda

yann

ur 6

70 5

95

Dt 2

3.12

.201

5

55

Yak

hoob

.M.

Kal

liad

Iritty

4

6/4

0.48

46

4/15

-16/

MM

/LT/

CR

PS

/ 22

.12.

16

S

/o K

amal

Haj

i.E.P

.

Acr

e D

OC

/M-5

856/

15

Fird

ous

Man

zil,

P.O

.Ela

mba

ra 6

70 5

95

Dt 2

3.12

.201

5

56

Saj

esh

Bha

rath

an

Kee

zhur

Iri

tty

48

0.09

71

465/

15-1

6/M

M/L

T/C

RPS

/ 22

.12.

16

S

/o B

hara

than

, San

thos

h,

H

ecta

re

DO

C/M

-545

3/15

P

.O.T

hala

sser

i 670

101

D

t 23.

12.2

015

57

P

rath

osh.

P.

Kal

liad

Iritty

4

6/4

0.09

71

466/

15-1

6/M

M/L

T/C

RPS

/ 27

.12.

16

S

/o P

rem

araj

an, P

ayat

t Hou

se,

H

ecta

re

DO

C/M

-514

4/15

P

.O.P

atta

nnur

670

595

D

t 28.

12.2

015

58

P

raka

san.

P.

Kan

kol

Talip

aram

ba

200

0.09

71

467/

15-1

6/M

M/L

T/C

RPS

/ 27

.12.

16

S

/o C

hant

huku

tty N

ambi

ar,

H

ecta

re

DO

C/M

-586

5/15

P

ayya

daka

th H

ouse

, P.O

.Kan

kol 6

70 3

07

Dt 2

8.12

.201

5

59

Sus

hobh

Kon

gatt

Cha

vass

eri

Iritty

3

0.09

71

468/

15-1

6/M

M/L

T/C

RPS

/ 27

.12.

16

S

/o K

.Suk

umar

an, S

usha

nth

Niv

as,

H

ecta

re

DO

C/M

-586

4/15

P

.O.S

ivap

uram

670

702

D

t 28.

12.2

015

60

M

uham

med

Asl

am.P

.P.

Pay

am

Iritty

3

/1B

0.

0971

46

9/15

-16/

MM

/LT/

CR

PS/

27.1

2.16

S/o

Abd

ulla

, T.C

.Niv

as,

H

ecta

re

DO

C/M

-596

5/15

P

.O.N

irmal

agiri

670

701

D

t 28.

12.2

015

61

P

rajit

h Ku

mar

.K.

Kal

liad

Iritty

3

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0.09

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470/

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16

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utty

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Cha

vass

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09/1

0.

0971

47

1/15

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PS/

29.1

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S/o

Moi

deen

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hina

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zil

H

ecta

re

DO

C/M

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.O.K

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702

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12.2

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63

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ishn

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umar

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71

472/

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16

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5

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as.P

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ram

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15

473/

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16

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ouse

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85

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5

65

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0.

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474/

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16

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475/

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16

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onth

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ecta

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.O.M

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31

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67

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72

476/

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anna

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cre

DO

C/M

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appi

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17

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osep

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ecta

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anth

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479/

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17

S

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opi,

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mat

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Hou

se,

H

ecta

re

DO

C/M

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P

.O.C

heru

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670

650

Dt 1

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6

71

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ndra

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ga

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29

0.09

71

480/

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17

S

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unha

mbu

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l Hou

se,

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ecta

re

DO

C/M

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.O.C

heng

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31

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6

72

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l Kum

ar.P

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anth

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ri 2

97/1

0.

0971

48

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MM

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S/o

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amba

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oray

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se,

H

ecta

re

DO

C/M

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lank

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92

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6

73

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anan

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297

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71

482/

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17

S

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anu,

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ivas

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74

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avee

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n M

anan

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25/

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0971

48

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MM

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1.17

S/o

Nar

ayan

an,

H

ecta

re

DO

C/M

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3/15

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oone

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ivas

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70 7

02

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6

75

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48

484/

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17

S

/o K

elu

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orik

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se,

H

ecta

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DO

C/M

-579

7/15

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.O.K

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70 1

41

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6

76

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ya K

umar

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aram

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22

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48

485/

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17

S

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ouse

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tare

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OC

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796/

15

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.O.K

angi

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70 1

42

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8.01

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6

77

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n.P.

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anni

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lipar

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3

1/1

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72

486/

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17

S

/o B

alan

, Pul

ikku

nnil

Hou

se,

H

ecta

re

DO

C/M

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16

P.O

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umat

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670

142

D

t 18.

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016

78

H

amsa

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. K

allia

d Iri

tty

46/

4 0.

0971

48

7/15

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MM

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CR

PS/

17.0

1.17

S/o

V.V

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tare

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OC

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01/1

6

A

raya

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l Hou

se, K

allia

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70 5

93

Dt 1

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6

79

San

thos

h.P.

P.

Nid

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ga

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aram

ba

5 0.

0971

48

8/15

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MM

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CR

PS/

17.0

1.17

S/o

Kan

nan,

Put

hiya

Pur

ayil

Hou

se,

H

ecta

re

DO

C/M

-143

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P.O

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aral

am 6

70 6

02

Dt 1

8.01

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6

80

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il K

umar

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Kal

liad

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3/1

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71

489/

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6/M

M/L

T/C

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17

S

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agha

van

Cha

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OC

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754/

15

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il N

ivas

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70 6

02

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6

81

Mun

eer K

aniy

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zhal

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lipar

amba

2

23/2

0.

0972

49

0/15

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MM

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CR

PS/

17.0

1.17

S/o

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ty H

assa

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D

OC

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637/

15

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aniy

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alap

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6

82

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kasa

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anko

l Ta

lipar

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1

63/3

0.

0603

49

1/15

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MM

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CR

PS/

19.0

1.17

S/o

Dam

odha

ran,

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ttayi

re H

ouse

,

Hec

tare

D

OC

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092/

15

P.O

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670

521

Dt 2

0.01

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6

83

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amm

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unhi

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adan

appa

lli

Kan

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84/

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0.09

71

492/

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6/M

M/L

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17

S

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zain

ar,A

njila

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ouse

,

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D

OC

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743/

15

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1

D

t 20.

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016

84

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unil

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as

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veri

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ba

145

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24

493/

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M/L

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17

S

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hom

as, P

uthu

ppar

ambi

l Hou

se,

188

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t D

OC

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anda

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dav

670

706

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6

85

Pre

man

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. M

anan

ther

i Th

alas

seri

41/

2 0.

0971

49

4/15

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MM

/LT/

CR

PS/

24.0

1.17

S/o

Nan

u, K

rishn

ajan

am

H

ecta

re

DO

C/M

-200

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P.O

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anth

eri 6

70 6

43

Dt 2

5.01

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6

86

Rag

hava

n M

oola

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Man

anth

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asse

ri 2

97/1

0.

0971

49

5/15

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MM

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CR

PS/

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1.17

S/o

Kan

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ouse

,

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tare

D

OC

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747/

15

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ttarip

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ba 6

70 6

50

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5.01

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6

87

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deep

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4

3/2

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72

496/

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17

S

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reed

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ande

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ivas

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tare

D

OC

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935/

15

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umat

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t 25.

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88

Sha

ji.A

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Put

hur

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asse

ri 1

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24

49

7/15

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MM

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mba

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ouse

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t D

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987/

15

P.O

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hiye

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6

89

Sha

ji.V

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Put

hur

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asse

ri 1

51/1

24

49

8/15

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MM

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CR

PS/

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1.17

S/o

M.R

amac

hand

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ent

DO

C/M

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4/15

A

thol

imm

al H

ouse

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anth

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43

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6

90

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ath

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sh

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am

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71

499/

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17

S

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alan

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ath

Hou

se,

H

ecta

re

DO

C/M

-86/

16

P.O

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nako

ttoor

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hiko

de 6

75 5

09

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5.01

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6

91

Mad

hu.P

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hur

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asse

ri 8

24

500/

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17

S

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anar

an, P

aray

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amba

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ouse

,

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t D

OC

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097/

15

Kal

luva

lapp

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.O.C

heru

vanc

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670

650

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5.01

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6

92

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il.P

. M

uzha

kkun

nu

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1

91/3

0.

0971

50

1/15

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MM

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CR

PS/

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1.17

S/o

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ran,

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dhya

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van

H

ecta

re

DO

C/M

-582

8/15

P

.O.M

atta

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670

702

D

t 25.

01.2

016

93

B

iju.V

. M

uzha

kkun

nu

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20

6 0.

1943

50

2/15

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MM

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CR

PS

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.01.

17

S

/o A

ndi,

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vayi

l Hou

se,

H

ecta

re

DO

C/M

-579

3/15

P

.O.K

olar

i 670

702

D

t 25.

01.2

016

94

M

anoj

Kum

ar.K

. M

anan

ther

i Th

alas

seri

41/

2 0.

0971

50

3/15

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MM

/LT/

CR

PS/

26.0

1.17

S/o

Dam

u, K

aruv

ath

Hou

se,

H

ecta

re

DO

C/M

-602

7/15

P

.O.M

anan

ther

i 670

643

D

t 27.

01.2

016

95

G

eorg

e K

utty

E

ruve

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aram

ba

57

24

504/

15-1

6/M

M/L

T/C

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17

S

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brah

am, A

ncha

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al H

ouse

,

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t D

OC

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.O.E

ruve

ssi 6

70 6

32

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6

96

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amac

hand

ran

Kee

zhal

lur

Thal

asse

ri 39

0.

1942

50

5/15

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MM

/LT/

CR

PS/

26.0

1.17

S/o

Kris

hnan

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biar

,

Hec

tare

D

OC

/M-5

354/

15

K

rishn

a N

ivas

, K

othe

ri, P

.O.M

atta

nnur

670

70

2

D

t 27.

01.2

016

97

Ja

mes

Joh

n M

anat

hana

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tty

57/

1A

0.09

71

506/

15-1

6/M

M/L

T/C

RPS

/ 26

.01.

17

S

/o J

ohn,

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limoo

ttil H

ouse

,

Hec

tare

D

OC

/M-5

565/

15

P.O

.Kan

icha

r 670

674

D

t 27.

01.2

016

98

N

aray

anan

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. K

olac

heri

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aram

ba

20

0.09

71

507/

15-1

6/M

M/L

T/C

RPS

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17

S

/o K

anna

n.E

.V.

H

ecta

re

DO

C/M

-568

3/15

K

attil

Hou

se, P

.O.M

ayyi

l

D

t 03.

02.2

016

99

A

nu R

aj R

ayar

oth

Man

anth

eri

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asse

ri 4

1/2

0.09

71

508/

15-1

6/M

M/L

T/C

RPS

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17

N

anda

nam

,

Hec

tare

D

OC

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032/

15

P.O

.Chi

ttarip

aram

ba 6

70 6

50

Dt 0

3.02

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6

100

Raj

u.P.

M

anan

ther

i Th

alas

seri

41/

2 0.

0971

50

9/15

-16/

MM

/LT/

CR

PS/

02.0

2.17

S/o

Gov

inda

n, K

aith

akka

l Hou

se,

H

ecta

re

DO

C/M

-203

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P.O

.Man

anth

eri 6

70 6

43

Dt 0

3.02

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6

101

Ham

za.K

.P.

Chu

zhal

i Ta

lipar

amba

3

83/4

0.

0971

51

0/15

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MM

/LT/

CR

PS/

02.0

2.17

S/o

Moi

deen

, Kal

loth

u P

uthi

ya P

uray

il

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tare

D

OC

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04/1

6

P

.O.C

heng

alla

yi 6

70 6

31

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6

102

Ass

ees.

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. P

atta

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Th

alas

seri

40

0.09

72

511/

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6/M

M/L

T/C

RPS

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17

N

afiy

a M

anzi

l,

H

ecta

re

DO

C/M

-28/

16

P.O

.May

yil 6

70 6

02

Dt 0

3.02

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6

103

Ash

raf.M

. C

huzh

ali

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aram

ba

383

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0.09

71

512/

15-1

6/M

M/L

T/C

RPS

/ 02

.02.

17

S

/o M

oide

en, M

arut

hiyo

dank

andi

Hou

se,

H

ecta

re

DO

C/M

-599

2/15

P

.O.P

ayya

voor

670

631

D

t 03.

02.2

016

10

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92

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6

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17

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6

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15

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18

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52

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S/o

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za, K

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C/M

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t 10.

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arid

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aji

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ande

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6

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6

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126

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02

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53

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02

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03

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129

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aman

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H

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2016

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6

131

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17

S

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umar

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DO

C/M

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6

P

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t 24.

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13

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17

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o R

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D

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2016

134

Muh

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H

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C/M

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13

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17

s/

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2016

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oth

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re

DO

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6

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2016

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mod

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17

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6

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re

DO

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6

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.O. K

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6

142

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016

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17

P

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6

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148

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ph

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6

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6

150

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D

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6

153

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a H

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DO

C/M

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6

P

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reek

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15

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ivas

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OC

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15

6 H

arid

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P

anni

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se

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15

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6

158

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C/M

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9 C

hand

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0.

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56

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atta

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6

160

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15

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6

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6

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166

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ulim

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re

DO

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167

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umar

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6

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huzh

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328

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OC

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re

DO

C/M

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17

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01

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17

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1943

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uthi

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93

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li,

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uthi

ya

Pur

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H

ecta

re

DO

C/M

-176

2/16

P

.O.C

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670

601

D

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6

176

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Kal

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71

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S/o

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inda

n, D

evi S

avid

am

H

ecta

re

DO

C/M

-352

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appa

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ur

Dtd

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016

17

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ashe

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akka

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olel

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ar,

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1

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72

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se,

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061/

16

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mal

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17

8 R

.K.S

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17

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16

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95

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016

17

9 R

.K.S

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adiy

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19

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17

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arak

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tare

D

OC

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593/

16

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lode

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70 5

95

Dtd

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016

18

0 K

unha

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K.

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ga

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aram

ba

63/1

A

0.09

71

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CR

PS/

03.0

5.17

S/o

Kun

ham

bu

H

ecta

re

DO

C/M

-118

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okka

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se, P

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D

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6

181

Bab

u.P

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ba

18/1

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71

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CR

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S/o

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akris

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iyat

h P

aram

bil H

ouse

,

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tare

D

OC

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187/

16

P.O

.Nid

iyen

ga 6

70 6

31

Dtd

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05.2

016

18

2 M

anoj

Mat

hew

N

uchi

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Iritty

1

0.09

71

22/1

6-17

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CR

PS/

03.0

5.17

S/o

Mat

hew

, Koc

hith

ara

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se,

H

ecta

re

DO

C/M

-186

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P

.O.C

hetti

yam

para

mb

D

td. 0

4.05

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6

183

Pra

sad

Che

ran

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ttil,

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iyen

ga

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aram

ba

41

24

23/1

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CR

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Pad

man

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n, C

hera

n V

eetti

l,

Cen

t D

OC

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764/

16

P.O

.Nid

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ga 6

70 6

31

Dtd

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016

18

4 G

opal

an.V

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Pan

apuz

ha

Kan

nur

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A

0.09

71

24/1

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CR

PS/

03.0

5.17

S/o

Odh

enan

Vay

akke

el, V

ayak

keel

Hou

se,

H

ecta

re

DO

C/M

-574

8/15

P

.O.K

uttiy

eri 6

70 1

42

Dtd

. 04.

05.2

016

18

5 M

anoh

aran

.P.P

.V.,

Nid

iyen

ga

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aram

ba

5 0.

052

25/1

6-17

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CR

PS/

03.0

5.17

S/o

T.V

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inda

n

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tare

D

OC

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096/

16

P

uthi

ya P

uray

il V

enga

loda

n, P

.O.C

huzh

ali

670

141

Dtd

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05.2

016

18

6 R

ajes

h.E

., K

allia

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tty

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0.

1942

26

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17/M

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17

S

/o N

aray

anan

, V.K

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se,

H

ecta

re

DO

C/M

-183

9/16

P

.O.E

daya

nnur

670

595

D

td. 0

4.05

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6

187

San

eesh

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Kal

liad

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17

0.

1942

27

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17/M

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17

S

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.K.K

anna

n, M

anas

am, V

aduv

anku

lam

,

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tare

D

OC

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825/

16

P.O

.Kut

tiatto

or 6

70 6

02

Dtd

. 09.

05.2

016

18

8 M

uham

ed B

ashe

er.K

.P.

Cha

vass

eri

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7

0/3

0.09

71

28/1

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CR

PS/

08.0

5.17

S/o

Abd

ulla

, Naj

ma

Man

zil,

H

ecta

re

DO

C/M

-171

8/16

P

arip

pum

kada

vu, P

.O.M

alap

patta

m 6

70 6

31

Dtd

. 09.

05.2

016

18

9 M

athe

w,

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ga

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ba

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17

S

/o V

argh

ese,

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irthi

muk

kil H

ouse

,

Hec

tare

D

OC

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16

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.O.C

hem

bant

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670

631

D

td. 0

9.05

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6

190

Pau

lose

, P

ayya

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lipar

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1

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0.09

71

30/1

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/MM

/LT/

CR

PS/

08.0

5.17

S/o

Var

ky, P

aram

ban

Hou

se,

H

ecta

re

DO

C/M

-176

3/16

P

.O.M

anat

hana

670

674

D

td. 0

9.05

.201

6

191

Thom

as V

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th

Pay

yavo

or

Talip

aram

ba

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0688

31

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17

S

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hack

o, V

ettit

hana

th H

ouse

,

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tare

D

OC

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877/

16

P.O

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sakk

ari 6

70 6

33

Dtd

. 09.

05.2

016

19

2 R

athe

esan

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allia

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tty

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32

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17/M

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17

S

/o V

ijaya

n, S

arig

a N

ivas

,

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t D

OC

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977/

16

P.O

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tiatto

or 6

70 6

02

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05.2

016

19

3 M

adhu

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hana

n.K

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Par

iyar

am

Talip

aram

ba

14/1

A

0.09

71

33/1

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CR

PS/

10.0

5.17

S/o

Kan

nan

Nai

r,

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tare

D

OC

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595/

16

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doth

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du, P

.O.C

heru

kunn

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0 30

1

D

td. 1

1.05

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6

194

Ven

ugop

alan

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hava

sser

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115

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0.09

71

34/1

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CR

PS/

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5.17

S/o

Kris

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Hec

tare

D

OC

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886/

16

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uvila

kand

y H

ouse

, P.O

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il 67

0 70

2

D

td. 1

1.05

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6

195

Ram

acha

ndra

n.C

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Nid

iyen

ga

Talip

aram

ba

42

0.09

71

35/1

6-17

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CR

PS/

10.0

5.17

S/o

Gop

alan

,

Hec

tare

D

OC

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767/

16

V

aliy

a V

alap

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Hou

se,

P.O

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iyen

ga 6

70

631

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05.2

016

19

6 P

rath

apa

Cha

ndra

n.C

.V.

Kee

zhur

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tty

173

0.09

71

36/1

6-17

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CR

PS/

12.0

5.17

S/o

Kris

hnan

Nam

biar

,

Hec

tare

D

OC

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619/

16

Ree

na N

ivas

, P.O

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nad

670

703

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05.2

016

19

7 G

eorg

e N

uchi

yad

Iritty

1

0.09

71

37/1

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/MM

/LT/

CR

PS/

17.0

5.17

S/o

Tho

mas

, Muk

kattu

Kav

unga

l

Hec

tare

D

OC

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876/

16

P.O

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kkat

hode

670

674

D

td. 1

8.05

.201

6

198

Abd

ulla

.M.

Nid

iyen

ga

Talip

aram

ba

41

0.09

71

38/1

6-17

/MM

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CR

PS/

17.0

5.17

S/o

Ibra

him

, Man

nan

Hou

se,

H

ecta

re

DO

C/M

-585

5/16

P

.O.T

alip

aram

ba 6

70 1

41

Dtd

. 18.

05.2

016

19

9 P

ram

od.P

. N

idiy

enga

Ta

lipar

amba

1

3/1

0.09

71

39/1

6-17

/MM

/LT/

CR

PS/

22.0

5.17

S/o

Nar

ayan

an P

adic

hal

H

ecta

re

DO

C/M

-184

1/16

Ill

ath

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se,

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dakk

ai 6

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602

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016

20

0 A

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ayam

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71

40/1

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/MM

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24.0

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S/o

Kum

aran

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lie

H

ecta

re

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C/M

-210

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lakk

al H

ouse

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70 7

02

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016

20

1 R

athe

esh.

E.P

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allia

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tty

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24

41

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17/M

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17

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unhi

ram

an, S

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ivas

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t D

OC

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072/

16

P.O

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tiatto

or 6

70 6

02

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016

20

2 Th

omas

P.J

. P

ayya

voor

Ta

lipar

amba

1

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71

42/1

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CR

PS/

31.0

5.17

S/o

P.D

evas

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ph.

H

ecta

re

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C/M

-219

5/16

P

uthu

para

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l H

ouse

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.O.K

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70

4

D

td. 0

1.06

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203

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ji Jo

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ayya

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lipar

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1

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71

43/1

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CR

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31.0

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S/o

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eph,

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mpl

anik

kal H

ouse

,

Hec

tare

D

OC

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196/

16

P.O

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dam

kada

v 67

0 70

6

D

td. 0

1.06

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6

204

Sus

hobh

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gatt

Pay

am

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3

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0.

0972

44

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17/M

M/L

T/C

RP

S/

31.0

5.17

S/o

K.S

ukum

aran

, Sus

hant

h N

ivas

,

Hec

tare

D

OC

/M-1

889/

16

P.O

.Siv

apur

am 6

70 7

02

Dtd

. 01.

06.2

016

20

5 S

unee

sh.N

. P

ayya

voor

Ta

lipar

amba

1

/1

0.09

71

45/1

6-17

/MM

/LT/

CR

PS/

31.0

5.17

S/o

Gop

i, P

allik

kand

i Hou

se,

H

ecta

re

DO

C/M

-202

0/16

P

.O.K

otta

yam

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l 670

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D

td. 0

1.06

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6

206

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keer

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4 24

46

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17/M

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17

S

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m, P

aram

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ouse

, P.O

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likuz

hi,

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ent

DO

C/M

-223

1/16

E

rnak

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Dtd

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016

20

7 R

ames

han.

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Kal

liad

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4

6/4

0.24

47

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17

S

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oran

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anka

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e D

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236/

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6

208

Sun

il K

unhi

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24

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PS

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17

S

/o K

undi

ram

an

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cre

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C/M

-222

9/16

A

mba

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ouse

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04

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06.2

016

20

9 B

ava

Kal

liad

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4

6/4

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71

49/1

6-17

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CR

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07.0

6.17

S/o

Ibra

him

Par

eeth

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hira

kkat

t,

H

ecta

re

DO

C/M

-223

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1

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8.06

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6

210

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lapp

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50

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17

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OC

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765/

16

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tikku

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671

313

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016

21

1 G

opal

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.V.

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liad

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51

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17

S

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unhi

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233/

16

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212

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P.K

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m,

H

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re

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C/M

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213

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Pay

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53

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17

S

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nand

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se,

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re

DO

C/M

-214

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.O.K

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02

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21

4 V

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anko

l Ta

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0.

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54

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17

S

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ya,

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215

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hilip

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55

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17

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se,

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ecta

re

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C/M

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likut

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32

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016

21

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anth

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ruve

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56

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31

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21

7 A

nil P

hilip

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lipar

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1

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71

57/1

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14.0

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S/o

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se,

H

ecta

re

DO

C/M

-231

1/16

P

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hand

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para

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ayya

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67

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D

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218

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kasa

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Talip

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48

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hand

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ouse

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e D

OC

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16

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02

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016

21

9 P

raka

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allia

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59

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17

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cre

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C/M

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602

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220

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aman

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C/M

-197

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P

.O.M

anga

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43

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016

22

1 M

anoj

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ayam

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61

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17

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ecta

re

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C/M

-244

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222

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25

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71

62/1

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ayan

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hoon

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ivas

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tare

D

OC

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360/

16

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02

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016

22

3 N

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0971

63

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17/M

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se,

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C/M

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.O.K

adam

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alap

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t. 67

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3

D

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6

224

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aram

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42

24

64/1

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CR

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21.0

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S/o

Kun

hira

man

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mal

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as,

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ent

DO

C/M

-164

7/16

P

.O.P

avan

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670

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D

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6

225

Em

man

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65

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17/M

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17

S

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osep

h, A

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se,

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ecta

re

DO

C/M

-222

6/16

P

.O.N

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632

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td. 2

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226

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deen

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66

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17

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240/

16

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6

227

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67

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17

S

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ussa

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utty

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ecta

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DO

C/M

-246

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P

.O.Ir

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593

D

td. 2

2.06

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6

228

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esha

n.R

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liad

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2

3/1

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17/M

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17

S

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reed

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avad

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16

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016

22

9 B

abu.

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Per

inth

atta

Ta

lipar

amba

4

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0.09

71

69/1

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CR

PS/

26.0

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ndan

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h H

ouse

,

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tare

D

OC

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425/

16

P.O

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him

anga

lam

670

309

D

td. 2

7.06

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6

230

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amac

hand

ran

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zhal

lur

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asse

ry

39

0.09

71

70/1

6-17

/MM

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CR

PS/

26.0

6.17

S/o

Kris

hnan

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biar

, Kris

hnal

ayam

Hec

tare

D

OC

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359/

16

P.O

.Mat

tann

ur 6

70 7

02

Dtd

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016

23

1 P

.Bal

an

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ari

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20

0.

0971

71

/16-

17/M

M/L

T/C

RPS

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17

S

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hekk

i Kan

nan,

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thi N

ivas

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tare

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OC

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487/

16

P.O

.Mur

inge

ri 67

0 61

2

D

td. 2

7.06

.201

6

232

Lase

r.K.M

. S

reek

anda

pura

m

Talip

aram

ba

163

/1

0.09

71

72/1

6-17

/MM

/LT/

CR

PS/

26.0

6.17

S/o

Mat

hew

, Kur

isin

gal H

ouse

,

Hec

tare

D

OC

/M-2

363/

16

P.O

.Sre

ekan

dapu

ram

670

633

D

td. 2

7.06

.201

6

233

Nis

ar.M

.V.

Mal

appa

ttam

Ta

lipar

amba

43

0.

0971

73

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o A

bdul

Kha

der,

Man

iyot

h H

ouse

,

Hec

tare

D

OC

/M-2

228/

16

P.O

.Mal

appa

ttam

670

631

D

td. 2

7.06

.201

6

234

Sun

il K

umar

.K.

Kal

liad

Iritty

2

3/1

0.09

71

74/1

6-17

/MM

/LT/

CR

PS/

26.0

6.17

S/o

Rag

hava

n, S

unil

Niv

as,

H

ecta

re

DO

C/M

-230

0/16

P

.O.K

uttia

ttoor

670

602

D

td. 2

7.06

.201

6

235

Abd

ul K

hade

r.K.R

. K

allia

d Iri

tty

46/

4 24

75

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o K

halid

.P.K

.

Cen

t D

OC

/M-2

505/

16

K.R

.Hou

se, P

.O.Ir

ikku

r 670

593

D

td. 2

7.06

.201

6

236

Raj

esh.

N.V

. P

erin

gom

e Ta

lipar

amba

11

7 0.

0971

76

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o V

ijaya

n, N

ghan

dam

are

Veet

til

H

ecta

re

DO

C/M

-246

6/16

P

.O.P

ayya

nnur

670

307

D

td. 2

7.06

.201

6

237

K.K

.Raj

eeva

n,

Cha

vass

eri

Iritty

10

4 0.

0971

77

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o G

ovin

dan,

Gov

inda

m, A

.K.G

.Nag

ar,

H

ecta

re

DO

C/M

-222

9/16

P

.O.M

atta

nnur

670

702

D

td. 2

7.06

.201

6

238

M.P

.Mad

hsoo

dhan

an

Kan

kol

Talip

aram

ba

25

3/5

0.04

08

78/1

6-17

/MM

/LT/

CR

PS/

26.0

6.17

S/o

Nar

ayan

an, E

dach

eri V

eedu

,

Hec

tare

D

OC

/M-2

197/

16

P.O

.Ezh

ilode

670

309

D

td. 2

7.06

.201

6

239

Sha

noj.V

. P

adiy

oor

Iritty

1

25/6

24

79

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o R

amak

rishn

an.C

.P.

C

ent

DO

C/M

-219

0/16

S

hano

j Niv

as, P

.O.E

lam

bara

670

595

D

td. 2

7.06

.201

6

240

N.K

.Man

oj K

umar

M

anan

ther

i Th

alas

sery

25/

1 0.

0971

80

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o K

rishn

an K

utty

, Krip

ama

H

ecta

re

DO

C/M

-236

1/16

P

.O.N

irmal

agiri

670

701

D

td. 2

7.06

.201

6

241

Gan

esh.

K.

Sre

ekan

dapu

ram

Ta

lipar

amba

1

61/2

0.

0971

81

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o K

anna

n, T

hayy

il V

alap

pil H

ouse

,

Hec

tare

D

OC

/M-2

227/

16

P.O

.Kay

aral

am 6

70 6

02

Dtd

. 27.

06.2

016

24

2 S

udhe

esh

Kum

ar.K

. E

ram

am

Talip

aram

ba

443

0.09

71

82/1

6-17

/MM

/LT/

CR

PS/

26.0

6.17

S/o

Bal

akris

hnan

Kad

en, B

alak

rishn

a,

H

ecta

re

DO

C/M

-141

2/16

C

heru

kunn

u, P

.O.M

otta

mm

al 6

70 3

31

Dtd

. 27.

06.2

016

24

3 A

nil K

umar

.M.

Mal

appa

ttam

Ta

lipar

amba

1

76/5

0.

0971

83

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o A

nand

an, K

oym

eth

Hou

se,

H

ecta

re

DO

C/M

-212

0/16

P

.O.K

ayar

alam

670

602

D

td. 2

7.06

.201

6

244

Kun

hika

nnan

.P.P

. P

utho

or

Thal

asse

ry

2/1

9.

71

84/1

6-17

/MM

/LT/

CR

PS/

26.0

6.17

S/o

Kor

an, S

ivam

Bha

van

A

re

DO

C/M

-207

1/16

P

.O.P

utho

or 6

70 6

92

Dtd

. 27.

06.2

016

24

5 S

asee

ndra

n.V

.C.

Kal

liad

Iritty

17

0.

1942

85

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o V

.Vel

ayud

han,

Val

iyap

aram

bath

Cha

lil H

ouse

,

Hec

tare

D

OC

/M-2

496/

16

P.O

.Pav

ando

or, K

ozhi

kode

673

613

D

td. 2

7.06

.201

6

246

Pra

jil.K

. K

anda

mku

nnu

Thal

asse

ry

53/

2 0.

0971

86

/16-

17/M

M/L

T/C

RPS

/ 26

.06.

17

S

/o M

.Pra

bhak

aran

, Pra

josh

Hou

se,

H

ecta

re

DO

C/M

-218

7/16

P

.O.A

yith

aram

amba

ram

670

643

D

td. 2

7.06

.201

6

247

Ane

esh.

M.

Kal

liad

Iritty

1

0.09

71

87/1

6-17

/MM

/LT/

CR

PS/

28.0

6.17

S/o

Gov

inda

n, M

avila

kkan

di H

ouse

,

Hec

tare

D

OC

/M-2

467/

16

P.O

.Per

uval

athu

para

mba

670

593

D

td. 2

9.06

.201

6

248

Pra

deep

Kum

ar.P

.K.

Sre

ekan

dapu

ram

Ta

lipar

amba

23

4 0.

1939

88

/16-

17/M

M/L

T/C

RPS

/ 28

.06.

17

S

/o N

aray

anan

, The

jus,

Kuz

hilo

or,

H

ecta

re

DO

C/M

-242

7/16

P

.O.P

adiy

oor 6

70 7

03

Dtd

. 29.

06.2

016

24

9 S

anee

sh K

umar

.K.

Sre

ekan

dapu

ram

Ta

lipar

amba

23

6 0.

0971

89

/16-

17/M

M/L

T/C

RPS

/ 28

.06.

17

S

/o N

aray

anan

, Kai

prat

h H

ouse

,

Hec

tare

D

OC

/M-2

504/

16

P.O

.Mal

appa

ttam

670

631

D

td. 2

9.06

.201

6

250

Pre

side

nt

Kut

tiyer

i Ta

lipar

amba

1

8/2

0.09

72

90/1

6-17

/MM

/LT/

CR

PS/

28.0

6.17

K

annu

r Ka

lluko

thu

Thoz

hila

li K

shem

a S

ahak

aran

a

Hec

tare

D

OC

/M-2

362/

16

S

anga

m

Ltd.

, D

herm

asal

a,

P.O

.Par

asin

ikad

avu

670

563

Dtd

. 29.

06.2

016

25

1 S

reej

esh.

V.

Kal

liad

Iritty

1

24

91/1

6-17

/MM

/LT/

CR

PS/

29.0

6.17

S/o

Sre

edha

ran,

Kap

pana

yil V

eedu

,

Cen

t D

OC

/M-2

603/

16

P.O

.Kay

ani 6

70 7

02

Dtd

. 30.

06.2

016

25

2 A

nil K

umar

.M.

Kol

ache

ri Ta

lipar

amba

8/1

0.

0971

92

/16-

17/M

M/L

T/C

RPS

/ 29

.06.

17

S

/o A

nand

an, K

oym

eth

Hou

se,

H

ecta

re

DO

C/M

-598

/16

P.O

.Kay

aral

am 6

70 6

02

Dtd

. 30.

06.2

016

25

3 R

iyas

.K.

Kal

liad

Iritty

2

3/1

0.19

42

93/1

6-17

/MM

/LT/

CR

PS/

29.0

6.17

S/o

Am

mad

, Kon

hant

avid

a H

ouse

,

Hec

tare

D

OC

/M-2

653/

16

P

.O.P

onm

erip

aram

bil,

Koz

hiko

de D

ist

673

542

Dtd

. 30.

06.2

016

25

4 R

iyas

.K.

Kal

liad

Iritty

2

3/1

0.09

71

94/1

6-17

/MM

/LT/

CR

PS/

29.0

6.17

S/o

Am

mad

, Kon

hant

avid

a H

ouse

,

Hec

tare

D

OC

/M-2

654/

16

P

.O.P

onm

erip

aram

bil,

Koz

hiko

de D

ist

673

542

Dtd

. 30.

06.2

016

25

5 V

.Raj

esh

Kal

liad

Iritty

4

6/4

9.71

95

/16-

17/M

M/L

T/C

RPS

/ 30

.06.

17

S

/o T

.V.G

opal

an, V

engo

ttil H

ouse

,

Are

D

OC

/M-2

535/

16

Cho

oliy

ad, P

.O.M

alap

patta

m 6

70 6

31

Dtd

. 01.

07.2

016

25

6 V

inod

Kum

ar.K

.P.

Pad

uvila

yi

Thal

asse

ry

2 9.

71

96/1

6-17

/MM

/LT/

CR

PS/

03.0

7.17

S

/o S

reed

hara

n, A

ndro

mid

a,

A

re

DO

C/M

-226

5/16

P

.O.A

ncha

rakk

andi

670

612

D

td. 0

4.07

.201

6

257

Rad

hakr

ishn

an.C

.M.

Per

ingo

me

Talip

aram

ba

38/

5 0.

097

97/1

6-17

/MM

/LT/

CR

PS/

03.0

7.17

S/o

Mad

hava

n N

air,

Che

ttikk

att H

ouse

,

Hec

tare

D

OC

/M-2

465/

16

P.O

.Eda

vara

mba

670

511

D

td. 0

4.07

.201

6

258

Raj

endr

an.C

.M.

Per

ingo

me

Talip

aram

ba

110

/3

0.09

6 98

/16-

17/M

M/L

T/C

RPS

/ 03

.07.

17

S

/o

Par

ames

hwar

an,

Che

mm

anch

eri

Hou

se,

H

ecta

re

DO

C/M

-252

2/16

P

.O.P

adiy

ottu

chal

670

307

D

td. 0

4.07

.201

6

259

Rad

hakr

ishn

an.K

. P

erin

that

ta

Talip

aram

ba

46/

1A

0.19

44

99/1

6-17

/MM

/LT/

CR

PS/

03.0

7.17

S/o

Kun

happ

a, K

unna

ran

Veed

u,

H

ecta

re

DO

C/M

-250

3/16

P

.O.M

athi

l 670

307

D

td. 0

4.07

.201

6

260

Ram

akris

hnan

Kur

uvan

K

allia

d Iri

tty

46/

4 0.

24

100/

16-1

7/M

M/L

T/C

RPS

/ 03

.07.

17

S

/o A

nand

an K

uruv

an, S

neha

Niv

as,

A

cre

DO

C/M

-267

0/16

P

.O.C

hava

sser

i 670

702

D

td. 0

4.07

.201

6

261

M.N

aray

anan

, K

allia

d Iri

tty

23/

1 0.

0972

10

1/16

-17/

MM

/LT/

CR

PS/

03.0

7.17

S/o

Kun

hira

man

, Bin

du N

ivas

,

Hec

tare

D

OC

/M-2

508/

16

P.O

.Pat

tann

ur 6

70 5

95

Dtd

. 04.

07.2

016

26

2 P

rade

epan

.C.

Kal

liad

Iritty

2

9/3A

0.

0971

10

2/16

-17/

MM

/LT/

CR

PS/

03.0

7.17

S/o

Gov

inda

n, P

aram

bath

anka

ndi H

ouse

,

Hec

tare

D

OC

/M-2

640/

16

P.O

.Mun

deri

670

591

Dtd

. 04.

07.2

016

26

3 H

amsa

Kut

ty.M

. S

reek

anda

pura

m

Talip

aram

ba

16

0/1

0.09

71

103/

16-1

7/M

M/L

T/C

RPS

/ 03

.07.

17

S

/o M

uham

med

, N

iduv

attp

uray

il H

ouse

,

Hec

tare

D

OC

/M-2

480/

16

P.O

.Mal

appa

ttam

D

td. 0

4.07

.201

6

264

Moh

anan

Ikko

mat

h P

erin

gom

e Ta

lipar

amba

2

25/5

0.

0965

10

4/16

-17/

MM

/LT/

CR

PS/

03.0

7.17

Ikko

mat

h H

ouse

, P.O

.Chi

ttadi

,

Hec

tare

D

OC

/M-2

470/

16

Ala

kkod

e 67

0 57

1

D

td. 0

4.07

.201

6

265

Vas

udev

an,

Cha

vass

eri

Iritty

10

5 0.

1943

10

5/16

-17/

MM

/LT/

CR

PS/

06.0

7.17

S/o

Kel

an, P

arak

kand

i Hou

se,

H

ecta

re

DO

C/M

-226

7/16

P

.O.P

.R.N

agar

670

702

D

td. 0

7.07

.201

6

266

Muh

amm

ed S

ajir

Talip

aram

ba

Talip

aram

ba

67

24

106/

16-1

7/M

M/L

T/C

RPS

/ 07

.07.

17

S

/o M

usth

afa.

N.,

Koo

ttukk

an H

ouse

,

Cen

t D

OC

/M-4

478/

16

P.O

.Kar

imba

m 6

70 1

42

Dtd

. 08.

07.2

016

26

7 C

.Man

ohar

an

Kal

liad

Iritty

22

0.

48

107/

16-1

7/M

M/L

T/C

RPS

/ 07

.07.

17

S

/o C

happ

adi K

anna

n,

A

cre

DO

C/M

-223

2/16

C

happ

adi H

ouse

, P.O

.Kal

liad

670

593

Dtd

. 08.

07.2

016

26

8 S

anee

sh.K

. N

idiy

enga

Ta

lipar

amba

3

7/1A

1 0.

1943

10

8/16

-17/

MM

/LT/

CR

PS/

10.0

7.17

S/o

Kan

nan,

Man

asam

,

Hec

tare

D

OC

/M-2

592/

16

Vad

uvan

kula

m, P

.O.K

uttia

ttoor

670

602

D

td. 1

1.07

.201

6

269

Sha

rafu

dhee

n.E

.P.

Kal

liad

Iritty

4

6/4

24

109/

16-1

7/M

M/L

T/C

RPS

/ 10

.07.

17

S

/o A

bdu

Rah

iman

, Sub

aida

Man

zil

C

ent

DO

C/M

-278

0/16

P

.O.M

ayyi

l

D

td. 1

1.07

.201

6

270

Raj

esh.

P.

Per

inth

atta

Ta

lipar

amba

4

5/1A

0.

0971

11

0/16

-17/

MM

/LT/

CR

PS/

10.0

7.17

S/o

Nar

ayan

an,

H

ecta

re

DO

C/M

-247

1/16

P

aruk

kara

n H

ouse

, P.O

.Por

akku

nnu6

70 3

06

Dtd

. 11.

07.2

016

27

1 P

rajit

h Ku

mar

.K.

Kal

liad

Iritty

4

6/4

0.09

72

111/

16-1

7/M

M/L

T/C

RPS

/ 10

.07.

17

S

/o K

unha

mbu

Nam

biar

,

Hec

tare

D

OC

/M-2

468/

16

Kris

hna

Krip

a, P

.O.K

allia

d 67

0 59

3

D

td. 1

1.07

.201

6

272

Ram

esha

n.V

. K

adan

appa

lli

Kan

nur

84/

2B

0.09

71

112/

16-1

7/M

M/L

T/C

RPS

/ 14

.07.

17

S

/o P

.V.R

aman

, Vad

akki

niyi

l Hou

se,

H

ecta

re

DO

C/M

-268

3/16

C

hand

apur

a, K

adan

appa

lli.P

.O. 6

70 3

04

Dtd

. 15.

07.2

016

27

3 G

afoo

r.A.T

. P

ariy

aram

Ta

lipar

amba

2

80/1

24

11

3/16

-17/

MM

/LT/

CR

PS/

17.0

7.17

S/o

K.P

.Mam

mu,

A.T

.Hou

se,

C

ent

DO

C/M

-889

/16

And

anku

lam

, C.P

oyil.

P.O

.670

502

D

td. 1

8.07

.201

6

274

Rav

eend

ran.

V.C

. S

reek

anda

pura

m

Talip

aram

ba

74/

2 0.

1942

11

4/16

-17/

MM

/LT/

CR

PS/

17.0

7.17

S/o

Kun

hira

man

, Van

nara

Cha

lil H

ouse

,

Hec

tare

D

OC

/M-2

481/

16

Ned

ungo

me.

P.O

. 670

631

D

td. 1

8.07

.201

6

275

Nar

ayan

an.V

.K.

May

yil

Talip

aram

ba

42/

3 0.

0972

11

5/16

-17/

MM

/LT/

CR

PS/

17.0

7.17

S/o

Kan

nan,

Kat

til H

ouse

,

Hec

tare

D

OC

/M-2

559/

16

May

yil 6

70 6

02

Dtd

. 18.

07.2

016

27

6 C

heriy

an.K

.C.

Cha

vass

eri

Iritty

8

3/2

0.09

71

116/

16-1

7/M

M/L

T/C

RPS

/ 17

.07.

17

S

/o C

heriy

an J

osep

h,

H

ecta

re

DO

C/M

-212

4/16

K

otta

para

mbi

l Hou

se, K

akka

d.P

.O. 6

70 0

03

Dtd

. 18.

07.2

016

27

7 A

nees

h.A

. M

alap

patta

m

Talip

aram

ba

47/1

0.

049

117/

16-1

7/M

M/L

T/C

RPS

/ 17

.07.

17

S

/o N

aray

anan

, Koo

nam

kand

i Hou

se,

H

ecta

re

DO

C/M

-290

0/16

M

ulla

kkod

i.P.O

. 670

602

D

td. 1

8.07

.201

6

278

San

eesh

.K.

Kal

liad

Iritty

17

0.

1942

11

8/16

-17/

MM

/LT/

CR

PS/

18.0

7.17

S/o

Kan

nan,

Man

asam

,

Hec

tare

D

OC

/M-2

921/

16

Vad

uvan

kula

m, P

.O.K

uttia

ttoor

670

602

D

td. 1

9.07

.201

6

279

Ane

esh.

K.C

. M

ayyi

l Ta

lipar

amba

1

48/3

0.

0971

11

9/16

-17/

MM

/LT/

CR

PS

/ 19

.07.

17

S

/o G

ovin

dan,

Hec

ate

DO

C/M

-297

3/16

A

jith

Niv

as, P

.O.M

ayyi

l 670

602

D

td. 2

0.07

.201

6

280

Nai

nesh

.P.

Man

anth

eri

Thal

asse

ry

297

/1

0.09

71

120/

16-1

7/M

M/L

T/C

RPS

/ 19

.07.

17

S

/o N

aray

anan

, Sre

yas,

Hec

tare

D

OC

/M-2

463/

16

Che

ruva

nche

ri.P

.O. 6

70 6

50

Dtd

. 20.

07.2

016

28

1 D

ines

han.

P.

Cha

vass

eri

Iritty

10

4 0.

1942

12

1/16

-17/

MM

/LT/

CR

PS/

19.0

7.17

S/o

Bal

an N

ambi

ar, K

elot

h H

ouse

,

Hec

tare

D

OC

/M-2

194/

16

Por

ora

670

702

Dtd

. 20.

07.2

016

28

2 B

iju

Per

ingo

me

Talip

aram

ba

22/

5 0.

0971

12

2/16

-17/

MM

/LT/

CR

PS/

19.0

7.17

S/o

Kur

iyak

ose,

Kun

nath

aray

il H

ouse

,

Hec

tare

D

OC

/M-2

464/

16

P.O

.Pad

iyot

tuch

al 6

70 3

07

Dtd

. 20.

07.2

016

28

3 R

ajee

van.

K.

Mok

eri

Thal

asse

ry

93/

1A

24

123/

16-1

7/M

M/L

T/C

RPS

/ 19

.07.

17

S

/o A

nand

an, K

otta

rant

avid

a H

ouse

,

Cen

t D

OC

/M-2

731/

16

Che

nday

ad.P

.O. 6

70 6

92

Dtd

. 20.

07.2

016

28

4 R

adha

kris

hnan

.K.P

. S

reek

anda

pura

m

Talip

aram

ba

74/

6 0.

194

124/

16-1

7/M

M/L

T/C

RPS

/ 19

.07.

17

S

/o K

unhi

ram

an, K

ayak

apur

ayil

Hou

se,

H

ecta

re

DO

C/M

-259

9/16

N

edun

gom

e.P

.O. 6

70 6

31

Dtd

. 20.

07.2

016

28

5 S

uhai

l.M.V

.P.

Per

ingo

me

Talip

aram

ba

21/

2 0.

098

125/

16-1

7/M

M/L

T/C

RPS

/ 19

.07.

17

S

/o H

amsa

Haj

i, M

.V.P

.Hou

se,

H

ecta

re

DO

C/M

-219

8/16

P

.O.T

hekk

umba

d 67

0 30

1

D

td. 2

0.07

.201

6

286

Dile

ep.K

.P.

Kal

liad

Iritty

3

/1

0.09

71

126/

16-1

7/M

M/L

T/C

RPS

/ 24

.07.

17

S

/o G

opal

an, K

.P.H

ouse

,

Hec

tare

D

OC

/M-2

597/

16

Kan

ghiro

de.P

.O. 6

70 5

92

Dtd

. 25.

07.2

016

28

7 P

rade

ep.A

. K

urum

atho

or

Talip

aram

ba

104

/1

0.09

71

127/

16-1

7/M

M/L

T/C

RPS

/ 24

.07.

17

S

/o A

ppu

Kut

tan

Nai

r, K

rishn

a B

hava

n

Hec

tare

D

OC

/M-2

404/

16

Kur

umat

hoor

.P.O

. 670

148

D

td. 2

5.07

.201

6

288

Ali.

K.C

. K

allia

d Iri

tty

46/

4 0.

0971

12

8/16

-17/

MM

/LT/

CR

PS/

24.0

7.17

S/o

Muh

amm

ed K

unhi

, Kin

akko

ol H

ouse

,

Hec

tare

D

OC

/M-2

882/

16

Per

uval

athu

para

mba

D

td. 2

5.07

.201

6

289

Sha

bu.K

. M

anan

ther

i Th

alas

sery

29

6 0.

0408

12

9/16

-17/

MM

/LT/

CR

PS/

24.0

7.17

S/o

Gop

i, C

ham

atha

yulla

para

mba

th H

ouse

,

Hec

tare

D

OC

/M-3

043/

16

Che

ruva

nche

ri.P

.O. 6

70 6

50

Dtd

. 25.

07.2

016

29

0 A

nand

an T

hach

aron

C

hava

sser

i Iri

tty

127

/1

0.19

42

130/

16-1

7/M

M/L

T/C

RPS

/ 24

.07.

17

S

/o K

elan

, Ana

ndam

,

H

ecta

re

DO

C/M

-260

2/16

M

atta

nnur

670

702

D

td. 2

5.07

.201

6

291

K.K

.Raj

eeva

n,

Kal

liad

Iritty

4

6/4

0.09

71

131/

16-1

7/M

M/L

T/C

RPS

/ 24

.07.

17

S

/o K

umar

an, K

unhi

kkan

di H

ouse

,

Hec

tare

D

OC

/M-3

018/

16

Che

kkik

ulam

.P.O

. 670

592

D

td. 2

5.07

.201

6

292

Ibra

him

Kut

ty.R

.P.

Chu

zhal

i Ta

lipar

amba

6

6/1A

1 0.

0972

13

2/16

-17/

MM

/LT/

CR

PS/

24.0

7.17

S/o

Aha

mm

ed K

utty

, Ram

Kun

num

mal

Hec

tare

D

OC

/M-2

811/

16

Put

hiya

Pur

ayil,

Mul

lako

di.P

.O. 6

70 6

02

Dtd

. 25.

07.2

016

29

3 S

hyju

.V.V

. K

anko

l Ta

lipar

amba

2

24/1

0.

0971

13

3/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S/o

T.M

.San

kara

n, V

adak

ke V

eetti

l Hou

se,

H

ecta

re

DO

C/M

-190

3/16

P

.O.K

aran

thad

670

308

D

td. 2

7.07

.201

6

294

Abd

ul J

abba

r.T.

Eru

vess

i Ta

lipar

amba

1

09/1

A

0.09

71

134/

16-1

7/M

M/L

T/C

RPS

/ 26

.07.

17

S

/o A

boob

acke

r, Th

ekka

n M

arak

kath

Hou

se,

H

ecta

re

DO

C/M

-294

1/16

S

reek

anda

pura

m.P

.O. 6

70 6

31

Dtd

. 27.

07.2

016

29

5 A

ssee

s.K

.P.

Mal

appa

ttam

Ta

lipar

amba

88

0.

1942

13

5/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S/o

Mam

mad

, Akk

aram

mal

Hou

se,

H

ecta

re

DO

C/M

-307

1/16

M

ayyi

l.P.O

. 670

602

D

td. 2

7.07

.201

6

296

Ram

esha

n.P

.V.

Kal

liad

Iritty

1

0.09

71

136/

16-1

7/M

M/L

T/C

RPS

/ 26

.07.

17

S

/o C

hand

u Ku

tty, P

uthi

ya V

eetti

l Hou

se,

H

ecta

re

DO

C/M

-260

1/16

K

osav

anva

yal.P

.O. 6

70 5

93

Dtd

. 27.

07.2

016

29

7 B

iju K

umar

.K.

Per

ingo

me

Talip

aram

ba

26/

14

0.09

61

137/

16-1

7/M

M/L

T/C

RPS

/ 26

.07.

17

S

/o R

aman

.T.K

., Ku

nnum

mal

Hou

se,

H

ecta

re

DO

C/M

-300

8/16

E

ttuku

dukk

a.P

.O. 6

70 5

21

Dtd

. 27.

07.2

016

29

8 A

ji.P

.P.

Per

ingo

me

Talip

aram

ba

22/

8 0.

0961

13

8/16

-17/

MM

/LT/

CR

PS

/ 26

.07.

17

S

/o D

amod

hara

n, P

utha

n P

aram

bil H

ouse

,

Hec

tare

D

OC

/M-2

931/

16

Per

ingo

me.

P.O

.

D

td. 2

7.07

.201

6

299

San

thos

h Ku

mar

.K.

Per

ingo

me

Talip

aram

ba

26/

1 0.

095

139/

16-1

7/M

M/L

T/C

RPS

/ 26

.07.

17

S

/o C

hand

an, K

adiy

an H

ouse

,

Hec

tare

D

OC

/M-3

009/

16

Koz

hum

mal

.P.O

. 670

521

D

td. 2

7.07

.201

6

300

Pre

yesh

.P.

Kal

liad

Iritty

17

0.

0971

14

0/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S/o

Vas

udev

an, K

anno

th H

ouse

,

Hec

tare

D

OC

/M-3

078/

16

Kos

avan

vaya

l.P.O

. 670

593

D

td. 2

7.07

.201

6

301

Ben

ny.M

.C.

Chu

zhal

i Ta

lipar

amba

30

0.

0971

14

1/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S/o

Cha

cko,

Mel

edat

h H

ouse

,

Hec

tare

D

OC

/M-6

64/1

6

Th

adik

kada

vu.P

.O. 6

70 5

81

Dtd

. 27.

07.2

016

30

2 R

athe

esh.

P.P

. K

allia

d Iri

tty

11/

1 24

14

2/16

-17/

MM

/LT/

CR

PS

/ 26

.07.

17

S

/o J

anar

dhan

an, K

alas

apar

amba

th H

ouse

,

Cen

t D

OC

/M-1

920/

16

Kal

liad.

P.O

. 670

593

D

td. 2

7.07

.201

6

303

Mus

thaf

a.M

.K.

Kal

liad

Iritty

2

9/3A

0.

0971

14

3/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S

/o K

unhi

Muh

amm

ed,

Mun

daya

dank

andi

H

ouse

,

Hec

tare

D

OC

/M-2

942/

16

Mun

der.P

.O. 6

70 5

91

Dtd

. 27.

07.2

016

30

4 R

avee

ndra

n.M

. P

azha

ssi

Iritty

1

42/1

24

14

4/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S/o

K.P

aith

al, A

run

Niv

as,

C

ent

DO

C/M

-304

4/16

P

.O.K

angh

ileri

670

702

Dtd

. 27.

07.2

016

30

5 Ib

rahi

m K

utty

.K.

Cha

vass

eri

Iritty

1

09/1

0.

0971

14

5/16

-17/

MM

/LT/

CR

PS/

26.0

7.17

S/o

T.M

oide

en, S

hahi

na M

anzi

l,

Hec

tare

D

OC

/M-2

676/

16

P.O

.Kol

ari 6

70 7

02

Dtd

. 27.

07.2

016

30

6 S

rees

han.

K.

Pat

tann

ur

Thal

asse

ry

9/1

9.

7 14

6/16

-17/

MM

/LT/

CR

PS/

27.0

7.17

S/o

Kun

hira

man

, Am

man

athi

l Hou

se,

A

re

DO

C/M

-300

6/16

E

daya

nnur

.P.O

. 670

595

D

td. 2

8.07

.201

6

307

Raj

in.K

.E.

Kal

liad

Iritty

22

24

14

7/16

-17/

MM

/LT/

CR

PS/

31.0

7.17

S/o

Nar

ayan

an, N

aray

anal

ayam

,

Cen

t D

OC

/M-2

729/

16

Mat

tann

ur 6

70 7

02

Dtd

. 01.

08.2

016

30

8 S

ures

h.P.

V.

Eru

vess

i Ta

lipar

amba

1

8/2

0.09

71

148/

16-1

7/M

M/L

T/C

RPS

/ 31

.07.

17

S

/o V

elay

udha

n, P

ayam

pani

yil H

ouse

,

Hec

tare

D

OC

/M-2

600/

16

Che

mbe

ri.P

.O. 6

70 6

32

Dtd

. 01.

08.2

016

30

9 A

nees

h.P

.V.

Kal

liad

Iritty

1

0.09

71

149/

16-1

7/M

M/L

T/C

RPS

/ 31

.07.

17

S

/o K

arun

akar

an, J

isha

Niv

as,

H

ecta

re

DO

C/M

-311

8/16

K

osav

anva

yal.P

.O. 6

70 5

93

Dtd

. 01.

08.2

016

31

0 S

ulph

ikka

r.N.

Koo

veri

Talip

aram

ba

189

0.09

73

150/

16-1

7/M

M/L

T/C

RPS

/ 31

.07.

17

S

/o A

bdul

la, S

as M

anzi

l,

Hec

tare

D

OC

/M-2

991/

16

Cha

lad.

P.O

. 670

014

D

td. 0

1.08

.201

6

311

Gan

esha

n.K.

K

allia

d Iri

tty

1 0.

0971

15

1/16

-17/

MM

/LT/

CR

PS/

31.0

7.17

S/o

Gov

inda

n, K

unna

rath

Hou

se,

H

ecta

re

DO

C/M

-315

1/16

K

allia

d.P

.O. 6

70 5

93

Dtd

. 01.

08.2

016

31

2 V

argh

ese

Jose

ph

Pad

iyoo

r Iri

tty

112

/4

24

152/

16-1

7/M

M/L

T/C

RPS

/ 31

.07.

17

S

/o J

osep

h, C

hira

tta V

elik

kuzh

i Hou

se,

C

ent

DO

C/M

-307

3/16

K

elak

om.P

.O. 6

70 6

74

Dtd

. 01.

08.2

016

313

Dev

assy

a N

idiy

enga

Ta

lipar

amba

41

0.

0971

15

3/16

-17/

MM

/LT/

CR

PS/

02.0

8.17

S/o

Jos

eph,

Ikka

ra H

ouse

,

Hec

tare

D

OC

/M-2

022/

16

Che

mbe

ri.P

.O. 6

70 6

32

Dtd

. 03.

08.2

016

31

4 Ja

yara

jan.

P.

Nid

iyen

ga

Talip

aram

ba

13/

1 0.

0971

15

4/16

-17/

MM

/LT/

CR

PS

/ 02

.08.

17

S

/o K

.V.N

aray

anan

, Kan

ghiro

dan

Hou

se,

H

ecta

re

DO

C/M

-307

4/16

N

idiy

enga

.P.O

. 670

631

D

td. 0

3.08

.201

6

315

Man

oj K

umar

.M.P

. P

atta

nnur

Th

alas

sery

40

9.

67

155/

16-1

7/M

M/L

T/C

RPS

/ 02

.08.

17

S

/o V

asud

evan

, Am

ith N

ivas

,

Are

D

OC

/M-3

007/

16

Kut

tiatto

or.P

.O. 6

70 6

02

Dtd

. 03.

08.2

016

31

6 B

alag

opal

an.A

. K

allia

d Iri

tty

46/

4 0.

1942

15

6/16

-17/

MM

/LT/

CR

PS/

02.0

8.17

S/o

Cha

thu

Kut

ty N

ambi

ar,

H

ecta

re

DO

C/M

-318

8/16

M

avila

chal

il H

ouse

, Pat

tann

ur.P

.O. 6

70 5

95

Dtd

. 03.

08.2

016

31

7 S

udee

p C

huzh

ali

Talip

aram

ba

42/

4 0.

0972

15

7/16

-17/

MM

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CR

PS/

02.0

8.17

S/o

Vel

ayud

han,

Kan

nam

balli

Hou

se,

H

ecta

re

DO

C/M

-219

1/16

K

adam

puzh

a.P

.O. 6

76 5

53

Dtd

. 03.

08.2

016

31

8 K

rishn

an.C

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Chu

zhal

i Ta

lipar

amba

4

3/2

0.09

72

158/

16-1

7/M

M/L

T/C

RPS

/ 02

.08.

17

S

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hand

u Ku

tty, C

hath

oth

Hou

se,

H

ecta

re

DO

C/M

-278

7/16

K

oyya

m.P

.O. 6

70 1

42

Dtd

. 03.

08.2

016

31

9 U

mm

er.P

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Chu

zhal

i Ta

lipar

amba

3

26/4

0.

0971

15

9/16

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MM

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CR

PS/

02.0

8.17

S/o

Ali,

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yakk

el P

oova

n K

ulat

hil H

ouse

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tare

D

OC

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28/1

6

C

huzh

ali.P

.O. 6

70 6

32

Dtd

. 03.

08.2

016

32

0 S

ures

h Ba

bu.T

. M

anan

ther

i Th

alas

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2

97/1

0.

0971

16

0/16

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MM

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CR

PS/

07.0

8.17

S/o

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u, M

otta

para

mba

th H

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Hec

tare

D

OC

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077/

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0 65

0

D

td. 0

8.08

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6

321

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Man

anth

eri

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asse

ry

296

0.09

71

161/

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7/M

M/L

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RPS

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.08.

17

S

/o R

agha

van,

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hapr

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,

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tare

D

OC

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989/

16

Che

ruva

nche

ri.P

.O. 6

70 6

30

Dtd

. 08.

08.2

016

32

2 P

.Abd

u H

anee

fa

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aval

lur

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asse

ry

57/

2B2

0.09

71

162/

16-1

7/M

M/L

T/C

RPS

/ 07

.08.

17

S

/o M

ayin

, Par

akka

l Hou

se,

H

ecta

re

DO

C/M

-185

2/16

K

ondo

tti.P

.O.,

Mal

appu

ram

673

638

D

td. 0

8.08

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6

323

Abd

ul S

alam

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. C

huzh

ali

Talip

aram

ba

320

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0.09

71

163/

16-1

7/M

M/L

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17

S

/o M

oide

en K

utty

, And

yan

Val

appi

l Hou

se,

H

ecta

re

DO

C/M

-731

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P.O

.Koy

yam

670

142

D

td. 0

8.08

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6

324

Muh

amm

ed S

ulim

an.M

. K

allia

d Iri

tty

23/

1 0.

1942

16

4/16

-17/

MM

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CR

PS/

07.0

8.17

S

/o K

unhi

Muh

amm

ed, A

lang

adan

Hou

se,

H

ecta

re

DO

C/M

-795

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Ven

gottu

r.P.O

., M

alap

pura

m 6

76 5

03

Dtd

. 08.

08.2

016

32

5 A

bdul

Sal

eem

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. K

allia

d Iri

tty

22

0.09

72

165/

16-1

7/M

M/L

T/C

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.08.

17

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K.P

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ul

Maj

eed

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i, K

aipp

ayil

P

uthi

ya

H

ecta

re

DO

C/M

-268

0/16

P

uray

il H

ouse

, P.O

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rupa

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si 6

70 6

01

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. 16.

08.2

016

32

6 P

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hi K

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an

Man

anth

eri

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asse

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25/

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166/

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17

S

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ovin

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16

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anth

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.O. 6

70 6

43

Dtd

. 16.

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016

32

7 A

bdul

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4

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24

167/

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7/M

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17

S

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iman

A

bdul

, C

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mal

H

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t D

OC

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996/

16

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rupa

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.O. 6

70 6

01

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016

32

8 S

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K.

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Iritty

4

6/4

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71

168/

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7/M

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RPS

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.08.

17

S

/o A

bdul

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iman

, Kee

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ath

Hou

se,

H

ecta

re

DO

C/M

-316

6/16

P

eruv

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hupa

ram

ba.P

.O. 6

70 5

93

Dtd

. 16.

08.2

016

32

9 M

anoj

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ar.N

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dam

kunn

u Th

alas

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6

4/1

0.09

72

169/

16-1

7/M

M/L

T/C

RPS

/ 15

.08.

17

S

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rishn

an K

utty

, Krip

ama

H

ecta

re

DO

C/M

-283

4/16

N

irmal

agiri

.P.O

. 670

701

Dtd

. 16.

08.2

016

33

0 R

avee

ndra

n N

ambi

ar,

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liad

Iritty

17

0.

0971

17

0/16

-17/

MM

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CR

PS/

15.0

8.17

S/o

Nar

ayan

an, P

appi

niss

eri H

ouse

,

Hec

tare

D

OC

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079/

16

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avan

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l.P.O

. 670

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D

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6

331

Pra

veen

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Kal

liad

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17

0.

0972

17

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MM

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15.0

8.17

S/o

Sre

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a N

ivas

,

Hec

tare

D

OC

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233/

16

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, Pat

tann

ur.P

.O. 6

70 5

95

Dtd

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08.2

016

33

2 S

ajes

h.A

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allia

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29/3

A

24

172/

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7/M

M/L

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17

S

/o R

amac

hand

ran

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t D

OC

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988/

16

S

anis

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hitta

ripar

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.P.O

. 67

0 65

0

D

td. 1

6.08

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6

333

T.As

hoka

n E

ram

am

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aram

ba

443

0.09

71

173/

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7/M

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17

S

/o M

adha

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T., T

hatta

rath

Hou

se,

H

ecta

re

DO

C/M

-298

3/16

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ana.

P.O

. 670

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D

td. 1

7.08

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6

334

M.V

.Ram

acha

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n K

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23/

1 0.

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17

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16.0

8.17

S/o

Gov

inda

n N

ambi

ar, T

heer

tham

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Hec

tare

D

OC

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042/

16

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uval

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aram

ba.P

.O. 6

70 5

93

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08.2

016

335

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ul H

amee

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gom

e Ta

lipar

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3

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72

175/

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7/M

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17

S

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ul R

ahim

an,

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ya H

ouse

,

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tare

D

OC

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228/

16

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iya,

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arag

od 6

71 3

16

Dtd

. 17.

08.2

016

33

6 Jo

shi

Pay

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aram

ba

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0.

0971

17

6/16

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MM

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CR

PS/

16.0

8.17

S/o

Tho

mas

, Akk

akku

nnel

Hou

se,

H

ecta

re

DO

C/M

-190

2/16

K

osav

anva

yal.P

.O. 6

70 5

93

Dtd

. 17.

08.2

016

33

7 V

ishn

u N

ambo

othi

ri P

erin

gom

e Ta

lipar

amba

1

44/1

0.

0959

17

7/16

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MM

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CR

PS/

21.0

8.17

S/o

San

kara

n N

ambo

othi

ri,K

arin

gula

thill

am,

H

ecta

re

DO

C/M

-283

5/16

A

thav

anad

.P.O

., M

alap

pura

m 6

76 3

01

Dtd

. 22.

08.2

016

33

8 R

enil.

T.C

. P

utho

or

Thal

asse

ry

7/1

14

.62

178/

16-1

7/M

M/L

T/C

RPS

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17

S

/o S

reed

hara

n, T

.C.N

ivas

,

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D

OC

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191/

16

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rupa

ram

ba.P

.O. 6

70 6

93

Dtd

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08.2

016

33

9 S

unny

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aham

K

elak

om

Iritty

K

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29

0.09

71

179/

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7/M

M/L

T/C

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17

S

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brah

am, A

rakk

al H

ouse

,

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tare

D

OC

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392/

16

Kan

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r.P.O

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674

D

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6

340

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an.M

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Ala

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Talip

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478

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t 0.

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18

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MM

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CR

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21.0

8.17

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Dav

id J

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h, M

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il H

ouse

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tare

D

OC

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316/

16

Pet

tikku

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P.O

., K

asar

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671

313

D

td. 2

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6

341

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Pad

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ry

2 0.

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18

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MM

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CR

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24.0

8.17

S/o

Kum

aran

, Tha

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enm

anal

Hec

tare

D

OC

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467/

16

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hara

kkan

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.O. 6

70 6

12

Dtd

. 25.

08.2

016

34

2 P

utha

n Pa

ram

bil J

osep

h Th

omas

, K

elak

om

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25

6 0.

0931

18

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MM

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CR

PS/

28.0

8.17

Jibi

n N

ivas

,

Hec

tare

D

OC

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192/

16

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r.P.O

. 670

651

D

td. 2

9.08

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6

343

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2

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0.

0971

18

3/16

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MM

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CR

PS/

28.0

8.17

S/o

Jos

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nass

eri H

ouse

,

Hec

tare

D

OC

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227/

16

Per

ikko

de.P

.O. 6

70 6

31

Dtd

. 29.

08.2

016

34

4 A

shok

an.A

. M

anan

ther

i Th

alas

sery

2

5/2B

1 0.

0971

18

4/16

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MM

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CR

PS/

28.0

8.17

S/o

Gov

inda

n, P

alliy

ath

Hou

se,

H

ecta

re

DO

C/M

-323

5/16

M

anan

ther

i.P.O

. 670

643

D

td. 2

9.08

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6

345

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ekum

ar.M

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lapp

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b Ta

lipar

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4

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0.09

71

185/

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M/L

T/C

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17

S

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anga

dhar

an, K

uthi

rum

mal

Hou

se,

H

ecta

re

DO

C/M

-331

7/16

V

aliy

apoy

il.P

.O. 6

71 3

13

Dtd

. 29.

08.2

016

34

6 S

anth

osh.

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idiy

enga

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lipar

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8

0.09

71

186/

16-1

7/M

M/L

T/C

RPS

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17

S

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anna

n, P

uthi

ya P

uray

il H

ouse

,

Hec

tare

D

OC

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648/

16

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aral

am.P

.O. 6

70 6

02

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08.2

016

34

7 D

evas

sya

Nid

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ga

Talip

aram

ba

1/1

0.

0971

18

7/16

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MM

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CR

PS/

30.0

8.17

S/o

Jos

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Ikka

ra H

ouse

,

Hec

tare

D

OC

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837/

16

Che

mbe

ri.P

.O. 6

70 6

32

Dtd

. 31.

08.2

016

34

8 D

amod

hara

n.P

. M

alap

patta

m

Talip

aram

ba

84/

1 0.

1942

18

8/16

-17/

MM

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CR

PS/

30.0

8.17

S/o

Rag

hava

n.V

.V.,

Van

nath

anka

ndi H

ouse

,

Hec

tare

D

OC

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448/

16

Per

uval

athu

para

mba

.P.O

. 670

593

D

td. 3

1.08

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6

349

Ram

acha

ndra

n.M

. K

eezh

ur

Thal

asse

ry

43/

1 0.

0971

18

9/16

-17/

MM

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CR

PS/

30.0

8.17

S/o

Kris

hnan

Nam

biar

, Kris

hna

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yam

Hec

tare

D

OC

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449/

16

Mat

tann

ur 6

70 7

02

Dtd

. 31.

08.2

016

35

0 A

ppuk

utta

n.P

.P.

Ala

ppad

amb

Talip

aram

ba

396

/2

0.08

9 19

0/16

-17/

MM

/LT/

CR

PS/

30.0

8.17

S/o

Kun

ham

bu, P

adin

ghar

e Pu

rayi

l Hou

se,

H

ecta

re

DO

C/M

-259

8/16

K

ozhu

mm

al.P

.O. 6

70 5

21

Dtd

. 31.

08.2

016

35

1 P

.P.H

amza

Kut

ty,

Kal

liad

Iritty

4

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0.09

71

191/

16-1

7/M

M/L

T/C

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17

S

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Haj

i, Pa

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di

Put

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P

uray

il

Hec

tare

D

OC

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516/

16

Kol

ache

ri.P

.O. 6

70 6

01

Dtd

. 31.

08.2

016

35

2 M

uham

med

Raf

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e

Kal

liad

Iritty

4

6/4

0.09

71

192/

16-1

7/M

M/L

T/C

RPS

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17

S

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rahi

m.P

.T.,

Par

atho

di H

ouse

,

Hec

tare

D

OC

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322/

16

P.O

.Ana

kkay

am, M

alap

pura

m 6

76 5

69

Dtd

. 31.

08.2

016

35

3 B

ijesh

.K.P

. M

ayyi

l Ta

lipar

amba

5

57/1

0.

0971

19

3/16

-17/

MM

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CR

PS

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.09.

17

S

/o B

alak

rishn

an, R

MB

Hou

se,

H

ecta

re

DO

C/M

-339

3/16

C

heru

pazh

assi

.P.O

. 670

601

D

td. 0

5.09

.201

6

354

Sur

esha

n C

huzh

ali

Talip

aram

ba

30

0.09

72

194/

16-1

7/M

M/L

T/C

RPS

/ 07

.09.

17

S

/o N

aray

anan

, Man

i Hou

se,

H

ecta

re

DO

C/M

-348

3/16

K

allia

sser

i, A

njar

akka

ndi.P

.O. 6

70 3

31

Dtd

. 08.

09.2

016

35

5 B

alak

rishn

an.K

. K

allia

d Iri

tty

22

0.09

71

195/

16-1

7/M

M/L

T/C

RPS

/ 18

.09.

17

S

/o K

umar

an, A

njal

i Niv

as,

H

ecta

re

DO

C/M

-337

9/16

P

.O.C

hattu

kapp

ara

670

602

Dtd

. 19.

09.2

016

35

6 B

inoy

.M.M

. K

allia

d Iri

tty

1 0.

0971

19

6/16

-17/

MM

/LT/

CR

PS/

18.0

9.17

S/o

Mat

hai.M

.J.

H

ecta

re

DO

C/M

-349

4/16

M

azhu

ppel

Hou

se, C

ham

atha

chal

.P.O

. 670

63

3

D

td. 1

9.09

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6

357

Cha

ndra

n.K

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ga

Talip

aram

ba

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19

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S

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unha

mbu

, Kun

nath

Val

appi

l Hou

se,

H

ecta

re

DO

C/M

-299

2/16

C

heng

alay

i.P.O

. 670

631

D

td. 1

9.09

.201

6

358

K.V

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hnan

K

allia

d Iri

tty

46

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24

198/

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.09.

17

S

/o N

aray

anan

, Lak

shm

i Niv

as,

C

ent

DO

C/M

-359

6/16

P

.O.E

daya

nnur

670

595

D

td. 1

9.09

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6

359

Sha

ji P

ayam

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60

0.09

71

199/

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M/L

T/C

RPS

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.09.

17

S

/o M

atha

i, M

amoo

ttil H

ouse

,

Hec

tare

D

OC

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521/

16

Mad

athi

l, P

.O.Ir

itty

670

703

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09.2

016

36

0 P

rasa

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P

ayam

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20

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MM

/LT/

CR

PS/

21.0

9.17

S/o

Kar

unak

aran

, Asw

athi

Hou

se,

H

ecta

re

DO

C/M

-249

9/16

P

adiy

oor.P

.O. 6

70 7

03

Dtd

. 22.

09.2

016

36

1 S

ham

sudh

een.

S.V

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ram

am

Talip

aram

ba

449

0.09

71

201/

16-1

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17

S

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bdul

Kar

eem

Hec

tare

D

OC

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599/

16

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il H

ouse

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hil.P

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70 3

07

Dtd

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016

36

2 R

aju.

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mam

Ta

lipar

amba

3

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0.09

71

202/

16-1

7/M

M/L

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17

S

/o N

aray

anan

, Cha

man

di, P

oora

kkad

avat

h

Hec

tare

D

OC

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682/

16

Hou

se, K

utto

or.P

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70 3

06

Dtd

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016

36

3 S

rees

han.

K.

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ari

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asse

ry

21/

1 0.

0971

20

3/16

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MM

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CR

PS/

25.0

9.17

S/o

Kun

hira

man

, Am

man

athi

l Hou

se,

H

ecta

re

DO

C/M

-273

5/16

E

daya

nnur

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. 670

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6

364

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Per

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atta

Ta

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71

204/

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17

S

/o T

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bu, K

azha

kakk

aran

Hou

se,

H

ecta

re

DO

C/M

-323

4/16

P

urak

kunn

u.P

.O. 6

70 3

01

Dtd

. 26.

09.2

016

36

5 S

aju.

M.V

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erin

gom

e Ta

lipar

amba

1

45/1

0.

0961

20

5/16

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MM

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CR

PS/

25.0

9.17

S/o

Var

key,

Mat

tath

ilani

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Hou

se,

H

ecta

re

DO

C/M

-317

0/16

P

uthi

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m.P

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4

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366

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ingo

me

Talip

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ba

162

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Am

badi

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n H

ouse

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tare

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126/

16

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tikku

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671

313

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6

367

Bal

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3 0.

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20

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MM

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27.0

9.17

S/o

Nar

ayan

an, E

lam

bayi

l Hou

se,

H

ecta

re

DO

C/M

-234

2/16

U

liyil.

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. 670

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8.09

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6

368

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oop.

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uzha

kkun

nu

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20

6 0.

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20

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MM

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CR

PS/

27.0

9.17

S/o

Moh

anan

, Sre

ehar

i Niv

as,

H

ecta

re

DO

C/M

-363

3/16

P

.O.V

ilakk

ode

670

703

Dtd

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09.2

016

36

9 R

ajee

v.T.

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tty

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209/

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17

S

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yyap

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H

ecta

re

DO

C/M

-330

8/16

Th

anik

kapa

ram

bil

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se,

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kal.P

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670

705

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016

37

0 P

raka

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ekan

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lipar

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1

61/1

0.

0971

21

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MM

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CR

PS/

27.0

9.17

S/o

Ram

an, R

amap

uram

Hou

se,

H

ecta

re

DO

C/M

-268

6/16

C

heru

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assi

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. 670

601

D

td. 2

8.09

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6

371

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anan

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anth

ali

Talip

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ba

183

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71

211/

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17

S

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hava

n, P

arat

hi H

ouse

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tare

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OC

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498/

16

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akko

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70 3

05

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09.2

016

37

2 M

uham

med

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hi.C

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erin

gom

e Ta

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16

1 0.

0971

21

2/16

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CR

PS/

02.1

0.17

S/o

Abo

obac

ker,

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ruku

nnon

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se,

H

ecta

re

DO

C/M

-330

6/16

Ta

lipar

amba

670

14

Dtd

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016

37

3 B

alam

ani.K

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Kan

kol

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ba

191

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71

213/

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17

D

/o C

hiru

kand

an, K

uthi

rum

mal

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se,

H

ecta

re

DO

C/M

-332

8/16

P

.O.K

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l 670

307

D

td. 0

3.10

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6

374

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mer

S

reek

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m

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aram

ba

235

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71

214/

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17

S

/o M

ayan

, Raf

seen

as,

H

ecta

re

DO

C/M

-380

5/16

A

ncha

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612

D

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6

375

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kara

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aman

thal

i Ta

lipar

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1

86/9

0.

081

215/

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17

S

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aray

anan

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ile V

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ouse

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OC

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164/

16

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akko

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.O. 6

70 3

05

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10.2

016

37

6 S

haji

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son

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or

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0.

089

216/

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17

S

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argh

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OC

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922/

16

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5

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6

377

Sun

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21

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S/o

Kun

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man

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bala

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se,

H

ecta

re

DO

C/M

-308

0/16

P

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670

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6

378

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ta

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78/

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71

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17

S

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ovin

dan,

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ichi

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se,

H

ecta

re

DO

C/M

-363

7/16

Th

avid

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ri, P

.O.P

orak

kunn

u 67

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6

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td. 0

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6

379

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m

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754

0.09

71

219/

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17

S

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ham

med

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ty, E

llikka

l Hou

se,

H

ecta

re

DO

C/M

-385

6/16

P

.O.M

ulla

kodi

670

602

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6

380

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42

220/

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17

S

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bdu

Rah

iman

, Sub

aida

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zil

H

ecta

re

DO

C/M

-319

9/16

M

ayyi

l 670

602

D

td. 0

3.10

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6

381

K.K

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hava

n,

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ga

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ba

41

0.09

71

221/

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17

S

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aray

anan

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undh

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tiatt

Hou

se,

H

ecta

re

DO

C/M

-377

6/16

P

.O.P

erik

kode

670

631

D

td. 0

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382

Mat

hew

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Ta

lipar

amba

3

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0976

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CR

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Mat

hai P

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ouse

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16

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32

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10.2

016

38

3 B

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1

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71

223/

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17

S

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ugus

ty, P

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ulan

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Hou

se,

H

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re

DO

C/M

-319

2/16

K

elak

om.P

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74

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10.2

016

38

4 Jo

y Jo

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0.

0971

22

4/16

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MM

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CR

PS/

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0.17

s/o

Jose

ph, M

ulla

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l Hou

se,

H

ecta

re

DO

C/M

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5/16

P

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670

631

D

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6

385

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od

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225/

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17

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amm

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se,

H

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re

DO

C/M

-352

8/16

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adan

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01

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10.2

016

38

6 S

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42

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71

226/

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17

S

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476/

16

P.O

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31

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10.2

016

38

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avid

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reek

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m

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17

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6

P

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31

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016

38

8 Li

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May

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560

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71

228/

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17

S

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alan

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ya H

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OC

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904/

16

P.O

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rupa

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01

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10.2

016

38

9 Jy

othi

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mas

P

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lipar

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1

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71

229/

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7/M

M/L

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17

S

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hom

as.P

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Hou

se,

H

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re

DO

C/M

-268

1/16

K

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a.P.

O. 6

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06

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016

39

0 S

anil.

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Kal

liad

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4

6/4

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71

230/

16-1

7/M

M/L

T/C

RPS

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17

S

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.K.S

athy

an

H

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re

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C/M

-363

2/16

S

alee

na N

ivas

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02

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016

39

1 To

min

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ayya

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1

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71

231/

16-1

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17

S

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eorg

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se,

H

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re

DO

C/M

-395

2/16

C

hem

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D

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6

392

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him

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ga

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ba

31/

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0.

0971

23

2/16

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MM

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CR

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S/o

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kan

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16

P.O

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670

633

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4.10

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6

393

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i.C.

Kal

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4

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71

233/

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17

S

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anna

n, C

happ

adi H

ouse

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tare

D

OC

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948/

16

P.O

.Kal

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670

593

Dtd

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10.2

016

39

4 D

ipes

h S

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Pay

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ba

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23

4/16

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MM

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CR

PS/

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,

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tare

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OC

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003/

16

Kak

ilam

para

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., C

hem

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670

632

Dtd

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10.2

016

39

5 S

adan

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ram

am

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ba

447

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71

235/

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17

S

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an, T

huru

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alli

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se,

H

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re

DO

C/M

-352

4/16

N

arik

kam

valli

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andu

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504

D

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7.10

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6

396

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l Kum

ar.M

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mam

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2

55/1

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23

6/16

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MM

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CR

PS/

16.1

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S

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Kar

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aran

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appi

l H

ouse

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Hec

tare

D

OC

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595/

16

Man

dur.P

.O. 6

70 5

01

Dtd

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10.2

016

39

7 S

ures

h B

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V.

Kal

liad

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4

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71

237/

16-1

7/M

M/L

T/C

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17

S

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agha

van.

K., I

ndee

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m H

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,

Hec

tare

D

OC

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992/

16

Kod

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ram

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tann

ur.P

.O. 6

70 5

95

Dtd

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10.2

016

39

8 C

.Ram

esha

n M

aniy

oor

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aram

ba

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30/

0.09

71

238/

16-1

7/M

M/L

T/C

RPS

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17

S

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ovin

dan,

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ivas

,

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45

Hec

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D

OC

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16

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ttuka

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.O. 6

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92

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10.2

016

39

9 R

ajee

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tiatto

or

Talip

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76/

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71

239/

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17

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chut

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945/

16

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601

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td. 1

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6

400

Rad

ha.K

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24

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401

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as,

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C/M

-352

5/16

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70 6

43

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40

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242/

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17

S

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andi

Hou

se,

H

ecta

re

DO

C/M

-400

9/16

M

adat

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P.O

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y 67

0 70

3

D

td. 1

7.10

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6

403

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u N

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71

243/

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M/L

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17

S

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anan

, Kar

att K

olla

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H

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DO

C/M

-377

9/16

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osav

anva

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70 5

93

Dtd

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10.2

016

40

4 S

umes

h.K

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mam

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42/1

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24

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S/o

Kan

nan,

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l Hou

se,

H

ecta

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DO

C/M

-330

7/16

P

.O.P

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kunn

u 67

0 30

6

D

td. 1

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6

405

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oj K

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17

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43

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016

40

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Ta

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71

246/

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17

S

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umar

an, C

hem

bach

eri H

ouse

,

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tare

D

OC

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979/

16

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uval

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670

593

D

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407

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478

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247/

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S

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.V.K

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C/M

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2/16

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.V.K

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670

307

D

td. 1

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6

408

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248/

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17

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95

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249/

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M/L

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17

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742/

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93

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016

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0 P

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25

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31

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41

1 M

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lapp

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4

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25

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C/M

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3

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6

412

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amm

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056/

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04

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3 N

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liad

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71

253/

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17

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Hou

se,

H

ecta

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DO

C/M

-218

9/16

K

adam

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Mal

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676

553

D

td. 1

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6

414

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N

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25

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MM

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CR

PS/

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S/o

Kan

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i Val

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l Hou

se,

H

ecta

re

DO

C/M

-405

1/16

P

.O.N

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670

631

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td. 1

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6

415

Geo

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S/o

Kud

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n,

H

ecta

re

DO

C/M

-319

3/16

K

udic

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Poo

para

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632

D

td. 1

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6

416

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17

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C/M

-352

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Pay

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19

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16

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42

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263/

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C/M

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athi

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303

D

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6

424

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hava

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ta

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26

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C/M

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D

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6

425

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C/M

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8/16

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31

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02

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948/

16

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C/M

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.O.K

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602

D

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430

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73

270/

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17

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C/M

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6/16

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432

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17

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71

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17

S

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32

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71

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C/M

-377

7/16

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93

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43

5 M

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aman

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2

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27

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43

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43

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27

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43

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27

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16

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310

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438

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27

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ha

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hi

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ent

DO

C/M

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6/16

P

allik

kunn

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70 0

04

Dtd

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11.2

016

43

9 U

.Man

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2

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27

9/16

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Kan

nan,

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ouse

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tare

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OC

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250/

16

P.O

.Kut

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or 6

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02

Dtd

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11.2

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44

0 M

uham

med

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6

1. District Resource Map, Kannur district, Kerala. Pubished by Geological Survey of India.

2. Detailed Information on Bauxite in India Geological Survey of India. 1994. Retrieved from

http://www.portal.gsi.gov.in/gsiDoc/pub/DID_Bauxite_WM.pdf Rajan, T. N. and Anil

Kumar, P. S. 2005.

3. Geology and Mineral Resources of the States of India Part IX Kerala. Geological Survey

of India Miscellaneous Publication No. 30.

4. Subramani S. M. 2013. Ground Water Information Booklet of Kannur district, Kerala.

ter Board.

5. www.dmg.kerala.gov.in

6. www.kerenvis.nic.in

7. www.keralasoils.gov.in

http://www.portal.gsi.gov.in/gsiDoc/pub/DID_Bauxite_WM.pdf

http://www.dmg.kerala.gov.in

http://www.kerenvis.nic.in

http://www.keralasoils.gov.in

Annexure 1: Geology of Kerala

Geology of Kerala

Physiography

Physiographically the state can be divided into four domains from east to west, viz., the Western

Ghats, the foothills, the midland and the coastal lowland.

Western Ghats

The hill ranges of the Western Ghats rise to an altitude of over 2500m above the MSL and the crest

of the ranges marks the inter-state boundary in most of the places. A breach in the continuity of the

ranges marks the Palghat Gap with a sinistral shift of 50 km between the shifted crests. The Wynad

plateau and the Munnar (10 57'00": 77 31'00") upland fall within this zone.

Foothills

The foothills of the Western Ghats comprise the rocky area from 200 to 600m.above MSL. It is a

transitional zone between the high -ranges and midland.

Midland region

This forms an area of gently undulating topography with hillocks and mounds. Laterite capping is

commonly noticeable on the top of these hillocks. The low, flat-topped hillocks forming the laterite

plateau range in altitude from 30-200m and are observed between coastal low-land and the foothills.

Coastal lowland

Coastal low-land is identified with alluvial plains, sandy stretches, abraded platforms, beach ridges,

raised beaches, lagoons and estuaries. The lowland and the plains are generally less than 10m above

MSL.

Rivers

Kerala is drained by 44 rivers, many of which orginate from the Western Ghats. Except Kabini,

Bhavani and Pambar which are east - flowing, the rest of rivers are west- flowing and join the Arabian

Sea. A few of them drain into the backwaters. Most important rivers (with their length in km in

paranthesis) of the state, are Chandragiri(105), Valapatnam (110), Achankovil (120) Kallada (121),

Muvattupuzha (121), Chalakudy (130), Kadalundi(130), Chaliyar (169), Pampa (176),Bharathapuzha

(209) and Periyar (244).

Geology

Geologically, Kerala is occupied by Precambrian crystallines, acid to ultra basic intrusives of

Archaean to Proterozoic age, Tertiary (Mio-Pliocene) sedimentary rocks and Quaternary sediments

of fluvial and marine origin (Fig.I). Both the crystallines and the Tertiary sediments have been

extensively lateritised.

Based on the detailed studies by GSI during the last three decades, the following stratigraphic

sequence has been suggested.

Archaeans

Rocks of Archaean Era encompass a wide spectrum of litho-assemblages ranging from khondalite,

charnockite, gneiss and meta-sedimentary rocks occupying the Western Ghats including the

foothill region. The Khondalite and Charnockite Group are correlated with the Eastern Ghat

Supergroup based on the overall similarity in lithology and geochronology.

Wynad Supracrustals

The meta-sedimentary, and ultramafic rocks occurring in the Wynad District generated keen

interest among the GSI geologists in 1970s. The high-grade Wynad supracrustal rocks are

correlated with the Sargur Schist Complex of the Karnataka (Nair, et al, 1975; Adiga, 1980). The

schistose rocks are characterised by intense deformation, medium to high-grade metamorphism,

migmatisation and lack of sedimentary structures. The schist complex consists of meta-

ultramafites, schist, meta-pelites, meta-pyroxenite, serpentinite, talc-tremolite rock and

amphibolite.

The meta-sedimentaries occur as thin linear bodies within the migmatites. These consist of pelites,

psammopelites and quartzites. The predominant rock types are corundum- mica schist, kyanite

schist, quartz- mica schist and iron stone.(Anil Kumar et al,1993).

These rocks occur as narrow arcuate belts, lenses, and other forms of enclaves within Peninsular

gneisses and charnockite. The group can be divided into medium-to low- grade metasedimentary

rocks and meta-mafic and meta-ultramafic rocks. The lithology of the high-grade schists consist

of quartz-mica schist with kyanite, quartz-sericite schists,quartzites,magnetite quartzite, fuchsite

quartzite and meta-ultramafites. Their contact with the surrounding gneisses are concordant due

to later co-folding. Several linear belts of such high-grade schists and ultramafite enclaves occur

as isolated bands within the granulite and gneissic terrain of Kasaragod and Kannur districts.

Layered ultrabasic- basic complex

Remnants of layered basic- ultabasic complex are reported from Attappadi area(Nambiar

1982).The ultramafics are represented by meta-pyroxenite, meta-dolerite, peridotite with chromite

and meta-gabbro (Lahiri et al, 1975). The anorthosite of Attappadi is only a few metre thick.

Occurrences are around Narsimukku, Pudur and Melmulli areas. An east-west trending narrow

lenticular body of serpentinised dunite is reported from Punalur mica mine belt.

A minor body (200 m long and 10-15m wide) of anorthosite was reported within pyroxene-

granulite-charnockite terrain from Katanjari parambu of Kasargod district (Adiga, 1979).

Another dismembered layered igneous complex consisting of alternate layers of peridotite and

pyroxenite within charnockite was traced around Panathadi area of Kannur District (Adiga,

1980).

Peninsular Gneissic Complex- I (PGC-I)

The rocks of Peninsular Gneissic Complex(PGC) are exposed in the northern parts of Kerala

adjoining Karnataka . This consists of a heterogeneous mixture of granitoid materials. The

equivalent rocks of PGC in Kerala include hornblende-biotite gneiss (sheared), biotite-

hornblende gneiss, foliated granite and pink granite gneiss. Granite gneiss is exposed along the

intra-State boundary of Palakkad District as well as in Idukki District. Pink granite gneiss,

though widespread, is best developed in Devikolam (10 04'00": 77 06'30"), and

Udumbanchola (10°00'00":77°15'00") areas of Idukki District.

This consists of gneisses showing preponderance of either hornblende or biotite. The

percentage of hornblende and biotite varies from place to place. This can be traced from

Manantoddy to further northwest upto the west coast. West of Manantoddy, the rock is

hornblende gneiss. It shows coarse granulitic to gneissic texture and is composed of

hornblende, feldspar, quartz, pyroxene, biotite and garnet. Alkali feldspar shows alteration to

clay and sericite. Biotite is mainly secondary after hornblende.

Around Mahe and Thalasseri, the biotite gneiss(Nair et al., 1974) is medium-grained and

gneissose rock consisting of alternate layers of mafics and felsics.

Khondalite Group

The Khondalite Group of rocks include calc-granulites, quartzite and para-gneisses of pelitic

parentage. Para-gneisses are ubiquitous and are well-developed in the southern part of the state,

particularly, in Thiruvananthapuram and Kollam districts. Calc-granulite and quartzite occur

as bands within the para-gneisses and amidst the Charnockite Group and migmatitic gneisses.

Calc-granulite

Calc-granulite occurs as linear bands mainly in the eastern part of Kollam and

Thiruvananthapuram District, northeast and east of Munnar in Idukki district and in parts of

Palakkad District. The rock is generally medium to coarse-grained, inequigranular and

granoblastic in texture. It consists of diopside and plagioclase. Minerals like wollastonite,

scapolite, calcite, garnet, spinel, sphene, quartz and apatite are also present in different

proportions.

Quartzite

Quartzite occurs as linear bands amidst the khondalitic gneiss, charnockite and migmatitic

gneisses. These bands are exposed between Pathanamthitta (9 15'45": 76 47'00"), and

Muvattupuzha (9 59'00": 76 35'00") in Ernakulam District. The rock is coarse-grained and

generally white in color with a brownish coating on the weathered surface. It consists of

granular quartz with subordinate feldspar, garnet and iron oxide.

Garnetiferous biotite-sillimanite gneiss

Garnetiferous biotite- sillimanite gneiss is well-developed in the southern part of the state. It

occurs in close association with the migmatitic gneisses, charnockite and charnockite gneisses,

mostly as weathered outcrops. Sillimanite- rich bands occur alternating with garnet - rich

portions or with quartzo-feldspathic layers. Rutile and iron oxides are the common accessory

minerals.

Charnockite Group

Charnockite Group shows great diversity in lithology comprising pyroxene granulite,

hornblende pyroxenite, magnetite quartzite, charnockite and hypersthene-diopside gneisses

and cordierite gneiss. Charnockite and charnockitic gneiss have preponderance over all other

crystalline rocks covering 40 -50% of the total area of the State. The charnockites are well-

exposed in the central and northern parts of Kerala including the high hills of the Western

Ghats. Char nockite has lesser predominance in Thiruvananthapuram and Kollam districts. In

Attappady, the Bhavani Shear Zone is limited by the charnockite massif of the Nilgiri plateau

on the north. Though the interrelationship of the Charnockite and the Khondalite is not clear,

in many places there are intercalations rather than interlayering of one with the other. In

Palakkad District, the Khondalite Group of rocks structurally overlie the charnockite. The

occurrence of pyroxene granulite as fine and linear bodies within the charnockite of Tirur,

suggests that charnockite is a product of migmatisation of pyroxene granulite(Vidyadharan and

Sukumaran, 1978). Charnockite and charnockitic gneiss consist of quartz, feldspar and biotite.

Garnet-bearing variants are also observed. The basic charnockite is more granulitic and

contains clino- and ortho- pyroxenes, feldspar, biotite and garnet whereas the acid variety

(alaskite/ enderbite) is greenish black, coarse-grained, massive to poorly foliated rock

consisting of quartz, feldspar and pyroxenes. Basic charnockite has low- potash feldspar and

more clinopyroxene. This is devoid of garnet and graphite, but shows a little amount of

biotite(Chacko, 1922). Due to the polygenetic nature of the rock, geochemical and

mineralogical variations do exist between charnockites reported from Kerala. In the Periyar

valley region, in Idukki and Kottayam districts, pyroxenite and alaskite constitute the

Charnockite Group (Nair, and Selvan, 1976).

The available age data indicate that the massive charnockites are older and their ages range

between 2155 and 2930 + 50 Ma (Soman ,1997).

Also charnockite has been subjected to retrogression and migmatisation.

Archaean to Palaeo-Proterozoic

Vengad Group

A succession of schistose rocks in parts of Tellicherry taluk in Kannur district is described as

Vengad Group of rocks (Nair, 1976). The Vengad Group comprises of basal conglomerate,

quartzite and quartz-mica schist. The contacts are highly gradational. The conglomerate shows

graded bedding and quartzite shows current-bedding.

An angular unconformity marked by conglomerate horizon extending from Kuthuparamba

(11 34'00") to Vengad (11 32'00") in Kannur district, separates the

younger quartz-mica schist and quartzite from the older schistose and gneissic rocks. The

lithology consists of basal oligomictic conglomerate, quartzite, quartz-biotite-muscovite schist

and biotite quartzite. The schists are exposed over an area of 300 sq km having a lensoidal

shape with its longer axis trending in NW-SE direction. The basement rock is gneissic or

migmatitic with relicts of high-grade schists, ultramafites and quartzites of the Wynad Schist

Complex. Four major occurrences of conglomerate are noticed in a NW-SE direction over a

length of 10 km.

Lack of migmatisation, presence of primary structures and low-grade metamorphic minerals

characterize these rocks.

Migmatite\ Gneiss\ Granitoid (PGC-II)

Quartzo-feldspathic gneiss

Migmatite includes variety of gneissic rocks which are next in importance to charnockite as a

dominant litho-assemblage. Quartzo-feldspathic gneiss occurring along the contact zone

between garnet-biotite gneiss and garnet-sillimanite gneiss of Thiruvananthapuram area

represents an original intrusive phase. It is a feebly foliated, fine-grained, leucocratic granulitic

rock occurring in close association with garnet-sillimanite gneiss and garnet-biotite gneiss with

gradational contact relationship in the southern parts of Kerala. The origin of this rock is

attributed to stress-induced injection of acid materials into the host rocks(Nageswara Rao and

Raju,1970).

Garnet- biotite gneiss

Garnet-biotite gneiss is well-developed in the northeastern parts of Kollam and

Thiruvananthapuram districts. This carries inclusions of pyroxene granulite and disseminations

of graphite at many places (Jacob, 1965). It consists of quartz, microperthite, biotite,

plagioclase and graphite. This rock also occurs in the northern parts of Palakkad District in

close association with khondalite, charnockite and hornblende gneiss. These rocks are

subsequently formed by retrogression and migmatisation of the Khondalite Group.

East of Kottayam and Idukki districts, light grey, pink garnet-bearing biotite gneiss is widely

seen. It is a gneissic granulite. The presence of biotite and concentration of garnet in layers

give the rock a banded appearance.(GSI, 1995).

Hornblende gneiss, hornblende-biotite gneiss, quartz- mica gneiss

These rock types occur within the migmatites and associated retrograded charnockite. The

naming is purely based on the preponderance of the minerals and these rocks occur in the

Periyar valley area east of Thodupuzha.(Nair and Selvan,1976). These medium-grained ,

foliated, banded rocks consist of alternate layers rich in hornblende or biotite. Bands of coarse

to medium- grained light grey to pink granite traverse these rocks. Hornblende- biotite gneiss

showing lit par lit relationship with the granite gneisses is the dominant rock type in the Periyar

valley. This is admixed with contorted bands and enclaves of pyroxene granulite, calc-

granulite and hornblende- biotite granulite. These are highly deformed.

In the Palakkad gap area, these gneisses occur over a large area, showing migmatitic structures

such as agmatites, nebulites, schlierens, ptygmatic folds, quartzo-feldspathic neosomes and

ferromagnesian palaeosomes.(Muraleedharan and Raman, 1989).

Proterozoic

Basic intrusives

Basic dyke emplacements within the Archaean crystalline rocks of Kerala are spread

throughout the entire length and breadth of the state. Of these, dolerite dyke occurring north of

the Palakkad gap had given Proterozoic age whereas in the south this dyke is of Phanerozoic

age. The older basic dykes are metamorphosed along with the country rocks and are now

recognised as epidiorite and amphibolite. Another set of dykes, apparently post-dating the

regional metamorphic event are subjected to thermal metamorphism. Clouding and

sericitisation of feldspars and uralitisation of pyroxenes are common in such dykes. In the

absence of chronological data such dykes are considered to be of Proterozoic age. Most of the

dykes are vertical in disposition and are traced as linear features. En-echelon pattern of some

dyke swarms suggests that magmatic intrusion was controlled by shearing of the host rock.,

Mineralogically, the dykes are made up mostly of plagioclase feldspar and pyroxene(augite

and aegirine-augite) with magnetite, apatite and olivine as accessories. The ENE-WSW dolerite

dyke swarm of Agali- Anakkati area in Palakkad District within the Bhavani Shear zone

showed in isotopic age from 1900 to 2000 Ma (Radhakrishna and Mathew Joseph, 1993). The

rock is highly jointed and altered (Jacob, 1965). Similar basic intrusive bodies are traced in the

Achankovil shear zone in Vazhamuttam (9 14'00":76 46'40"), Kulasekhara pettah

(9 16'00":76 47'45") (Thomas Mathai et al, 1984). Sheet-like bodies of fine to medium-

grained, dark coloured meta-gabbro occurs in Periyamuli (11 13'00"; 76 43'00") for about 20

km in ENE-WSW direction, Karuvarai (11 04'00"; 76 32'30") and few gabbro bodies south of

Thuvapattu (11 06'30"; 76 44'45") in Attapady valley, Palakkad district. Meta-gabbro forms

small hillocks east of Payyanam (10 31'00"; 76 21'00"), southwest of Kainur (10 36'00";

76 09'00") and Chemmannur (10 41'00"; 76 01'00"), Vaga (10 35'00"; 76 06'00") and Arthat

(10 37'00"; 76 03'00") in Trichur District (Mahadevan, 1962).

Dykes in north Kerala show , NW-SE, NE-SW and NNW-SSE trends. Host rocks are

charnockite, gneisses and supracrustals(Radhakrishna et al 1991). Dykes are mainly dolerite

but occasional meta-gabbro or meta-norite are also traced. In Agali- Anaikatti area of the

Attapadi- Bhavani shear zone, dykes are confined within a 20-25km wide zone and extend

from west of Agali to eastward for about 100km following a ENE-WSW

direction.(Radhakrishna, et al, 1999).

The rock consists of 95% calcic plagioclase, 5% clinopyroxenes and subordinate amounts of

magnetite. There are a number of concordant and discordant basic intrusive of dolerite and

gabbro,meta-gabbro, meta-norite, meta-pyroxenite and anorthositic gabbro. These are not

mappable and are seen in Pappinpra (11o06'20", 76o05'56") Velli(11o04'00":76o07'45"),

Kalpetta (11o04'12":76o05'32). An extensive basic diorite has been mapped over an area of 25

sq km at Panavalli (11o53'30",76 o 2'30"; Nair, et al 1976).

The rock is composed predominantly of calcic plagioclase (95%) rest clinopyroxene with

subordinate amount of magnetite. Another relatively small body of anorthosite is around

Kalivalli (11 51'30"; 76 12'30") in south Wynad taluk, Wynad District.

Ultrabasic/ basic intrusive (younger)

Perinthatta Anorthosite

A major elliptical body of anorthosite spread over an area of more than 50 sq.km is reported

from Perinthatta (12o10'00":75o17'30";Vidyadharan et al, 1977). The anorthosite is with a very

irregular border and a tongue-like projection into the country rock of charnockite and pyroxene

granulite of Kannur District.The anorthosite is coarse to very coarse-grained, and shows

variations from pure anorthosite to gabbroic anorthosite and gabbro from the centre to the

periphery suggestive of zoning. The modal composition corresponds to nearly 95% plagioclase

(An 58-72) and <10% clinopyroxene, apatite, calcite and magnetite. The gabbroic variants have

more of mafics.

The structural configuration suggests that the anorthosite was emplaced in synformal structure

as a phacolith. The flow-banding in anorthosite indicates its syntectonic emplacement. The

Perinthatta anorthosite is assigned a Proterozoic age.

Ezhimala gabbro-granophyre complex

The major high-relief feature proximal to the Perinthatta anorthosite is constituted by the

gabbro-granophyre Complex (Nair and Vidyadharan, 1982). The granophyre massif is fringed

by the gabbro to the east and south. The Bavali fault running north of the complex is presumed

to have dismembered the body from the Perinthatta anorthosite. Locally, the gabbro has

anorthositic differentiates within it. Veins of granophyre traverse the gabbro at places give rise

to breccia-like structures. The granophyre shows a sharp contact with the gabbro into which it

intrudes. Rapakivi structure is observed within the granophyre. According to Nair and

Vidyadharan (1982) rocks of Ezhimala complex display bimodal character with conspicuous

basic and silicic components.

Kartikulam and Karraug Gabbro

Two gabbro bodies namely Kartikulam gabbro and Karraug gabbro are located northeast of

Manantoddy bordering the Karnataka (Nair et al, 1975).The gabbro body at Kartikulam

occupies an area of about 45 sq.km. with an elliptical shape within the gneissic terrain. The

actual contact with the gneiss is concealed but it is believed to be sharp. At many places, the

gabbro is agmatised by coarse quartzo-feldspathic material.

The gabbro is coarse-grained and of uneven texture consisting essentially of plagioclase and

pyroxene. Variation to anorthositic composition is noticed. The plagioclase is of labrodorite

composition and shows alteration to sericite at places (Rema Warrier and Venkataraman,

1986). The pyroxenes are uralitised to varying degrees.

The Karraug gabbro body is located east of it and south of the Kabini River. It shows similar

features as that of the Kartikulam gabbro. The rock shows phenocrysts of feldspar set in a fine

matrix of flaky minerals.

Adakkathodu gabbro

At Adakkathodu(12 31'35"; 75 10'25"), northwest of Manantoddy, a 8 km long meta-gabbro,

is intrusive into the basement gneisses on three sides and the Wynad schists in the east. It occurs

proximal to the Bavali fault/lineament. It encloses, patches of quartz-sericite schists and biotite

gneiss. (Nair et al, 1975). The rock is mesocratic to melanocratic, medium to coarse grained

consisting mainly of pyroxene and plagioclase. The rock shows sub-ophitic texture and consists

of enstatite and intermediate plagioclase of andesine-labrodorite composition (Nair et al, 1976).

While the gabbro bodies of Kartikulam and Karraug to the east are olivine- bearing, the

Adakkathodu gabbro is enstatite- bearing. Olivine, augite and zoned feldspars are recorded

from the eastern body while the western body is enstatite- bearing, without the zoning in

feldspar.

Begur diorite

An extensive basic diorite body (25 sq.km.) has been traced north of Manantoddy in the Begur

Reserve Forest (Nair, et al, 1976). It extends from Thirunelli to the Karnataka State border.

The southern contact is with augen gneisses indicating emplacement along shear zones while

the northern one with sillimanite gneisses. Aplite and dolerite veins are seen traversing the rock

mostly parallel to the regional foliation. The rock is mesocratic to melanocratic, coarse-grained

and consists of pink to grey feldspar, hornblende and biotite.

The rock is feebly gneissic and at places porphyritic (Rema Warrier and Venkataramana,

1986). The phenocrysts are mostly plagioclase. Mafics at times swerve round the phenocrysts

giving rise to augen structure. Hornblende is altered to biotite and chlorite. Accessories include

epidote, apatite, zoisite and opaques.

The diorite shows tholeiitic charcteristics.The diorite is considered as a transitional rock from

the gabbro with which it is spatially associated in the nearby area with the plagioclase become

more sodic.

Charnockites [younger]

The area south of Palakkad exposes charnockite over large areas.The charnockites are

represented by acid microperthitic charnockite and intermediate gneissic charnockite occurring

in association with garnetiferous biotite gneiss and khondalite (Narayanaswamy and Purna

Lakshmi, 1967). Massive charnockites are developed on a regional scale and occur as

mappable litho-units (Raju and Gopalakrishnan, 1972), around Nedumangad. The massive

charnockites in majority of the cases are acid and intermediate in composition. The rock is

medium to coarse-grained and shows xenoblastic texture. It is composed of quartz, feldspar,

pyroxenes, garnet and graphite with accessories like biotite, zircon, apatite and monazite.

Small patches, lenses or veins of charnockite occur in the gneisses of amphibolite facies in the

Thiruvananthapuram area (Nageswara Rao and Raju, 1970). Here, the incipient charnockites

are thought to have formed by transformation of paragneisses. (Hansen et al, 1987; Santosh et

al, 1990). A few dominant varieties of incipient charnockites have been categorized by

Ravindra Kumar and Chacko (1986) on the basis of their mode of occurrence, association and

chemical processes involved in their development. At Kottavattom, north of

Thiruvananthapuram, the charnockite consisting of quartz, K-feldspar, plagioclase, biotite,

garnet and orthopyroxene as essential minerals and graphite, zircon, ilmenite, monazite,

apatite, rutile and magnetite as accessory minerals are products of transformation of gneisses

into coarse-grained charnockites along a system of conjugate fractures and foliation planes.

(Saritha and Santosh, 1996).

Cordierite or Charnockite Gneiss

Cordierite bearing large linear zones of charnockites were reported around Pathanamthitta

(Nageswara Rao and Jacob, 1967) area. Cordierite charnockites or orthopyroxene-garnet-

cordierite bearing gneisses (Sinha Roy et al, 1984; Santosh, 1987) occur as discontinuous

bodies in the northern parts of Thiruvananthapuram and in selected stretches further south

around Koliakode. The rock is composed of cordierite, orthopyroxene, plagioclase, K-feldspar,

spinel and quartz and a little garnet and biotite.

The growth of cordierite and orthopyroxene took place concomitantly during the conversion of

gneisses to charnockites. At Nellikala in Pathanamthitta, the cordierite occurs as anhedral

grains of variable sizes in the charnockites (Nandakumar, 1996).

Younger granites

The granites and its variants occur around Chengannur in Alappuzha and Pathanamthitta

districts, Munnar in Idukki District, Peralimala in Kannur district and Kalpetta and

Ambalavayal in Wynad District. Many of these granites occur as later emplacements along

crustal fractures and faults. The Achenkovil Tamraparni tectonic zone, the Attapadi shear

zone, Bavali shear zone and the Moyar shear zone are all marked by granitic emplacements

Ambalavayal granite

The Ambalavayal (11

sq.km. The granite is light pink in color and is composed of quartz, pink feldspar, hornblende

and biotite. The pegmatites traversing the granite show occasional flakes of molybdenite. The

Amabalavayal granite occurring in the proximity of the Bavali lineament is thought to be

emplaced during its reactivation. The granite is intrusive into the hornblende-biotite gneiss

(migmatite) and the Wynad Supracrustals (Anilkumar et al, 1993). Four types of granites are

recorded, viz.,foliated granite, pink granite, grey granite and aplitic granite.

The foliated granite consists of quartz, microcline, orthoclase, plagioclase, biotite, hornblende,

chlorite, calcite and zircon .The pink granite is a medium-grained consisting of quartz,

microcline, plagioclase, sericite, chlorite, apatite, rutile, zircon and biotite. The grey granite is

a medium-to fine-grained rock consisting of quartz, microcline, sericite, biotite, chlorite and

calcite. The aplitic granite is a very fine-grained massive rock consisting of quartz, microcline,

orthoclase, plagioclase, sericite, biotite, calcite, chlorite, apatite and opaques.

K-Ar age of Ambalavayal granite (560+ 30 Ma, Nair, et al,1985) is lower than Rb-Sr age (595

+ 20 m.a Santhosh et al, 1986), but is higher than that of U-Pb-age(505+20ma, Odom,1982).

The reason for this variation in the date may be attributed to the different techniques adopted

and also to the presence of biotite of multiple generation.

Munnar granite

The Munnar (10 05'00";77 05'00") granite with an areal extent of 50 sq km is an E-W trending

irregular body emplaced within the migmatite and apophyses extend into the surrounding

gneisses. The granite dated to be 740 30 m.y (Odom, 1982) is traversed by pegmatite, aplite

and quartz veins. Three types of granite are recorded. Foliated granite, Coarse pink granite and

medium grey granite.The foliated granite consists of stringers and streaks of mafics consisting

of biotite, hornblende, chlorite and magnetite alternating with felsics consisting of quartz and

potash feldspar. Potash feldspar is predominantly orthoclase. The closely spaced foliations are

persistent but discontinuous.This granite forms a domal structure south of Munnar. It has a

sharp contact with the migmatite. Coarse pink granite consists of pink feldspar, quartz and a

little amount of mafics. Mafics are biotite, sphene and hornblende. Medium grained grey

granite, consists of quartz, feldspar, biotite, chlorite, zircon, sphene, epidote, calcite and

sericite.

Major element data of Munnar granites do not show any significant variation amongst the three

granites. Content of iron is more in medium grey granite and foliated granite. Different

variation diagrams reveal a slight tendency towards alkali granite. The foliated granite shows

more percentage of orthoclase than the other two granites. (Nair and Anil Kumar, 1990)

Ezhimala granophyre granite complex

A prominent granophyre body forms the hill known as Ezhimala, covering an area of 20 sq km

in Kannur District. The granophyre is associated with gabbro and granite and is traversed by

dolerite dykes. Two types of granophyres have been deciphered;coarse- grained leucocratic

one and medium - grained one with more mafics. Drusy type, confined to higher elevation

contain numerous vug lines with secondary minerals like quartz and calcite. Rocks of Ezhimala

Complex display bimodal character with conspicuous basic and silicic components and total

lack of rocks of intermediate composition typical of anorogenic suites (Nair and Vidyadharan,

1982). The granophyre is pink to ash grey coloured, massive, fine to coarse- grained,

holocrystalline with equigranular texture. The granites are of two types. The major light pink

granite with less of mafics show gradational relationships with the more greyish porphyritic

variant ( Varadan and Venkataraman, 1976 ).

Granophyre shows a typical granophyric intergrowth of quartz and feldspar forming the ground

mass with phenocrysts of potash feldspar and some zoned plagioclase. The groundmass is

totally of orthoclase. Augite is the chief ferro-magnesium mineral. Accessories include apatite,

sphene, epidote, calcite and magnetite. Texturally the rock shows variation from coarse-

grained leucocratic types with less mafics in the southern portion of the hill and medium to

coarse grained type towards northern parts.

Minor outcrops of rapakivi granites are recorded within the granophyres of Ezhimala Complex.

Anorthosites of Perinthatta and Kadannappally and granite, granophyre of Ezhimala together

form the Ezhimala Complex. The light pink granite with less mafics is the major variety

showing a gradational relationship with the more greyish porphyritic variety. The porphyritic

variety, at places, shows rapakivi structure. The porphyritic granite shows mantled feldspar

megacrysts. This variety grades into porphyritic granites without mantled feldspar and at higher

levels grades into granophyre.The granite contains 60% of orthoclase feldspar, 5-10% of

plagioclase, 20-25% of quartz with 4% of biotite, epidote, magnetite and fluorite. The low

initial Sr 87/ Sr 86 ratio indicate that the rocks have a relatively minor amount of older sialic

material . The Rb-Sr age of the granophyre is estimated to be 678 m.y (Nair and Vidyadharan,

1982). The Ezhimala Complex lies in close proximity to the Bavali lineament suggesting

reactivation along the lineament and intrusion of the body.

Kalpatta granite

The Kalpatta ((11 36'15";76 05'15") granite is an oval- shaped intrusive into the Wynad schist

and covers an area of 44 sq km (Rao and Varadan, 1967). The rock is grey coloured, medium-

grained, homogenous biotite granite and has sharp contact with the country rock. A feeble

foliation is imparted to the granite at places by biotite flakes. Xenoliths of amphibolite /

hornblende gneiss are visible near the periphery. Irregular veins of pegmatite / aplite traverse

the granite and also the enclaves. The K-Ar age of the biotite from the Kalpatta granite is dated

as 512 30 m.a (Nair et al, 1985) and 527 m.a (GSI). Presence of enclaves and absence of

significant replacement textures along with the geochemical characteristics assign a magmatic

parentage for the granite. The proximity of the pluton to the Bavali lineament probably suggests

intrusion along this fracture.

Three types of granites such as coarse grained biotite-granite, fine grained biotite granite, and

porphyritic granite are mapped on the basis of texture, colour and mode of occurrence. Coarse-

grained granite is a massive bluish grey rock with large xenoblasts of quartz and feldspars. The

accessories include biotite, zircon, apatite and sphene. Blastesis of feldspar and sphene are

common. Microcline, orthoclase, and plagioclase are seen as the major feldspar. Plagioclase

composition varies from albite to oligoclase. This rock is exposed in Trikkaippetta

(11035'04":76008"41":), Manikkunnu (11035"41":760 07'09"), Kuttamangalam

(11030'08":76007'11":) (Anilkumar et al, 1993).

Fine biotite-granite is a fine grained massive rock exposed around Muttilmala

(76006'38":11037'06"). It consists of orthoclase, quartz, microcline, biotite, sericite, zircon,

sphene, apatite and opaques. Myrmekitic quartz is recorded. Pophyritic granite consists of

myrmekitic quartz, microcline, sericite and biotite. Very coarse grained biotite with included

crystals of orthoclase, microcline and albite are common. Except for the texture, all the three

granites show similar characters. ( Anilkumar, et al 1993). Based on Rb-Sr dating , Kalpatta

granite is dated 765 Ma. (Odom 1982).

Chengannur granite

The Chengannur (9 18'45"; 76 31'00") granite in Pathanamthitta District is an oval shaped

body with the long axis trending in east-west direction covering an area of 15 sq.km in and

around Chengannur. The granite is intrusive into the charnockite gneisses. The body is

emplaced close to the Achankovil shear zone. K-Ar date of the hornblende indicates an age of

550 m.a (Soman et al, 1983). The Chengannur granite is inferred to be a post kinematic granite

of magmatic parentage.

Two types of granites are recorded. One is medium-grained pink granite and the other is

coarse-grained grey granite. The former consists of quartz, perthitic feldspar, plagioclase,

biotite, hornblende, apatite and zircon. The composition of plagioclase varies from albite to

oligoclase. Microcline perthite is also seen. The coarse grained grey granite consists of

perthite, plagioclase, hornblende, biotite, quartz with occasional occurrence of

hypersthene,apatite and zircon. Hornblende and biotite are less common by occurred minerals

than hypersthene. Relicts of hypersthene are also seen. This granite may be a product of

granitisation of charnockite. K2O content always exceeds that of Na2O . The high SiO2,high

alkali, high Fe/Mg ratio, high values of Gallium indicate that the granite belongs to alkali type.

It might have an origin from recycled and rehydrated continental crust. ( Nair and Anil

Kumar,1990).

Peralimala granite

The Peralimala (11°09'19":75°38'46") alkali granite is a linear intrusive body emplaced along

the axial trace of a mega fold in EW direction. Peralimala intrusive body occurs as a diatreme

of alkali composition with a maximum linear extension of 15 km and a width of 3 km. Based

on colour, texture, composition and mode of occurrence four types of granites are identified.

These are pink gneissic granite, porphyritic granite, grey granite and pink granite. Pink alkali

granite is a coarse-grained rock consisting of microcline, orthoclase, plagioclase, quartz,

hornblende, epidote, aegirine, sphene, calcite, perthite and apatite. Quartz is present in only

subordinate amounts. Feldspar content is very high. The preferred orientation of feldspar gives

a crude alignment. At Perumpunna, (75°44'00":11°55'28") pink gneissic granite shows

preferred orientation of biotite and pyroxene. The porphyritic granite occurs as a lensoidal

body containing quartz, feldspar, pyroxene and hornblende. Feldspar forms the phenocrysts in

a matrix of quartz-feldspar and mafics. Grey granite is a coarse- to medium- grained rock with

microcline, quartz, orthoclase, perthite, hornblende and zoisite. Light grey granite is a medium-

grained rock consisting of microcline, orthoclase, plagioclase (albite to oligoclase), epidote,

aegirine, hornblende and rutile. The major element chemistry of the granite do not show much

variation. The pink granite shows high content of potash. A negative correlation for K2O

content with respect to SiO2 is very pronounced for pink granite owing to its alkaline nature.

Barium and strontium show very high values for Peralimala granite. ( Anilkumar et al,1993).

Sholayur granite

The Sholayur (11 04'15";76 42'00") granite, is exposed around Kuttiyadikal Mala

(11001'52":76042'00") and Vachchapathi (11004'15":76044'00"). It is a homophanous medium-

grained, pink coloured granite, consisting of quartz, orthoclase, microcline, oligoclase, perthite,

aegirine augite, biotite, hornblende and sphene. In some places, calcite, apatite, sericite are also

observed. The schlierens mark the contact zone of the granites with the host rock. This granite

is emplaced within the Wynad supracrustals. SiO2 varies from 58.76 to 73%, Al2O3 14% to

17%, Na2O 1.8% to 2.4% and K2O 0.8 to 1.5%. The distribution of SiO2 is highly non-uniform

within the same type of granite. The pink granite is becoming alkali granite at places.(Anil

Kumar and Nair,1992).

Intermediate intrusives

The syenite body at Mannapra (10 30'00";76 32'00") is exposed as an elongated NW-SE

trending body covering an area of 8 sq km in Thrissur District. The syenite intrusive, makes

sharp contact with the charnockite near the charnockite-migmatite contact. The rock is medium

to coarse- grained at its peripheries and tends to be coarse-grained towards the centre.

Mineralogically, the rock is composed of alkali feldspar, orthopyroxene, clinopyroxene and

amphibole with minor amounts of plagioclase, biotite and opaques. A small syenite

(Angadimugar syenite) body is located in Kumbala village (12 35'15"; 76 07'00") and about

20 km east of Kumbla in Kasaragod District. The intrusive body has an elliptical outline and

covers an area of 5 sq km. The body is intrusive into the Khondalite Group and encloses

enclaves of amphibolite in the peripheral parts. The rock is medium to coarse grained, light

grey and massive.

Mesozoic intrusives

Basic intrusives

Basic intrusives in Kerala, mainly represented by dyke swarms in NNW-SSE to NW-SE trend,

cut across all the metamorphic rocks and the earlier structural trends. Their unmetamorphosed

nature and stratigraphic relation with the country rocks prompted their correlation to the

Deccan Trap volcanism.

The basic dykes have been emplaced into the migmatites and charnockite in NNW-SSE to NW-

SE and ENE-WSW directions along distensional and shear fractures respectively. Dolerite

dykes of Kerala are mostly quartz tholeiites rarely clinotholeiite. The basic dykes of

Pathanamthitta (9015'45":76045'30") are genetically unrelated types. These dykes have not

undergone any internal differentiation during intrusion.

The variation in the chemistry of individual dykes may be due to the cogenetic differential

sequence. Dolerite dykes intrude the country rocks at an angle greater than 800. The dolerite

dykes of Kuttuparamba (11049'30":75034'00") in Kannur District shows cross cutting

relationship with all the formations. The basic dykes of Vamanapuram (8043'00":76054'00")

are either gabbroic or doleritic intruding the gneissic rocks. These are trending NNE to SSW

and NNW to SSE directions and are unmetamorphosed. Mineralogically all these dykes show

more or less same composition except the meta-dolerites. Variation in the trace elements like

Ti, Zr can be attributed to the differential degree of partial melting of the mantle material. (Nair

and Gopala Rao, 1989).

The unmetamorphosed Idamalayar gabbroic dyke with a NNW-SSE trend is traced for over

80 km in the central part of Kerala. The rock is mesocratic, medium-grained, porphyritic and

is composed of plagioclase (andesine to labradorite), hornblende and opaques. The reported

age of 75 m.y for the Idamalayar dyke (Subramaniam, 1976) links it in time-relationship with

Deccan Trap volcanism.

The NNW-SSE trending leucogabbro dykes in central Kerala dated by whole rock K-Ar

method gave an age of 81 2 m.y and the NW-SE trending dolerite dyke 69 1 m.y. The

dolerite dykes are thought to have represented the feeder system for Deccan Trap volcanic

sequences (Radhakrishna et al, 1994).

Basic dykes of Pathanamthitta area yielded ages of 99 Ma to 117 Ma and there are dykes which

have yielded ages 104 + 5 Ma, 127 + Ma and 476 + Ma. These wide variations may be due to

a protracted history of emplacement and the effect of Eocambrian to palaeozoic tectonothermal

events affecting this region ( Sinha Roy and Ramakrishnan, 1983.)

In Thiruvananthapuram District, Anakudi and Nedumannur dolerite dykes are dated by K-Ar

method and the whole rock ages are 104 5 Ma and 127 2 Ma respectively (Sinha Roy and

Ramakrishnan,1983).

Tertiary Sedimentary rocks

Mio-Pliocene sedimentary rocks are fairly widespread in the southern coastal belt, their

remnants being noticeable in the central and northern coastal areas. These sedimentary rocks

consist of a series of variegated clay and sandstones with lenticular seams of lignite, known as

Warkalli Formation, underlain by more compact marly sands with shell fragments and thin

horizons of limestone (Quilon Formation).

The Tertiary sediments have a gentle dip towards west. The Warkalli Formation extends in a

narrow belt from Thiruvananthapuram (8 28'30": 76 57'20") to Kasaragod (12 30'00":

74 59'00") between coastal and midland regions with intervening promontories of the

crystalline rocks. The Quilon Formation is mainly seen at Paravur (08 48'00": 76 40'00")

Padappakkara (08 58'30": 76 38'00") and some other places around Kollam and Alappuzha

districts.

Quilon Formation

The Quilon Formation consisting of fossiliferous shell limestone alternating with thick beds of

sandy clays and calcareous clays have been reported from Padappakkara (type

locality),Nedumgolam, Edavai (8 45'20";76 42'00") and Varkala (8 44'00": 76 43'00") and

Cherthala (9 41'00":76 20'00") along the west coast of Kerala. The Quilon limestone contains

numerous fossils of foraminifera, corals, echinoids and molluscs. The Lower Miocene age for

lower stratigraphic horizons and the Upper Miocene age for the topmost beds of the Quilon

Formation indicate the lower and upper age limits of these marine sediments. The

predominance of black clays, sandstone, bluish grey brackish water shell limestone and nodular

limestone clearly indicate deposition in a lagoonal condition .

Warkalli Formation

The Warkalli Formation of Mio-Pliocene age extends all along the Kerala coast.The type

section of the Warkalli Formation described by King (1882) is from the sea cliff at Varkala.

The exposed section at Varkala cliff is 28-30 m thick consisting of unconsolidated sands of

variegated clays, white plastic clays, and carbonaceous sandy clays enclosing impersistent

seams and lenses of lignite. The carbonaceous clays and lignite are often impregnated with

nodules of marcasite.

Fairly thick beds of carbonaceous clays with lignite seams occur around Nadayara kayal,

Tamarakulam (9 08': 76 37'), Puliyur (9 18'00": 76 35'00"), Payangadi (12 00'20'':

75 15'40"), Nileswaram (12 15'00": 75 07'00"), Kanhangad (12 17'40': 75 05'00") and in the

cliff sections near Cheruvathur (12 13'00": 75 09'50").The most characteristic feature of the

Warkalli Formation is the impersistent nature of the constituent beds, suggestive of shallow

basin margin deposits.

Laterite

Kerala is the home of the laterite as it was first named by the Dutch traveller, Buchanan 1807.

Laterite is widespread in its distribution in the midland region of Malappuram, Kannur and

Kasaragod districts where it forms well-defined mesas. The Archaean crystalline rocks and the

Tertiary sedimentary rocks are extensively lateritised. The laterite has wide areal distribution

in the State and occurs at all levels upto 2000 m, height though mostly restricted to an altitude

of 50-150 m above MSL. in the coastal and midland region. A few bauxitic patches also occur

within the laterites. The thickness of laterite cappings varies from a few metres to 50 metre at

places. At Chovvara (8 21'30"; 77 01'30") in Thiruvananthapuram District and Chattannur

(8 50'30"; 76 46'30") and Kundara (8 57'00": 76 40'30") in Kollam District, a zone of about

2 m thick bauxite is recognised at the contact between the crystallines and the overlying

sedimentary rocks. The overlying sedimentary column is also blanketed by laterite of varying

thickness. The bauxite at the base of the sedimentaries indicates an earlier pre-Warkalli spell

of lateratisation. Further, the erosional features on the top part of the bauxite horizon

corroborates the antiquity of the earlier spell of lateritisation (Mallikarjuna and Kapali, 1980).

Generally, the laterite after the crystalline rocks is compact and the top crust moderately

indurated. The dark brown crust passes downward to pink and buff coloured soft laterite.

Quartz veins, joints and fractures can be traced from the top to the bottom of the laterite profile.

The laterite profile over pyroxene granulites, meta-ultramafites and gneisses are characterised

by relict foliation that conforms to those of the subjacent rocks which indicate the insitu nature

of the laterite. Porous and spongy texture is discernible in laterites, after meta-ultramafites.

Laterite after the Tertiary sedimentaries is well indurated at the top for about 2 to 5 m.

Downwards, the profile grades into soft laterite with remnants of gritstone and culminates into

a zone of variegated clay.

Quaternary sediments

Recent to sub-Recent sediments of coastal sands, sticky black clay with carbonized wood, silty

alluvium and lagoonal deposits are observed mostly in the low-lying areas from Kollam

(11 27'00": 75 40'30") to Ponnani and between Kannur (11 51'30":75 21'45") and

Nileswaram (12 15'30":75°08'16"). Alluvium is observed along the major river valleys. At

places, along coastal tracts, there are raised sandy beaches composed of fine grained reddish

-beach ridges alternate with marshy lagoonal clay in

the coastal area.

The sandy stretches are widest between Alappuzha (9 30': 76 20') and Kottayam (9 35':

76 31'), upto 25 km inland from the shoreline. The Quaternaries of the coastal plain have been

classified into (i) the Guruvayur Formation representing the earlier strandline deposits with an

elevation of 5-10 m; (ii)the Viyyam Formation of tidal plain deposits; (iii) Periyar Formation

being mainly of fluvial deposits and (iv) the Kadappuram Formation representing the beach

deposits (Krishnan Nair, 1989).

A pebble bed is traced in Valapattanam and Taliparamba river banks in Kannur district. It is

exposed south of Valapattanam (11

Morazha (11 58'30": 75 20'30") and Arathiparamba (12 06'00": 75

pebbles ranges in dimension from 4.5 cm x 3 cm to 7 cm x 3 cm with occasional cobbles of

size 13 cm x 12 cm. The base of the pebble bed is generally 20 to 40 m above MSL and at

places, the pebble bed directly rests over the basement rocks. The pebbles are mostly of quartz

and rarely of granite and pyroxene granulite. The distribution of the pebble bed along the major

river banks demonstrate it to be flood plain deposits, probably of early Quaternary period (Nair

et al, 1976). In Malappuram and Kozhikode districts, the pebble bed is traced in the riverine

terraces at Mavur (11 17'45":75 59'00" ), Cheruvannur (11 12'8": 75 49'35") and

Chellepparambu (11 14'30":75 59'00"). In Thiruvananthapuram District, the Quaternary

pebble bed occurs at an elevation of 45 to 50 m above MSL at Pothenkode (8 37'00":

76 48'56"), Idaikode (8 40'11":76 50'49"), Attingal (8 41'49": 76 48'56") and Andoorkonam

(8 36'00": 76 52'30").

Submerged upright tree trunks have been reported from a number of places in the coastal area

of Kottayam and Alappuzha districts, indicating neotectonic reactivation in the area. Carbon

dating of a sample from the submerged forest at Iravimangalam indicate an age of 7050 130

B.P (Pawar et al, 1983).

Structure

The structural grain of the southern Peninsula is controlled mainly by the NNW-SSE trending

near longitudinal Dharwarian trend which had folded all earlier structures. Since Kerala State

falls in the western limb of the mega-structure almost all the rock distribution is aligned in

NW-SE direction. However, detailed structural studies carried out in selected parts of the

Kerala (Nair and Nair, 2001) had shown that (a) the earliest folds (F1) which are represented

both on mesoscopic and megascopic scale are tight appressed folds of asymmetrical nature

which had given rise to axial plane foliations with characteristic platy mineral alignments (b)

the F2 folds on these foliations (post-folial) are open symmetrical and have developed mainly

on megascopic scale and control the disposition of the major lithologies. (c) Subsequent folds

(F3) which deform F1 and F2 axial plane traces are broad folds on mega-scale identified with

the longitudinal Dharwarian trends and (d) a broad swerve on these Dharwarian trends in ENE-

WSW is also decipherable (Fig.2).

Detailed analysis of the remote sensing data had revealed the presence of a number of

significant lineament patterns in WNW-ESE, NW-SE, NNW-SSE, NNE-SSW and ENE-WSW

directions (Nair, 1990). Mega and intermediate lineaments in WNW-ESE were originally

crustal fractures and shears which got sealed or obliterated by a number of igneous

emplacements of alkali granite, syenite, gabbro, anorthosite, granophyre etc. The

emplacements along the Bavali lineament and those along the Achenkovil lineament both of

which trending in this direction had given ages ranging from 500 678 Ma. Hence they are

iden tified to be the oldest lineament. The Bavali lineament forms the western termination of

the Moyar shear. The NW-SE trending lineaments constitute mega lineaments and coincide

with the basic dykes occurring throughout the length and breadth of the state. These dykes have

given ages ranging from 61 to 144 Ma. The NNW-SSE trending lineaments are generally

intermediate lineaments and are attributed to fractures, faults and major joint patterns in the

area. It is recognized that the NNW-SSE trending lineaments define a weak zone along which

the west coast evolved by faulting. The eastern limit of the Tertiary basin is found restricted

along this lineament direction. These lineaments occurring along the west coast are be active

as suggested by the progradation of the coast west of these lineaments (Nair, 1987). The

lineaments in NNE-SSW are prominent and are identified with major fractures and this together

with those in NNW-SSE are taken to constitute a conjugate system of faults in a N-S

compressive regime due to the collision of the Indian plate. The ENE-WSW trending

lineaments are intermediate lineaments and are well- developed in the northern parts of the

Kerala . Since these lineaments truncate other lineaments as evidenced especially in the coastal

stretches it is considered the youngest. Many a recent tremors reported are aligned in this

direction and hence considered neotectonically active.

Metamorphism

The Precambrian crystalline rocks of Kerala are chiefly metapelites, charnockites with

associated gneisses and granulites, schistose rocks with distinct metapelitic and metamafic /

ultramafic affinity and granitic derivatives which include the Peninsular gneisses and

migmatites. Except the Wynad schists and the Vengad group, the bulk of the crystalline rocks

show granulite to upper amphibolite facies of metamorphism. Wynad schist displays a prograde

amphibolite facies metamorphism and the retrogression of these rocks leads to lower

amphibolite facies metamorphism. The vast charnockite belt occurring on either side of the

Wynad schist belt, in north Kerala, shows petrographic evidences of prograde and retrograde

reactions (Nambiar, 1996). The rocks of the Vengad Group show greenschist to lower

amphibolite facies of prograde metamorphism. The older intrusive bodies show effects of

incipient metamorphism, marked by clouding of feldspar and bending of twin lamellae.

Recent investigations on the pressure temperature range for the formation of characteristic

mineral suits within the metamorphic rocks provide a fair idea on the poly-metamorphic history

of the rock suits. Rocks of the Khondalite belt of south Kerala indicate a temperature range of

650 to 850 C and pressures 5 to 6 kb (Srikantappa et al, 1985). In the Thiruvanathapuram area,

the temperature at the peak of metamorphism indicated by the mineral assemblages of the calc-

silicate rocks is about 830ºC at 5 K bar considering the vapour absent garnet forming equilibria

(Satish Kumar and Santosh, 1996). The scapolite equilibria indicates a peak metamorphic

temperature of above 800ºC. Stable isotopes in the marble bands suggest that there was no

pervasive infiltration of external fluids. Local infiltration of external carbonic fluid took place

during decomposition. Synthesis of such data from different lineament/shear bound segments

in Kerala indicate varying metamorphic conditions and uplift history. It is also summerised

that there is a progressive decline in the uplift of different segments from north to south

(Soman, 1997).

environmentclearance.nic.inenvironmentclearance.nic.in/writereaddata/Online/TOR/25_May_2018... · List of Figures Figure 1: Geology and mineral resources of Kannur. Figure 2: Geomorphology

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