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1

F:\DSR DANTEWADA FINAL.docx

Notice

“District Survey Report, Dantewada” has prepared as par the terms

and conditions of appendix-10 of Notification No. S.o. 141 (A) New Delhi

15 junuary 2016 of Ministry of Environment, Forest and Climate Change,

introduced through the Environment (Protection) Act. 1986.

The draft of District Survey Report, Dantewada is placed on the

website of the NIC, Dantewada as will notice board of DEAC, Dantewada

for inviting comments/suggestions from the general public, persons and

entities concerned. The last date for receipt of the comments/suggestions is

21 day from the publication of this Reprot i.e. 08th

Aug 2016.

The comments/suggestions may be sent by e-mail to the following

ID: [email protected]

It my kindly be ensured that the comments are sent on MS-Office

Word file.

Alterntively, comments/suggestions may also be sent by post to the

following address:

Member Secretary

District Environment Impact Assessment Authority

Mining Section, Office of the Collectorate Dantewada

Pin 494449

The envelop may kindly be super scribed on the top with: -

“comments/suggestions on the District Survey Report”.

2


MINERAL RESOURCE DEPARTMENT

DIRECTORATE OF GEOLOGY AND MINING

CHHATTISGARH

DISTRICT SURVEY REPORT

DANTEWADA

3


INTRODUCTION

Dantewada district is one of the Twenty Seven districts of Chhattisgarh State and

Dantewada town is the administrative headquarters of this district. The Dantewada

district occupies the southern part of Chhattisgarh state. Major part of the district

falls in the Survey of India Degree Sheet No.65 F and is bounded between latitudes

17˚48’32”:19˚24’33”N and longitudes 80˚14’46”:82˚15’35”E. The total area of the

district is approximately 3410.50 km2.

Dantewada is connected with Jagadalpur the nearest town, by National Highway

No.16. Dantewada is also connected by road with Hyderabad, the capital city of the

neighboring state Andhra Pradesh. Apart From Hyderabad Bus Connectivity is also

available from two more major cities of Andhra Pradesh Vijayawada & Vishaka

Pattanam.

South East Railway is running a regular train (Passenger) from Vishakha Pattanam

to Bailadila which passes through the beautiful Araku Vally, and stops a while at

Dantewada before reaching its destination Bailadila. The nearest Air terminal is

Raipur.

District survey report has been prepared as per the guidelines mentioned in

appendix-10 of the notification No. S.O. 141 (E) New Delhi, 15 January, 2016 of

Ministry of Environment, Forest and Climate Change. This report has prepared by

the Regional head, DGM Jagdalpur as per instructions issued by the Director,

Geology & Mining (C.G.), Raipur by its letter no.5103-05/ geology-1/f.no.11/2015-

16, dated 22/04/2016.

The report primarily is focused on the Geological Details i.e. minerals its

occurrence, deposit and mining. Along with the mineral data, geographical and

infrastructure information is also included.

District Environment Impact Assessment Authority and District Environment

Assessment Committee will utilize this report in favour of the environment

concerned activities and act accordingly.

Also this report will act as reference for the lease holders of minerals and those

willing to apply for lease.

4


5


OVERVIEV OF MINING ACTIVITY IN THE DISTRICT

Minerals of economic importance are found in Dantewada district mainly Iron ore

and Tin ore etc. Building materials like aggregate, sand, murrom, ordinary stone,

brick clay are also found in enough quantity.

Five mines of Iron ore has been allotted to National Mineral Development

Corporation Limited and eight mines of Tin ore has been allotted to Precious

Minerals and Smelting Limited.

Beside these 15 Stone quarries at Kirandul, Bade Bacheli, Dhurli, Gumda, Bade

Kameli and Kadampal area have been leases out.

10 sand quarries have been leased out on the bank of river Shankhani-Dhankhni at

different villages for sand mining.

Approximately 578.28 crore rupees royalty is earned from all minerals in the

district in 2015-16.

6


LIST OF MINING LEASES OF IRON ORE IN THE DISTRICT (as on 01.04.2016)

Ø lapkyudrkZ dk

uke o irk vof/k xzke rglhy daikVZesaV uacj

ouHkwfe

jdck

jktLo Hkwfe

jdck dqy jdck

1 2 3 4 5 6 6 7

1

es-,u-,e-Mh-lh-

fyfeVsM

cSYkkMhyk

12-09-1995 ls

31-03-2020rd

fdjUnqy fM0 14

,e,y

624, 626, 627, 628, 629, 637, 639

322-368 gs- 0 322-368 gs-

2

es-,u-,e-Mh-lh-

fyfeVsM

cSYkkMhyk

07-12-1995 ls

31-03-2020 rd

fdjUnqy fM0 14

,u,etsM,e,y

626, 627, 638, 639, 640

506-742 gs- 0 506-742 gs-

3 es-,u-,e-Mh-lh-

fyfeVsM cpsyh

13-09-1995 ls

31-03-2020 rd

cpsyh narsokM+k

fM0 05

: 1834,1880,1881,1883,1884,1885,1887,1888,1889,1890

540-050 gs- 0 540-050 gs-

4 es-,u-,e-Mh-lh-

fyfeVsM cpsyh

12-09-1995 ls

31-03-2020 rd

cpsyh narsokM+k

fM0 10

: 1839,1840,1841,1842,1843,1844

309-34 gs- 0 309-34 gs-

5

es-,u-,e-Mh-lh-

fyfeVsM

fdjanqy

13-09-1997 ls

12-09-2017 rd

fdjanqy narsokM+k

fM0 11 ,e,y

638, 640, 641, 642, 643, 645, 654, 655, 656, 657, 658, 659

874-924 gs- 0 874-924 gs-

7


LIST OF MINING LEASES OF TIN ORE IN THE DISTRICT

Ø0 [kfuiV~Vk/kkjh dk

uke

[kfut

dk uke

xzke dk

uke

[kljk uacj jdck

gsDVs;j

esa

Lohdr̀ vkns'k dzekad fu"iknu

fnukad

Lohdr̀

vof/k

fjekdZ

1 2 3 4 5 6 7 8 9 10

1 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

cMs

cpsyh

70]71]74 7-739

gs0

,Q&3@52@99@12@I 11@7@2000

10/11/2000 20 o"kZ dk;Z'khy

2 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

cMs

cpsyh

25d]1046 ls 1061 ls

1062]1067]1068

17-087

gs0

,Q&3@53@99@12@

1-04-2003

30/9/2003 20 o"kZ dk;Z'khy

3 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

cMs

cpsyh

979 ls 984 5-314

gs0

,Q&3@53@99@12@

1-04-2003

30/9/2003 20 o"kZ dk;Z'khy

4 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

cMs

cpsyh

20 d 60 ls 66

69]75]76]126]118]39@21

40 ls 142 144 ls 150

36-067

gs0

,Q&3@53@99@12@

01-04-2003

30/9/2003 20 o"kZ dk;Z'khy

5 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

y[kkjkl 115@1 d 21-084

gs0

,Q&3&118@99@12@2

27-7-2005

1/20/2006 20 o"kZ f'kfFky

6 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

usjyh 179]182]189 4-97 gs0 ,Q&3&89@12@2003

10-01-2005

7/7/2005 30 o"kZ dk;Z'khy

7 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

ijpsyh 872 7-55 gs0 ,Q&3&8@06@12

08-05-2007

9/11/2007 30 o"kZ f'kfFky

8 es0 izsf'k;l

feujYl ,.M

LesfYVax fyfeVsM

txnyiqj

fVu

v;Ld

usjyh 164]167]168]170]172 ls

177

16-40

gs0

,Q&3&30@2005@12

01-02-2007

6/30/2008 30 o"kZ f'kfFky

8


LIST OF QUARRY LEASES IN THE DISTRICT

l-dz- iV~Vk/kkjh dk uke o

irk

[kfut

ftlds

fy, iV~Vk

fn;k x;k

gS

Lohdf̀r vkns'k dz0

,oa fnukad

fu"iknu fnukad dkykof/k xzke

iapk;r ,oa

rglhy

[kljk

Øekad

{ks=Qy ¼gs-

esa½

varj.k fd;k x;k

1 2 3 4 5 6 7 8 9 10

1 Jh vCnqy oghn

fl|hdh fdjanqy

iRFkj dz'kj

LFkkfir

90@[kfut@m0i0

01@2006 fn0

28@04@2006

6/22/2006 19@10@2006 ls

18@10@2016 rd

10 o"kZ

fdjUnwy 46 3-38 gs0 dk;Z'khy

2 Jh vCnqy oghn

fl|hdh fdjanqy

iRFkj dz'kj

LFkkfir

128@[kfut@m0i0

03@06 fnukad

08@05@2006

6/22/2006 03@04@2007 ls

02@04@2017 rd

10 o"kZ

fdjUnwy 61 1-47 gs0 dk;Z'khy

3 Jh vCnqy oghn

fl|hdh fdjanqy

iRFkj dz'kj

LFkkfir

130@[kfut@

m0i0 02@06 fn0

08@05@2006

22/06/2006 05@04@2007 ls

04@04@2017 rd

10 o"kZ

fdjUnwy 46 2-024 gs0

5-00 ,dM+

dk;Z'khy

4 Jh vCnqy oghn

fl|hdh fdjanqy

iRFkj dz'kj

LFkkfir

146@[kfut@

m0i0 01@2006

fn0 11@05@2006

23-06-2009 01@04@2007 ls

31@03@2017 rd

10 o"kZ

fdjUnwy 46 1-821 gs0

4-50 ,dM+

dk;Z'khy

5 ;wfud feujYl

nUrsokM+k izkijkbZVj

vk'kh"k ekyoh; esu

jksM+ narsokM+k

iRFkj dz'kj

LFkkfir

835@[kfut@

m0i0 19@07 fn0

07@01@2009

23-05-2009 23@05@2009 ls

22@05@2019 rd

10 o"kZ

cMs desyh 571 1-53 gs- dk;Z'khy

6 ;wfud feujYl

nUrsokM+k izkijkbZVj

vk'kh"k ekyoh; esu

jksM+ narsokM+k

iRFkj dz'kj

LFkkfir

836@[kfut@

m0i0 18@07 fn0

07@01@2009

23-05-2009 23@05@2009 ls

22@05@2019 rd

10 o"kZ

cMs desyh 796 4-000 gs- dk;Z'khy

7 es-;wfud feujYl

narsokM+k izkijkbZVj

vk'kh"k ekyoh; esu

jksM+ narsokM+k

iRFkj dz'kj

LFkkfir

553@[kfut@ m0

i0 03@2011 fn0

05@08@2011

26-07-2012 26@07@2012 ls

25@07@2022 rd

/kqjyh 988@2 1-417 gs0 dk;Z'khy

8 es-;wfud feujYl

narsokM+k izkijkbZVj

vk'kh"k ekyoh; esu

jksM+ narsokM+k

iRFkj dz'kj

LFkkfir

377@[kfut@ m0

i0 05@ 2009 fn0

08@08@2011

26-07-2012 26@07@2012 ls

25@07@2022 rd

/kqjyh 988@2 1-821 gs0 dk;Z'khy

9 Jh dey lksekuh

txnyiqj

iRFkj dz'kj

LFkkfir

44@[kfut@m0 i0

07@10 fn0

12@04@2010

10-08-2010 10@08@2010 ls

09@08@2020

xqeMk 240@1 4-000 gs- dk;Z'khy

10 Jh dey lksekuh

txnyiqj

iRFkj dz'kj

LFkkfir

267@,@[kfut@

m0 i0 07@10 fn0

07@07@2010

10-08-2010 10@08@2010 ls

09@08@2020

xqeMk 257 1-42 gs0 dk;Z'khy

11 Jh veu vxzoky

fuoklh fdjUnqy rg-

dqvkdks.Mk ftyk

nf{k.k cLrj narsokM+k

iRFkj

¼;kaf=d

fdz;k }kjk½

379@[kfut@

m0i0 10@2010

fn0 17@08@2010

14-07-2010 14@07@2010 ls

13@07@2020 rd

dMeiky 816 1-35 gs- dk;Z'khy

12 Jh nsosUnz flag

dq'kokgk 'kkafr uxj

u;k cl LVS.M ds

ikl txnyiqj

ftyk cLrj

iRFkj

¼;kaf=d

fdz;k }kjk½

383@,@ [kfut@

m0 i0 05@2009

fn0 18@08@2010

30-10-2010 30@10@2010 ls

29@10@2020 rd

10 o"kZ

cMs cpsyh 272 2-55 gs- Lohdr̀ {ks= dk rglhy

dk;kZy; ls lhekadu

izfrosnu vizkIr ,oa dz'kj

IykaV LFkkfir u fd;s tkus

ds dkj.k dk;Z vuqefr ugha

iznku dh x;h gSA vr%

f'kfFkyA

13 Jh ds lh 'kekZ

narsokM+k

iRFkj dz'kj

LFkkfir

128@[kfut@m0i0

02@05 fn0

08@05@2006

23-06-2006 23@06@2006 ls

22@06@2016 rd

cM+s desyh

narsokM+k

168@1 1-80 gs- f'kfFky

14 Jh ds lh 'kekZ

narsokM+k

iRFkj dz'kj

LFkkfir

6855@[kfut@

m0i0 10@03 fn0

19@11@2008

17-02-2009 17@02@2009 ls

16@02@2019 rd

10 o"kZ

cMs+ desyh 796 3-33 gs- f'kfFky

15 Jh eukst nklkuh

nqxZ

iRFkj 120@[kfut@

m0i0 22@2008

fn0 01@05@2008

02-09-2008 02@09@2008 ls

01@09@2018 rd

dMeiky 799@2 2-69 ,dM+ dk;Z'khy

9


LIST OF SAND MINES IN THE DISTRICT

dz0 vkosnd xzke

iapk;r vkosfnr {ks=

i;kZoj.k

foHkkx

izi=

1&4

mR[kuu

Iyku rS;kj

dh fLFkfr

i;kZoj.k Lohd`fr dh

fLFkfr i;kZoj.k foHkkx esa yafcr

1 2 3 5 6 7 8

1 ckywn ckywn v [k0dz0 31 jdck 8-

000 gs0 iw.kZ iw.kZ

Ik;kZoj.k Lohd`fr izkIr

fnukad 27-11-2015 80]000 ?ku ehVj izfro"kZ vkxkeh 02 o"kZ gsrq

2 ckywn ckywn c [k0dz0 31 o 1310

jdck 5-000 gs0 iw.kZ iw.kZ Ik;kZoj.k Lohd`fr izkIr 50]000 ?ku ehVj izfro"kZ vkxkeh 02 o"kZ gsrq

3 uxj iapk;r

narsokM+k

[kljk dz0 385 jdck 5-000

gs0 {ks= iw.kZ iw.kZ Ik;kZoj.k Lohd`fr izkIr 50]000 ?ku ehVj izfro"kZ vkxkeh 02 o"kZ gsrq

4 xqeM+k [kljk 1224 jdck 5-000 gs0 iw.kZ iw.kZ Ik;kZoj.k Lohd`fr izkIr


5 fcatke [kljk 818 jdck 14-700 gs0 iw.kZ iw.kZ Ik;kZoj.k Lohd`fr izkIr


6 ckyisV [kljk dz0 599 jdck 35-91 esa

ls 10-000 gs0 iw.kZ iw.kZ

Ik;kZoj.k Lohd`fr izkIr


7 elsukj

jktLo Hkwfe [kljk dz0 1395]

86] 1243] 1169 ,oa 1077 esa

ls jdck dze’k% 5-600 gs0] 6-

970 gs0] 6-080 gs0] 4-430 gs0

,oa 15-660 gs0

iw.kZ iw.kZ & i;kZoj.k Lohdf̀r yafcrA

8 cM+s rqeukj [kljk 751 jdck 5-000

gsDVs;j iw.kZ iw.kZ & i;kZoj.k Lohdf̀r yafcrA

9 cM+s dkjyh [kljk 1058 jdck 5-000


10 NksVs dkjyh [kljk 1599 jdck 5-000


10


MINERAL BASED INDUSTRIES IN DANTEWADA DISTRICT

S.

NO

NAME OF UNIT & ADD. REGISTRATION

NO/ DATE

INVESTMENT

(IN LAC)

PRODUCT PRODUCTION

DATE

EMPLOYEE

1 M/S Arti Cement Blocks

Nirmad Pro. Harish Kumar

Sharma, New market Bacheli

22/16/00198

29.11.2001 0.65 Cement Block 10.11.2001 03

2 M/S k. Papachand Stone

crusher

Pro. K.A. Papachand, Kirandul

22/16/00243

31.01.2004 35.80

Stone

Chipstone

Dust

17.04.2003 25

3 M/S Arihant Minerals, Gumda,

Geedam, Pro. Shri Jain 22/16/00249

13.05.2004 8.34

Stone

Chipstone

Dust

24.05.2003 22

4 M/S KCM Industries,

Dantewada Pro. Chabindra

Karma, Katiyaras Dantewada

22/16/11/00018

28.02.2008 7.00 Cement Bricks 15.02.2007 20

5 M/S Pawan Bricks Industries,

Bacheli, Pro. Smt. Jhilkibai

22/16/11/00041

05.07.2011 1.00 Cement Bricks 10.04.2011 07

6 M/S Maa Bhitla Industries,

Harampara, Geedam, Pro.

Jaiprakash Chauhan

22/16/11/00053

16.11.2011 21.00 Flyesh Bricks 11.11.2011 14

7 M/S Kaveri Cement Bricks

Product, Pataras, Pro. Sanjay

Kumar Vishvakarma

22/16/11/00056

21.12.2011 3.50

Cement Bricks

Polls 10.01.2010 04

8 M/S Harsh Cement Bricks,

Balud Dantewada, Pro. Smt.

Balmati Tati

22/16/11/00058

25.02.2012 3.00 Cement Bricks 01.10.2011 09

9 M/S Umesh Bricks, Ghotpal

Geedam, Pro. Umesh Kumar

Sethiya

22/16/11/00062

23.03.2012 2.20 Clay Bricks 18.04.2011 19

10 M/S Parihar Industries, Hitawar

Nakulnar, Pro. Vipin Singh

Parihar

22/16/11/00063

23.03.2012 0.75 Clay Bricks 15.10.2011 13

11 M/S Danteshwari Enterprises,

Barsoor, Pro. Sambhunath

Singh

22/16/11/00065

26.04.2012 7.00 Cement Bricks 06.03.2012 04

12 M/S Somya Cement Bricks,

Haram Geedam, Pro. Smt.

Padma Gupta

22/16/11/00067

21.06.2012 20.00 Flyesh Bricks 20.04.2012 10

13 M/S Danteshwari Cement

Bricks, Kuankonda Dantewada,

Pro. Smt. Prema Devi

22/016/11/00092

10.07.2014 3.50 Cement Bricks 20.04.2014 10

14 M/S Thakur Cement Bricks,

avrabhat, Dantewada, Pro. Smt.

Devshri Thakur

22/016/11/00095

28.02.2015 3.00 Cement Bricks 10.04.2014 11

15 M/S Kiran Cement Bricks, Pro.

Smt Daimati Thakur, Chitapur

Balud

22/016/11/00096

24.03.2015 1.50 Cement Bricks 10.02.2015 07

16 M/S Yadav Cement Bricks

Industries, Pro. Jaldhar, Chote

Tumnar Geedam

22/016/11/00105

31.07.2015 1.50 Cement Bricks 24.04.2015 11

11


DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEAR

MAJOR MINERALS

S. NO. MINERAL ROYALTY OR REVENUE RECEIVED

2013-14 2014-15 2015-16

1 Iron Ore 6761162745.00 9537448671.00 5772118730.00

2 Tin Ore 2094402.00 1830083.00 398178.00

Total 6763257147.00 9539278754.00 5772516908.00

DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEAR

MINOR MINERALS

S. NO. MINERAL ROYALTY OR REVENUE RECEIVED

2013-14 2014-15 2015-16

1 Ordinary Stone 3316189.00 9713175.00 8459634.00

2 Clay for making Bricks 79353.00 126885.00 125242.00

3 Sand 283855.00 1547809.00 154710.00

4 Murum 329292.00 1396410.00 153697.00

Total 4008689.00 12784279.00 8893283.00

DETAILS OF PRODUCTION & ROYALTY OF SAND IN LAST THREE YEAR

ORDANARY SAND

Sand is mined from the bank of Balud during last two years. 06 more sand mines i.e.

Balud-B, Gumda, Dantewada, Balpet and Binjam are senctioned and got

environment clearance.

S. NO. FINANCIAL YEAR PRODUCTION OF SAND

(in m3)

ROYALTY RECEIVED

(in Rs)

1 2013-14 Nil Nil

2 2014-15 31330.00 626600.00

3 2015-16 38135.00 762700.00

Total 69465.00 1389300.00

12


PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS

Rivers have a lot of energy and because they have energy, they do stuff. The

obvious things rivers do with their energy is flow but, besides this, they also transport

load, erode load and erode the channel through which they flow. Erosion is the

breaking down of material by an agent. In the case of a river, the agent is water. The

water can erode the river’s channel and the river’s load.

A river’s load is bits of eroded material, generally rocks, which the river

transports until it deposits its load. A river’s channel is eroded laterally and vertically

making the channel wider and deeper. The intensity of lateral and vertical erosion is

dictated by the stage in the river’s course, discussed in more detail here but

essentially, in the upper stage of the river’s course (close to the source of the river)

there is little horizontal erosion and lots of vertical erosion. In the middle and lower

stages vertical erosion is reduced and more horizontal erosion takes place. There are

several different ways that a river erodes its bed and banks. The first is hydraulic

action, where the force of the water removes rock particles from the bed and banks.

This type of erosion is strongest at rapids and waterfalls where the water has a high

velocity. The next type of erosion is corrasion. This is where the river’s load acts

almost like sandpaper, removing pieces of rock as the load rubs against the bed &

banks. This sort of erosion is strongest when the river is transporting large chunks of

rock or after heavy rainfall when the river’s flow is turbulent.

Corrosion is a special type of erosion that only affects certain types of rocks.

Water, being ever so slightly acidic, will react with certain rocks and dissolve them.

Corrosion is highly effective if the rock type of the channel is chalk or limestone

(anything containing calcium carbonate) otherwise, it doesn’t have much of an effect.

Cavitation is an interesting method of erosion. Air bubbles trapped in the water get

compressed into small spaces like cracks in the river’s banks. These bubbles

eventually implode creating a small shockwave that weakens the rocks. The

shockwaves are very weak but over time the rock will be weakened to the point at

which it falls apart. The final type of erosion is attrition. Attrition is a way of eroding

the river’s load, not the bed and banks. Attrition is where pieces of rock in the river’s

load knock together, breaking chunks of rock off of one another and gradually

rounding and shrinking the load.

Transportation, when a river erodes the eroded material becomes the river’s

load and the river will then transport this load through its course until it deposits the

load. There are a few different ways that a river will transport load depending on how

much energy the river has and how big the load is. The largest of particles such as

boulders are transported by traction. These particles are rolled along the bed of the

river, eroding the bed and the particles in the process, because the river doesn’t have

enough energy to move these large particles in any other way. Slightly smaller

particles, such as pebbles and gravel, are transported by saltation.

13


This is where the load bounces along the bed of the river because the river has

enough energy to lift the particles off the bed but the particles are too heavy to travel

by suspension. Fine particles like clay and silt are transported in suspension; they are

suspended in the water. Most of a river’s load is transported by suspension.

Solution is a special method of transportation. This is where particles are

dissolved into the water so only rocks that are soluble, such as limestone or chalk,

can be transported in solution. Capacity & Competence Rivers can only carry so

much load depending on their energy. The maximum volume of load that a river can

carry at a specific point in its course is called the river’s capacity. The biggest sized

particle that a river could carry at a specific point is called the river’s competence.

Deposition to transport load a river needs to have energy so when a river loses

energy it is forced to deposit its load. There are several reasons why a river could lose

energy. If the river’s discharge is reduced then the river will lose energy because it

isn’t flowing as quickly anymore. This could happen because of a lack of

precipitation or an increase in evaporation. Increased human use (abstraction) of a

river could also reduce its discharge forcing it deposit its load. If the gradient of the

river’s course flattens out, the river will deposit its load because it will be travelling a

lot slower. When a river meets the sea a river will deposit its load because the

gradient is generally reduced at sea level and the sea will absorb a lot of energy. As

rivers get nearer to their mouths they flow in increasingly wide, gentle sided valleys.

The channel increases in size to hold the extra water which the river has to receive

from its tributaries. As the river gets bigger it can carry larger amounts of material.

This material will be small in size, as larger rocks will have broken up on their way

from the mountains. Much of the material will be carried in suspension and will

erode the river banks by abrasion. When rivers flow over flatter land, they develop

large bends called meanders. As a river goes around a bend most of the water is

pushed towards the outside causing increased erosion. The river is now eroding

sideways into its banks rather than downwards into its bed, a process called lateral

erosion. On the inside of the bend, in contrast, there is much less water. The river will

therefore be shallow and slow-flowing. It cannot carry as much material and so sand

and shingle will be deposited. This is called a point bar or slip off slope. Due to

erosion on the outside of a bend and deposition on the inside, the shape of a meander

will change over a period of time. Notice how erosion narrows the neck of the land

within the meander. In time, and usually during a flood, the river will cut right

through the neck. The river will then take the new, shorter route. The fastest current,

called the thalweg, will now tend to be in the centre of the river, and so deposition is

likely to occur in gentler water next to the banks.

Eventually deposition will block off the old meander to leave an oxbow lake.

The oxbow lake will slowly dry up, only refilling after heavy rain or during a

flood. Streams lose velocity and make deposits when their gradient decreases,

14


when the volume of water decreases, when there is an increase in cross section,

when they encounter obstructions, or when they enter still water. They deposit

alluvial fans, alluvial cones, piedmont alluvial plains, channel fill, bars, flood

plains and deltas.

15


GENERAL PROFILE OF THE DISTRICT

S. NO. PARTICULARS STATISTICS

1 GENERAL INFORMATION

Geographical Area 3410.50 km2

Geographical Position latitudes 17˚48’32”:19˚24’33”N

longitudes 80˚14’46”:82˚15’35”E

Administration Division/ No. of Tehsil 5

No. of Panchayat/ Villages 124/239

Population (as per Census 2011) 283479

Population Density (as per Census 2011) 83

2 GEOGRAPHOLOGY

Major Strategraphic/ Rock Granite, BHQ, BHJ, Quartzite etc.

Major Drainage Shankhani, Dankini and Haram

River

Temperature (in 0C Minimum 10

Maximum 45

3 LAND USE (km2)

Forest area 1710.685

4 Major Soil Type

5 No. of GROUND WATER MONITORING STATION OF CGWB (10.05.2016)

No. of Dugwells -

Water level Enslosed

No. of major bridges 8

6 HYDROGEOLOGY

Major water bearing formation Granite

Pre-Monsoon depth of water level Enclosed

Post-Monsoon depth of water level Enclosed

7 MINING SCENARIO

Total No. of Mining Leases (Major Minerals) 13

Total area of Mining Leases (Major Minerals) 2669.635 Hact.

Total Royalty or Revenue Received from Major Minerals

in 2015-16

5772516908.00

Total No. of Quarry Leases (Minor Minerals) 15

Total area of Quarry Leases (Minor Minerals) 33.001 Hact.

Total Royalty or Revenue Received from Minor Minerals

in 2015-16

8893283.00

Total No. of Notified Sand Leases 10

Total area of Sand Leases 56.00 Hact.

Total production of Sand in 2015-16 38135 m3

No. of Quarry Lease to be extended as per Amended

CGMMR 2015

12

16


LAD USE PATTERN IN THE DISTRICT

FOREST LAND

S.

NO.

NAME OF FOREST

RANGE

PROTECTED

FOREST

(Hact.)

RESERVE

FOREST

(Hact.)

UNDEMARCATED

FOREST

(Hact.)

TOTAL

(Hact.)

1 Dantewada 11263.769 9816.538 2352.108 23432.415

2 Geedam 17902.527 3757.748 3615.695 25275.970

3 Nelasnar 24839.088 23661.181 1769.724 50269.993

4 Basoor 1358.893 13261.699 1238.645 15859.237

5 Bacheli 26630.893 19399.542 10200.450 56230.885

Total 81995.170 69896.708 19176.622 171068.500

AGRICULTURE AND IRRIGATION LAND

1 Total Agriculture land 102472 Hact.

2 Name of the crops mostly cultivated Paddy

3 Source of Irrigation Canal, Tank, Tube well,

Dugout well and other

4 Method of Irrigation Flood Irrigation method

5 Total Irrigation Land (in percent) 3860 Hact. (2.34%)

17


PHYSIOGRAPHY OF THE DISTRICT

The Dantewada district occupies the southern part of Chhattisgarh state. Major part

of the district falls in the Survey of India Degree Sheet No.65 F and is bounded

between latitudes 17˚48’32”:19˚24’33”N and longitudes 80˚14’46”:82˚15’35”E.

The total area of the district is approximately 3410.50 km2. It is surrounded by

Bastar district in the north and north east, Bijapur district in the west, Sukma district

in the south and south-east.

Physiographically, major part of the district exhibits pediment/pediplain landforms.

Other landforms seen in the district are structural plateau of upper and lower level in

the western part, structural plain in the south eastern part, structural hills and valleys

in the northen and eastern part, denudational plateau in the eastern part and

denudational hills and vallys in the centeral and western part. Most of the district

area falls in Indravati, Shankhni and Dankini catchment. Indravati, Shankhni,

Dankini rivers and their tributaries constitute the surface drainage network of the

district. The general gradient is towards south, southeast and southwest. The

maximum elevation in the area is -----1265 m above mean sea level as recorded in

the Bailadila ranges in the northern part while the minimum elevation of ---99 m.

above mean sea level is noted in the south western part of the district.

18


RAINFALL OF DISTRICT DANTEWADA

(MONTH WISE)

YEAR 2013-14 (mm)

MONTH DANTEWADA GEEDAM KUANKONDA KATEKLYAN

April-2013 24.00 23.00 23.00 20

May-2013 0.00 0.00 0.00 0.00

June-2013 299.90 355.70 399.80 465.30

July-2013 411.20 609.90 625.60 655.40

August-2013 267.60 314.90 361.00 452.20

September-2013 61.70 84.80 174.10 118.00

October-2013 151.10 212.00 141.70 238.60

November-2013 0.00 0.00 0.00 0.00

December-2013 0.00 0.00 0.00 0.00

January-2014 0.00 0.00 0.00 0.00

February-2014 0.00 0.00 0.00 0.00

March-2014 0.00 0.00 0.00 0.00

YEAR 2014-15 (mm)


April-2014 0.00 0.00 0.00 0.00

May-2014 0.00 0.00 0.00 0.00

June-2014 120.60 52.20 134.20 155.70

July-2014 204.00 368.60 343.60 326.30

August-2014 241.60 394.80 200.90 295.40

September-2014 190.80 251.00 59.90 93.00

October-2014 30.60 112.00 52.90 32.00

November-2014 0.00 0.00 0.00 0.00

December-2014 0.00 0.00 0.00 0.00

January-2015 0.00 0.00 0.00 0.00

February-2015 0.00 0.00 0.00 0.00

March-2015 0.00 0.00 0.00 0.00

YEAR 2015-16 (mm)


April-2015 0.00 0.00 0.00 0.00

May-2015 0.00 0.00 0.00 0.00

June-2015 421.40 563.20 223.30 242.40

July-2015 77.10 94.70 146.00 180.70

August-2015 337.20 388.80 225.50 434.90

September-2015 180.40 180.60 106.20 124.10

October-2015 13.00 0.00 0.00 2.00

November-2015 0.00 0.00 0.00 0.00

December-2015 0.00 0.00 0.00 0.00

January-2016 0.00 0.00 0.00 0.00

February-2016 0.00 0.00 0.00 0.00

March-2016 13.00 18.40 .00 0.00

19


WATER LEVEL OF PRE MONSSON & POST MONSOON

DISTRICT DANTEWADA

S. NO. NAME OF

BLOCK

NAME OF

TEHSIL

WATER LEVEL

POST MONSOON

AUGUST-2015

(m)

WATER LEVEL

PRE MONSOON

APRIL-2016

(m)

1 Dantewada Dantewada 8.75 10.90

2 Dantewada Bade Bacheli 8.50 11.00

3 Geedam Geedam 9.15 12.00

4 Kuankonda Kuankonda 8.00 10.90

5 Kateklyan Kateklyan 8.00 10.90

20


GEOLOGY

Physiographically, major part of the district exhibits pediment/pediplain landforms. Other

landforms seen in the district are structural plateau of upper and lower level in the western part,

structural plain in the south eastern part, structural hills and valleys in the northen and eastern part,

denudational plateau in the eastern part and denudational hills and vallys in the centeral and

western part. Most of the district area falls in Godavari, Indravati and Sabari catchment. Indravati,

Godavari, Sabari rivers and their tributaries constitute the surface drainage network of the district.

The general gradient is towards south, southeast and southwest. The maximum elevation in the

area is -----1265 m above mean sea level as recorded in the Bailadila ranges in the northern part

while the minimum elevation of ---99 m. above mean sea level is noted in the south western part

of the district.

Rock formations belonging to Archaean to Neo Proterozoic, Cainozoic and Quaternary are

exposed in the district. The olderst rocks in the area are represented by Eastern Ghat Supergroup

and Bengpal group of Archaean age. Estern Ghat Supergroup is exposed from Mattimark,

,arwada to Pamed in the western part of district and comprises leptynite (garnetiferous granite

gneiss), Charnockite, pyroxene granulite, khondalite and ulramafic granulite. Rock belonging to

Bengapal group are exposed in the major part of the district and comprises various types of

gneisses and schists, amphibolites, meta-basics, meta-ultramafics, migmatites and different

varieties of quartzites e.g. pyroxene quartzite, cherty quartzite, ferruginous quartzite, sericitic

quartzite,banded magnetite and grunerite-magnetite-quartzite.

Bailadila Group of Archaean to palaeo Proterozoic age are exposed from south of Kunjangwara

to Kidindul in the north eastern part of the district and comprises hornblende schist, meta-basic,

meta ultrabasic, talc- tremolite schist, banded magnetite quartzite, quartzite, meta-conglomerate,

quartz-sericite schist, ferruginous shale, phyllite and meta-tuff. This group owes its importance

due to the associated iron ore deposits which are being mined since long.

Dongarghar Granite of palaeo Proterozoic age is exposed in Madepur,Bairamghar, south of

Kunjangwara and east of gangalur areas in the northern part of the district and include a variety of

granite i.e. biotite granite, hornblende-biotite granite, amphibole granite, leucogranite etc.

Abujmar Group of rock of Palaeo to Meso proterozoic age are exposed from Thukanar,

Murumwara to kunjangwara, Gawad in the northern part of the district. It is further divided into

Gundal and maspur formations. Maspur Formation is a meta-volcanic sequence where as Gundal

Formation is a sedimentaey sequence comprising conglomerate, sandstone and shale. Tulsi

Dongar Group considered as equivalent to the Abujmar Group is exposed to the north east and

south east of Chidpal in the eastern extent of the district. It is a volcanosedimentary sequence and

comprises meta-basalt/gabbro, sandstone and quartzite.

The Bengpal and Abujmar group of rocks and Dongarghar Granite are profusely intruded by basic

dykes/sills and quartz/pegmatite/aplite reefs/veins.

The Albaka formation, which is directly classified under Pakhal supergroup and the

Lakhanavaram formation and Pattipalli formation of Mulug Group of Pakhal Supergroup of Meso

21


Proterozoic age are exposed from Timed to west of Lankapalli and Utlapalli to Kottapalle in the

south western part of district. The Albaka formation is mainly composed of sandstone whereas

Mulug formation is mainly a shale unit with minor quartzite. Pattipalle formation is mainly a

quartzite unit.

Sabari Group of rocks of Meso Proterozoic age are exposed around Rokel, Talner, Sukma,

Guttaguda and bot side of Sabri/Kolab River in the south eastern part of the district and comprises

sub-arkose, orthoquartzite, siltstone, conglomerate, limestone and shale.

Doli and Usar formation of Sullavai Group of Neo Proterozoic age exposed from Lankapalli to

Nambi in the south western part of the district. Doli formation comprises intraformational

breccias, conglomerate, pebbly sandstone and sandstone. Usar formation is mainly a sandstone.

Laterite of Caonozoic age occurs mainly on Bailadila ranges as a fairly thick blanket. Alluvium of

Quaternary age occur fro Kodta to Kukanar in the mid-eastern part of the district.

The district is richly endowed with mineral wealth. The major economic mineral

deposits/occurrences reported in the district include gold,coper,iron ore,tin (cassiterite),

radioactive mineral, chromite, asbestos, bauxite, clay, corundum, garnet, graphite, kyanite,

magnesite, mica, sillimanite, and limestone. Primary gold mineralization has been reported from

Puspal. Copper is reported from Modernar. Large deposits of haematitic iron ore occur associated

with Bailadila Group and are reported from 3.5 km south east of Kondapal, southwest of

bailaidila, 2.5 km west of Bacheli, --- 1265m, 4 km north east of Purngel and 4 km south west of

kidindul. Cassiterite, the ore of tin occurs in pegmatite and also as colluvial deposit and is reported

from Churwada, Govindpal, Mundval, Pushpal and Bodavada. Radioactive minerals are reported

from Yenchawasa, Raiguda and Pushpal. Chromite in talc-tremolite schist is reported from

Kondasanvali. Pockets and lenses of tremolite asbestos are reported from Kondasanvali and

Gollapalli. Bauxite occurs associated with laterite and is reported from Taralimeta. Fairly large

deposits of while/buff/variegated clay suitable for low grade pottery occur at Rokel and Sindigar.

Corundum occurrence is reported from Bhopalpatnam and Kuchnoor. Granet crystals varying in

size from 1 to 10 cm are reported from 12 km westnorth west of Konta. Specks of flaky graphite

are reported from Borakonda-Sanuali, 3 km south west of Kamaram, Palachelam and Bate Tongu.

Kyanite occurs in schists and gneisses of Bengpal Group and is repoeted from Mura-Ka-Gutta and

Nilamraia-Gutta thin veinlets of magnesite associated with talc-tremolite schist and tremolite

schist are reported from nedra. Minor occurrences of lepidolite (mica) are reported from

Mundaval and Kawargaon. Massive sillimanite is reported from Samsatta. Deposits of limestone

associated with shale formation of Sabri Group are reported from Gudra, Ikmeras, Pujariras and

Rokel.

22


GEOLOGICAL AND MINERAL MAP OF DANTEWADA DISTRICT

23


24


DRAINAGE SYSTEM WITH DESCRIPTION OF MAIN RIVER

S.NO. NAME OF

RIVER / NALA

TOTAL DISTANCE

IN DISTRICT

(km)

PLACE OF SOURCE HIGHT IN SOURCE

(Height above MSL)

(m)

1 Dantewada River 17 Dantewada

(Sankni-Dankani

Junction)

400

2 Sabguda River 26 - -

3 Dankani River 20 Dongrari Dongar -

4 Sankni River 25 Nandiraj Bailadila -

5 Temrujodi Nala 18 Bailadila 538

6 Bhogam Nala 17 Kanwalnar 440

7 Kerawpur Nala 15 - -

8 Pharaspal Nala 17 Bailadila 712

9 Goujodi Nala 16 - -

10 Kori River 28 - -

11 Mundipara Nala 19 - -

12 Gamawada River 16 Hill of Bailadila 750

13 Renganar Nala 15 Gadmiri Nikat 690

14 Kumharas Nala 17 Chandenar 650

15 Dugeli Nala 14 Hill of Bailadila 700

16 Maniya Nala 15 - -

17 Gudra River 20 Narayanpur -

18 Mandar River 30 Koder rain forest 720

19 Indravati River 80 Kalahandi -

20 Duman River 15 Dotra Dongri 760

21 Maach Nala 18 - -

22 Bengalur Madhya

Gandi Nala

16 Maggupara

Bengalur

640

23 Alibahar Nala 13 Barsur 457

24 Lanka Bahar Nala 14 Bhalu Dongri 553

25 Ganesh Nala 30 Bhalu Dongri 560

26 Chimal Nala 12 - -

27 Gumalnar Nala 19 Gumalnar 412

28 Mafalnar Nala 15 Karli forest 611

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