6 O 6 BATTLE MOUNTAIN CANADA LTD. REPORT ON DIAMOND DRILLING PLACER OPTION (QUED) PROPERTY N.T.S. 42C13 EASTERN CANADA Project No 443 Battle Mountain Gold July 27, 1997 Manitowadge Exploration Office Jim Edwards Exploration Geologist Battle Mountain Canada Ltd. Eastern Canada 42C13SW0177 2.17606 WABIKOBA LAKE 010
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6 O 6
BATTLE MOUNTAIN CANADA LTD.
REPORT ON DIAMOND DRILLING
PLACER OPTION (QUED) PROPERTY
N.T.S. 42C13
EASTERN CANADA
Project No 443Battle Mountain GoldJuly 27, 1997Manitowadge Exploration Office
Jim Edwards Exploration Geologist Battle Mountain Canada Ltd. Eastern Canada
42C13SW0177 2.17606 WABIKOBA LAKE 010
Table of Contents
Page
LO SUMMARY AND INTRODUCTION l2.0 LOCATION AND ACCESS l3.0 PROPERTY DESCRIPTION 24.0 PREVIOUS WORK 25.0 REGIONAL GEOLOGY 56.0 DIAMOND DRILLING RESULTS 67.0 DISCUSSION OF DRILL RESULTS 68.0 CONCLUSIONS AND RECOMMENDATIONS 89.0 REFERENCES 9
Appendices
Appendix I DDH Logs and Assay Results Appendix II Battle Mountain Regional Legend
List of Figures and Maps
Scale
Figure l Location Map 1:1584,000Figure 2 Claim Map 1:15,000Figure 3 Regional Geology 1:50,000Figure 4 Surface Plan Map of DDH Locations l :5,000Figure 4a Surface Plan Map of DDH Locations l: 15000Figure 5 Geology of the North Limb Region l :50000
Map l Section Line 115+00 E of Q97-1 1:1,000Map 2 Section Line 105+00 E of Q97-2 1:1,000Map 3 Section Line 97+02 E of Q97-3 l: l ,000Map 4 Section Line 90+50 E of Q97-4 1:1,000Map 5 Section Line 93+50 E of Q97-5 1:1,000
42C13SW0177 2 17606 WABIKOBA LAKE 010C
1.0 SUMMARY AND INTRODUCTION
The Placer Option (Qued) is a property which is owned by Placer Dome Canada and was
optioned to Hemlo Gold Mines Inc.in 1996. Hemlo Gold Mines Inc merged on July 19,1996 with
Battle Mountain Gold. As a result of the merger Battle Mountain Canada Ltd worked the Placer
Option. During the months of May, June and July, 1997 a hole diamond drill program was
conducted on the Placer Option (Qued) claim group. Five diamond drill holes totaling 1604 metres
were completed July 6, 1997. The expenditures associated with this program were sufficient to
meet the requirements of the agreement. Battle Mountain Canada Ltd. is now 60y0 vested in the
property.
The purpose of this 1997 diamond drill program was to test the alteration and potential
mineralization associated with the strike extent of the Armand Lake Porphyry along its northern
contact and the Qued Porphyry. The other criteria used in defining drill targets along the northern
contact of the Armand Lake Porphyry included geophysical IP anomalies and soil geochemistry
anomalies that are situated near the contacts of both the Armand Lake and Qued Porphyry
contacts.
Holes Q97-1 and Q97-4 are stratigraphic fences to test the lateral strike length of both the
Armand Lake and Qued Porphyry to determine if they have a similar alteration characteristics as
seen along the contact of the Lunny Lake Porphyry on the Fowler Option where drilling in 1995
intersected two horizons of anomalous gold mineralization. Although these horizons are spatially
associated with the Armand Lake and Lunny Lake Porphyries no significant alteration or gold
mineralization was intersected along the contacts of the Armand Lake Porphyry or the Qued
Porphyry. Numerous quartz phyric and quartz sericitic porphyritic sills which intruded mafic
flows between these two porphyries were encountered in all holes. Generally the alteration and its
intensity increased along the western section of the property.
The best gold assay values from this program were encounted in hole Q97-5. The interval
from 208.5 to 212.5 returned an average gold value of 0.429 g/ton over a four metre interval,
including a one metre sample of 0.625 g/ton Au, located along the southern contact of the Qued
Porphyry. Another anomalous gold value was encountered in hole Q97-2 where a one meter
sample grades 0.643 g/ton Au from 132-133 metres. This sample was hosted in a mafic volcanic
with minor interflow sediments that are magnetic. These mafics occur along the footwall contact of
the Armand Lake Porphyry.
The best sericitic alteration and gold values were from holes Q97-3 where gold values
range from 11 ppb (.0011 g/ton Au) to 81 ppb (.0081 g/ton Au). The average grade over a 5 metre
interval is 0.03 g/ton Au. These gold values are hosted in a sericitized quartz feldspar porphyry.
These values are directly north of significant intersections of 3.34gA: over 3 metres to the south
hosted in the Lunny Lake Porphyry.
2.0 LOCATION AND ACCESS (Figure 1)
The Placer Option (Qued) property is located approximately 5 km east of Highway 614
down the Dead Otter Lake/ Twist timber road. The Dead Otter Lake timber road is situated 14 km
north of Highway 17. Access can by gained to the property by either two of four wheel drive
vehicles.
MANITOUWADGE
Property•^ MARATHON\
PUKASKWA NATIONAL
i PARK
/WAWA
SUPERIOR
SAULT STE -MARIE
Scale 1:1,584,000 or l"-25miles
Figure 1. Location Map
3.0 PROPERTY DESCRIPTION (Figure 2)
The property consists of 24 single unit unpatented mining claims listed below. The listed
claims are optioned to Battle Mountain Canada Ltd. by Placer Dome Canada Ltd. This exploration
program was conducted on the following claims 1164418, 1164419, 1164422, 1164423, 1164425,
property. The hole consists mostly of mafic volcanics with small altered porphyritic sills of quartz
feldspar porphyry up to 5 metres in width. The best alteration with in the hole comes from a 4.4
metre wide intensely silicified and moderately sericitized QFP located between 265.59 - 269.00
metres. The IP target was explained by a iron formation which occurs from 129 - 155 metres.
The most significant mineralization occurs with in the iron formation from 131-134 metres where
Py and Po form stringers of up 2 - 4 cm long and ^ mm wide. Pyrite is disseminated though out
the unit. Anomalous gold values of 183 ppb, 230 ppb and 127 ppb are from the interval between
349.95-353.92 metres. They are hosted in a weakly sericitized quartz feldspar porphyry from
344.40-356.81.
Q97-2:
Hole Q97-2 was collared in the Armand Lake Porphyry. The purpose of this hole was test
the sericitic alteration associated with the northern contact of the Armand Lake and Qued
Porphyries. The upper portion of hole (5 - 128.38 m's) consists of variable phases of fine to
medium grained feldspar porphyry. A narrow 2 metre wide quartz sericite schist l alteration zone
is present at the contact of the Armand Lake Porphyry and a magnetic iron formation which hosted
a sample of 0.643 g/ton Au over a l metre interval and is flanked by two l metre samples of 0.145
g/ton Au and 0.108 g/ton Au. This iron formation also explains the IP anomaly. The lower
portion of the hole is comprised of mafic volcanics with intercalated chemical and clastic
metasediments.
There is a series of weak to moderately altered porphyritic sills that exist between the
northern contact of the Armand Lake Porphyry to the south and the Qued Porphyry at (174 -
222.20 m) to the north. The lower section of the Qued Porphyry is a quartz sericite schist with thin
2 -3 cm wide feldspathic bands locally with weakly anomalous gold values. This unit returned an
average grade of .085 g/ton over a 5 metre interval from 207.54 to 213.54 metres
Q97-3:
Hole Q97-3 was collared in the northern contact of the Armand Lake Porphyry. It is along
strike of Q97-2 and is stratigraghically similar in the lithological units encounted along strike. The
hole intersected a series of medium to fine grained porphyritic sills that are unaltered to weakly
sericitized. The sericitized sills were also quartz phyric and occur at 139.44 - 142.76 m. The
Qued Porphyry occurs between 344 - 377.46 metres. The mafic volcanics are pillowed with flow
top breccia units that are mineralized with up to 207o pyrite.
The most significant alteration was at 190.5 - 198.5 metres where the presence of minor
feldspathic bands < l cm wide occur in sediments.
The IP anomaly in this hole can be explained by clastic and chemical metasediments from 171.95
- 200.20 metres. Locally within the iron formations are semi massive stringers of pyrite < .50 cm
wide and disseminated pyrrhotite mineralization.
The only significant gold values in this section were returned from a 5 metre interval
grading 0.03 g/ton, hosted in a quartz phyric porphyry from between 364 and 369 metres.
Q97-4
The purpose of hole Q97-4 was to test the lateral extent of the Qued Porphyry and test alteration
mapped on surface at depth. The hole was collared into a small granodiorite/ diorite felsic
intrusion, which was unexpected since there is no magnetic low associated with this area of the
property. The IP anomaly can be associated with a narrow iron formation 4 metres wide. Again the
section consists of pillowed and massive mafic volcanics that have been intruded with various
phases of feldspar and quartz feldspar porphyritic sills which have been moderately to strongly
sericitized. These units occur at 22.59 - 38.32 metres. The best sericitic alteration occurs at 87.5 -
101.70 metres. This unit is a quartz sericite schist with fine feldspathic laminations between 93.66
- 101.70.metres. There were no significant gold values associated with is alteration but a small
fleck of Mo, Pyrite 207o and tourmaline were present with in fine feldspathic laminations. The
highest assay value returned from this hole was 0.039 g/ton from this hole is from l metre interval
of brecciated pillowed mafic volcanics at 199 metres.
Q97-5:
This hole was designed to determine the strike extend of the Qued Porphyry to the west.
The Hole was collared in mafic volcanics and there is a series of feldspar and quartz porphyries
sills within the hole. The sills observed in this hole have the best alteration seen on the stratigraphic
horizons tested by this 1997 diamond drill program. The lower section of this hole intersected the
Qued Porphyry which where strong sericite alteration was observed. Assay results from this unit
returned gold vales of up to 0.625 g/ton over l metre and 0.429 g/ton over a four metre interval.
8.0 CONCLUSION AND RECOMMENDATIONS
Due to the limited alteration halo and lack of significant gold values along the contacts of The
Qued and Armond Lake Porphyry have a limited alteration halo and lack of significant gold values.
There is however a north south spatial relationship associated with anomalous gold in the Lunny
Lake Porophyry to the south and the Qued Porphyry to the north.
Future exploration efforts should concentrate on: Following the strike and depth extent of the
anomalous horizon located within the Armand Lake Porphyry to the East where significant gold
assays values and molybdenite mineralization have been encountered
Respectfully submitted,
Battle Mountain Canada Ltd.
Jim Edwards
Exploration Geologist
Eastern Canada
Battle Mountain Canada Ltd. July 27, 1997
9.0 REFERENCES
Muir, T.L.,1982a. Geology of the Heron Bay Area, District of Thunder Bay. Ontario Geological Survey, Geological Report 217, 65 p. Accompanied by Map 2439, scale l inch to 1A mile.
Muir, T.L.,1982b. Geology of the Heron Bay Area, District of Thunder Bay. Ontario Geological Survey, Geological Report 217, 65 p. Accompanied by Map 2452, scale l inch to [A mile.
Muir, T.L.,1983. Geology of the Heron Bay Area. P.230-239, in The Geology of Gold in Ontario, edited by A. C. Colvine, Ontario Geological Survey, Miscellaneous Paper 110. P 230-239
Muir, T.L., 1988 Hemlo tectono-stratigraphic study; in Summary of Field Work and Other Activities 1988, Ontario Geological Survey, Miscellaneous Paper 141, p. 226-229.
Muir, T.L.,Schnieders, B.R. and Smyk, M.C., (Compilers and Editors), 1995, Geology and Gold Deposits of the Hemlo Area; Geological Association of Canada - Toronto'91, Hemlo Field Trip Guidebook, 120p.
Williams, H.R, Heather, K.B., Muir, T.L., Sage, R.P. and Stott, G.S. 1991. Wawa Subprovince; in The geology of Ontario, Ontario Geological Survey, Special Volume 4, Part l, p.485-539.
APPENDIX I
Drill Logs and Assays, Results
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
Property: Placer
Option
Project No: 443
Hole No: Q97-1
Length: 386 m
Overburden: 4
Core Size: NQ
Drilling Bradley
Company: Brothers
Date Hole
Started: 05/21/97
Date
Completed: 05/27/97
Logged By: Jim
Edwards
Date Logged: 05/29/97
Core Storage: Hemlo
Casing In Hole
(in
hole/pulled)
Grid Ref. Surveys ACID
east
north
UTM E
UTM N
azim.
incli.
elev.
grid az.
claim no.
115+00
94+50
591043.15
5409032.2
20
-45
5325
000
1164438
depth
75
150225
300
350
386
azim. inclin.
-44
-43
-43
-43
-43
-42
Signature:
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
FROM TO LITHOLOGICAL DESCRIPTION
Carbonate and calcite veining increase down section and the unit is weakly to moderately magnetic. Locally spotty rounded calcite infilled amygdules Between 24.3 - 24.5 there is intense area of calcite veining and carbonate bands
33.50 40.54 (6G,Bi,[PY]) [Gabbro]Mafic Intrusive: the unit is medium green in colour and coarse grained to crystalline. No Alteration and l - 2^/0 pyrite which is disseminated and clustered.
40.54 74.90 (2U, fol, Sil, Bi, Ep, Chl, Py)[Moderately Foliated Mafic Volcanic] Mafic Volcanic: The unit is medium grey to green in colour and fine to medium grained. The unit is foliated 62 - 66 degrees to the core axis. Locally there is moderate silicification. There is < 2*Xo quartz carbonate veins that have < Wo pyrite associated with them. One quartz vein 2 cm wide has tabular tourmaline. The Biotite bands are locally intense and are up to 3 cm wide and are parallel to the foliation. Where biotite bands are present the unit around these bands takes on a greenish hue due to epidote. The pyrite has a cubic habit and ^"/o of the units volume.60.58 - 61.18 small dyke of [9FP] weakly foliated 63 degrees to the core axis. It has It is moderately silicified and with trace pyrite. The lower contract of this unit with a Mafic Intrusive dyke is 57 degrees.
74.90 91.18 (6U, m, Chl,)[Mafic Intrusive]The unit is coarse grained with a mottled greyish colour. The unit is quartz carbonate veined and weakly magnetic.A small sub unit at 84.97 - 85.63 of weakly altered fine grained, buff coloured, silicified biotic mafics with a foliation of 63 degrees to the C. A. Pyrite strings are present along millimeter wispy quartz carbonate veins. The amount of Biotite in the 6U increases down section and is medium to coarse grained No significant alteration is present.
91.18 101.90 (2U, fol, Sil, Bi, Ep, Chl, Py) [Foliated Mafic Volcanic]The unit is fine to medium grained and light grey in colour with a mottled appearance in some areas Biotite is weak, and is elongated along the foliation
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
FROM TO LITHOLOGICAL DESCRIPTION
67 degrees to the core axis. Calcite veining is also present. The lower contact of this unit is 72 degrees to the C. A.
101.90 111.42 (9FP, qe, fol, SIL, Ser, Bi, Py, Po) [Feldspar Porphyry!The unit is medium grey to dark grey, It is medium grained and porphyritic and becomes finer grained as sericite alteration increases. It has a well developed foliation which is 63 degrees to the C.A. The feldspar pheno's go from being rounded to elongated along the foliation to being smeared along and washed out in area of weak sericite alteration laminations and patches. Pyrite occurs as stringers and forms clusters parallel to the foliation. Biotite is weak and oriented along the foliation. Fracturing in the unit is weak possibly stockwork.
111.42 130.70 (2U, fol, BI, Py, Gt, Cv) [Mafic Volcanic]The upper 3 meters of the unit is moderately magnetic and non magnetic down section. The unit is medium green in colour and fine to medium grained. It is cut by calcite bands. Biotite is weak and elongated along the foliation which is 65 degrees to the C.A. Epidote is weak and gives the unit a greenish hue. There is a very subtle contact between this Mafic unit and the sediments below marked by an increase in silicification Small inter-flow sediments is present at 128 -130.19 the sub unit is moderately magnetic .
130.70 155.12 (4IF/5ST, Bi, GT, Sil, Ser, Po, PY, ) [Iron Formation l Siltstone]The upper 2 m of the section is fine to medium grained with a purplish sheen. The unit has alteration laminations of weak sericite, locally sericite is moderate and is parallel to the foliation 65 degrees to the C.A. The alteration fizzles out at 134 m. The sediments are weakly magnetic and are garnet bearing. There is calcite bands and veins though out the unit Biotite gives the unit a mottled look in some areas while in some areas garnets are concentrated in 3 -5 cm bands. The unit is area is thinly laminated with silty interbeds.
155.12 160.5 (2U,BiI,Ep, Py,) [Mafic Volcanic ]
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
FROM TO LITHOLOGICAL DESCRIPTION
The contacts are very subtle and this unit is fine grained and weakly magnetic. It is the void of any garnets and has a weak foliation 63 degrees to the C. A. Calcite veins are present and carbonate is a weak part of the groundmass.
160.5 162.51 (9FP, fol, Bi, Cv,)[Feldspar Porphyry]The unit is light to medium grey in colour and ismedium grained. The unit is unaltered yet has ahazy overcast to it due to carbonate. The feldsparpheno's are rounded and easy recognized. The unitis foliated 62 degrees to the C. A. with minor calciteveins.
162.51 165.02 (2U, Bi, Ep, Py )[Foliated Mafic Volcanic] The unit is a massive looking volcanic. It is fine grained and greyish to medium green in colour. The unit is weakly magnetic and Biotite and Epidote gives the unit a greenish hue. Pyrite is parallel to the foliation and occurs as stringers
165.02 167.85 (9FP,qe, Bi, Py)[Feldspar Porphyry]The unit is similar to other small porphyry sills. It is medium grained and light to medium grey in colour. It is weakly foliated 63 degrees to the core axis. Locally there are well developed quartz eyes and minor carbonate veining. There are a few flecks of pyrite.
167.85 171.96 (2U, Bi, Ep.Py)[Foliated Mafic Volcanic] The unit is fine grained and dark grey in colour. There is a weak foliation 63 degrees to the C.A. The unit is not magnetic and has minor calcite veins.
171.96 173.0 (9FP,qe, Bi, Py)[Feldspar Porphyry]The unit is similar to other small porphyry sills. It is medium grained and light to medium grey in colour. It is weakly foliated 63 degrees to the core axis. Locally there are well developed quartz eyes
and minor carbonate veining. No pyrite Mineralization present
The unit has a mottled appearance and is light grey to medium green in colour. The calcite veining and bands are moderate. The unit is well foliated 62 degrees to the C. A. The groundmass has a moderate amount of carbonate present 5 07o per/volume. There is a small 9FP dyke between 183.72 and 183.72
183.72 189.97 (2U, fol, Bi, Chl ,Cv)[Foliated Mafic Volcanic]Fine to medium grained dark grey to black unit. It is well foliated at 66 degrees to the core axis and weakly magnetic. Fractures are very chlorite. Calcite veining is on a micro - scale while carbonate is apart of the groundmass
189.97 193.04 (9FP, Ser, Hem, Bi, Py) [Feldspar Porphyry]The unit is weakly altered with pervasive sericite and patchy hematization. Which gives the unit a greyish to reddish granitic appearance. It is foliated at 67 degrees to the C. A. and the lower contact is at 74 degrees to the C.A.
193.04 225.40 (2U, fol, Ep, Carb ,Bi ,Gt, CV, Py) [Carbonatized Mafic Volcanic] Fine to medium grained, locally a mottled appearance. It is grey to medium grained and well foliated at 70 degrees to the C.A. The unit is weakly to moderately magnetic. Again carbonate is apart of the matrix and calcite veining is orientated along the foliation. Epidote is patchy. Locally there is trace pyrite Sometimes there is intense biotite bands that parallel the foliation and there is garnets near the lower contact.
225.40 237.00 (2U/4DF, Bi, Gt, Qcv, Sil, Py, Po)[Mafic Volcanic l Inter-flow Sediments]The unit is mostly non magnetic yet there are areas of strongly magnetic inter-flow sediments. The mafic section of the unit are medium grained and green to dark grey in colour. The 4IF is more silicified and thinly laminated with Pyrite stringers parallel to the foliation and minor Po. These section are strongly magnetic and garnet bearing.
237.00 250.35 (2U, fol, Carb, Ep, Bi, Py)
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
FROM TO LITHOLOGICAL DESCRIPTION
[Mafic Volcanic]The unit is non magnetic. Fine to medium grained and grey to medium green in colour. The unit is foliated 71 degrees to the C. A. Calcite veins and biotite are associated with each other.
250.35 252.75 (9FP, Ser, Qcv, Bi, Py) [Feldspar Porphyry]Light to medium grey and weakly sericitized locally. The unit is massive and The feldspar pheno's are angular. There is some quartz carbonate veins on a micro scale.
252.75 265.60 (2U, Ep, Cv,)[Mafic Volcanic]The unit is massive and there is trace pyrite thought out the unit. The unit has calcite veins with no preferred orientation. It has a mottled appearance and medium green in colour. There are a few small 9FP dykes that intrude the unit. At 257.8 - 257.46 and at 252.26 - 252.58 they are weakly sericitized.
265.61 269.52 (9QFP, qe, Ser, Sil, Bl, Bi, PY, Kfd, Hem) [Altered Quartz Feldspar Porphyry]The unit is mostly a buff cream colour. Yet there is locally area where the unit is dark grey near the upper contact and in the middle of the unit is bleached and white looking in appearance. The lower section of the unit is more brown to khaki looking. The unit has well developed quartz eyes and is feldspar phyric . Locally the unit is blitzed and is dominantly sericite. There are small area that appear to be weakly feldspathic. The unit is intensely silicified almost marble looking. Py ^"/o.
269.52 271.76 (4IF, lam, Bi, Sil, Gt, Py)[Magnetic inter-flow Sediments]The unit is laminated and fine to medium grainedand dark grey to black in colour. There are somemafic units that are medium green in colour and nonmagnetic.
271.76 274.26 (2U, fol, Ep, Sil, Cv) [Mafic Volcanic]The unit is similar to the above mafic units. It is fine to medium grained and medium green in colour
274.26 281.93 (8U, Py, Sil)
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
FROM TO LITHOLOGICAL DESCRIPTION
[Diabase]Diabase: grey to medium grey in colour, medium grained and moderately magnetic. The unit has the typical diabase texture. The lower chill margin is silicified.
281.93 292.20 (2U/5SI)[Mafic With Inter-flow Sediments] The unit consists of mafic volcanic that have inter-flow sediments with are moderately silicified and weakly altered. The unit is massive and thinly laminated. Locally the unit is magnetic.
292.20 329.31 (2U, fol, Bi, Py, Cv)[Carbonitized Mafic Volcanic]The unit is dark grey to medium green incolour and biotite is developed along the foliation .biotite increase in swirling contorted calcite veins. The lower section is more laminated small altered section of mafic volcanic between 309.59 - 309.20 m. A bullish quartz vein at 320.6 320.7 m The unit has narrow mafic dykes which are coarse grained and less than 20 cm wide. Note the increase in biotite between 321 - 322.67 This sub unit is light brown in colour there is intense quartz carbonate veining.
329.31 332.34 (2U/4IF Gt, Bi, SIL, Qcv, PY, PO) [Mafic l Iron Formation] The unit is well laminated and Sulphide mineralization occurs as stringers with in finer grained laminations and quartz carbonate veins. It consists of 2^0 Py and 3 07oPY. The unit is dark grey to black in colour and is moderately silicified The unit is fine grained with mostly mafic minerals.
332.34 344.63 (2U, fol, Bi, Py, Cv)[Carbonitized Mafic Volcanic] Again this unit is similar to the above mafics. It is medium green in colour and fine to medium grained. There is a weak foliation 68 degrees to the C.A. A small bleached zone occurs between 336.07 - 336.90 with increased quartz carbonate veining.
344.40 356.81 (9QFP, qe, Ser, Hem, Ep, Py)[Weakly Sericitized Quartz Feldspar Porphyry]The unit is grey pinkish brown in colour. The unit is
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-1
FROM TO LITHOLOGICAL DESCRIPTION
feldspar phyric and locally serialized with well developed quartz - eyes and weak hematization. The unit takes on a greenish hue down section due to epidote alteration. Pyrite ^"/o.
356.81 386.00 (2U, Sil, Carb, Cv, Qcv, Ep, Po) [Carbonitized Mafic Volcanics] Mafic Volcanic: Dark green fine to medium grained. The unit is massive and at 381.5 - 381.9 a small zone of hyloclastite. In some of the quartz carbonate veins trace to ^"/o Po.
5.00 7.75 (9FP, qe, BI, Hemv, Epv)[Biotitic Fine Grained Armand Lake Porphyry]
Fine grained, dark grey FP, The unit is porphyriticand feldspar pheno's are sub rounded to rounded < 3 mm in diameter. Minor hematite veining and the odd quartz eye is present.
7.75 16.87 (9QFP, fol, por.Bi, Ep, Py)[Coarse Grained Quartz Feldspar Porphyry]The unit is coarse grained and light to medium grey in colour. Locally Epidote veining is present. The unit is feldspar and Quartz phyric. Quartz eyes are rounded while Feldspar pheno's are lath shaped to sub rounded. The unit has a Biotitic matrix There is a .5 metre weakly serialized zone at 14.01 -14.51 with trace pyrite. This alteration band is parallel to a weak foliation of 66 degrees to the C.A.
16.87 29.00 (9FP, fol, qe, [Bi], Epv, Hemv, PY)[Biotitic Fine Grained Armond Lake Porphyry]The unit is dark grey in colour and fine grained. The unit is feldspar phyric and these pheno's are sub rounded. Down section there is an increase in Epidote and hematite veining. Spotty areas of the unit take on a greenish or reddish hue. These vein sets are parallel to the foliation. There is small injections of coarse grained pink 9QFP. Pyrite occurs along stringers which are parallel to a weak foliation 65 degrees to the core axis.
29.00 35.3 (9QFP, qe, Bi,Qv,Pk, Py, Po.)[Coarse Grained Quartz Feldspar Porphyry]A Small injection of pinkish coarse grained porphyry with more angular quartz eyes and feldspars. Along Quartz veins, Pyrite and Pyrrhotite present up to 2"7o locally.34.5 - 35.3 Weakly altered .75 metre sub-unit at the contact between the above and a 9FP. The unit is intensely silicified and weakly sericited with intense Hematite and Epidote veining. The unit has a diffuse reddish halo due to hematite and possibly potassium feldspathization. Pyrite is finely disseminated and up to 3% locally along minor stockwork ? fractures.
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-2
FROM TO LITHOLOGICAL DESCRIPTION
35.3 41.6 (9FP,BI,Epv)[Feldspar Porphyry]The unit is a medium grained feldspar porphyry thatis dark grey in colour with a biotitic matrix. The unitis very pristine in appearance with no alteration.The unit has feldspar that are sub roundedThe unit is crystalline and dead looking.
41.6 45.92 (9FP, fol, fx, qe, Ser, Epv, Hemv, PY)[Biotitic Fine Grained Armond Lake Porphyry]The unit is a greyish green with a purplish sheen to it. Hematization is weak and occurs along fractures which are filled with quartz carbonate.
45.92 53.45 (9QFP, fx, qe, Bi, Pk, Sil, Qv, PY) [Quartz Feldspar Porphyry] QFP feldspar and quartz phyric. Feldspars are sub rounded and qe's arelarge l - .5 centimeters in diameter with a biotitic matrix. The unit is a transition phase to a fine grained Feldspar Porphyry. With a small mafic dyke.At 53.09 - 53.44. A small altered zone of sericite
alteration with pyrite stringers. The stringers and Weak gm is parallel to sub parallel to the foliation At 57.67 - 58.48 the sericite is moderate and silicification is intense and pervasive. The alteration fades in and out along the unit and consists of weak to moderate sericite.
59.66 115.8 (9FP, fx, BI.Epv, Qv.Sil, Py 20Xo) [Armand Lake Porphyry] The unit has variable phases of coarse to fine grained 9FP. The coarse grained phase of the Armand Lake porphyry is feldspar phyric and light grey to medium grey in colour. The finer grained equivalent of the above is more biotitic and silicified This unit has a purplish sheen to it and medium grey in colour. The feldspars are faint. There is a weak foliation of 64 degrees to the core axis. Down section the unit becomes moderately to strongly silicified and more pyrtic. The pyrite py (1- 3 07o) is finely disseminated and forms stringers parallel to sub - parallel to the foliation.
The upper contact of the unit is moderately serialized and silicified The unit is fine grained and
light grey to pale green in colour. Quartz eyes are well developed and feldspar pheno's stretched with fuzzy rims. The alteration becomes weak around 117.5.
119.5 128.38 (9FP, fx, qe, Bi, Sil, Py)[Armond Lake Porphyry]The unit is dark grey to black and medium grained . It is feldspar phyric. Feldspar pheno's are well developed and there are a few quartz eyes present. The unit is silicified and there is trace pyrite along along micro quartz fractures.
128.38 132.29 (4IF, Ep, Chl Gt, Py.Po, Cp.Qvc,) [Iron Formation]The unit is fine grained and dark grey to medium green in colour. The unit is well laminated and there is minor hematization. The Py and Po are associated with quartz carbonate and from small stringers. The unit is very magnetic. There is evidence of soft sediment deformation with slumping along thin laminations and contorted quartz carbonate veins
132.29 135.7 (2U, Ep.Bi, Py,)[Mafic Volcanic minor interflow Sediments] The unit is weakly magnetic. It looks like a mafic intrusion The unit is medium grained and medium green in colour with a mottled appearance
135.7 139.5 (4IF, Bi ,Py ,Po, Qcv, Hem) [Interflow Sediments]Small interflow sediment with weak sericite and garnet bands. The unit is dark grey to black in colour with contorted quartz carbonate veins and stringers of Py and Po. The unit is magnetic. Areas of weak sericite also have hematite associated with them.
139.5 174.0 (2U, M, Bi.Cv, Chl, Py)[Massive Mafic Volcanics] The unit is medium grained. The unit is dark grey to medium green. In localized area the unit looks recrystallized with a mottled texture. The unit is weakly magnetic and there is minor interflow sediments less than .5 metres wide. They are dark grey
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-2
FROM TO LITHOLOGICAL DESCRIPTION
and usually have garnets and increased Po associated with it. The is also small injections of 9QFP(169.9 -170.73) The unit's lower contact angle is at 64
degrees to the core axis
174.0 191.9 (9QFP, qe.fx.SER, Ep, Py ) [Qued Porphyry]The unit is dark grey and down section becomes more greyish brown in colour. Local areas where the unit is pale green due to Ep.The unit is porphyritic and locally moderately sericitezed with well developed quartz eyes. It becomes more feldspar phyric down section. Locally more intense sericite alterations are present near the lower contact. There are minor mafic dykes in this unit that are less than 20cm wide.
191.9 193.6 (4IF75St, Bi, Gt, Py, Po, Qv)[Laminated Interflow Sediments] The unit displays soft sediment deformation (slumping along thinly laminated beds of fine grained Iron Formation and Siltstone. Local Qv are contorted and convoluted
193.6 201.45 (9FP,qe,Bi,Py)[Qued Porphyry]The unit is dark grey to black with minor quartz eyes. It is locally feldspar phyric with trace pyrite. The unit becomes finer grained down section.
201. 207.58 (9QFP, SER,fx,Py)[Quartz Sericite Schist]The unit is cream colour to light grey in colour. The unit is very fine grained and there is locally well developed quartz eyes.
207.58 208.18 (4EF, Bi, Py, Po.Ep, Qcv) [Iron Formation]The unit is dark green to black in colour and locally intense bands of biotite. The unit is fined grained and magnetic Qcv are contorted and convoluted and Py and Po from fine stringers.
208 222.20 (9QFP, fol, Ep.qe, tour, Qv, SER, Kfd, Py) [Quartz Sericite Schist]The unit is light grey to white with a greenish hue. The unit is moderately to locally strongly serialized The unit is very fine grained schist. There is minor quartz veining with tourmaline. Locally the unit is
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-2
FROM TO LITHOLOGICAL DESCRIPTION
feldspathic . In the light green areas of the unit the quartz eyes are unaltered. The lower contact of this unit is at 64 degrees to the core axis.
222.20 228.09 (2U,P,Cv,Po,Lx,Bi)[Pillowed Mafic Volcanics]The unit is fine to medium grained and medium greyto medium green in colour. There are minorstringers of pyrite and pyrrhotite. The unit has a saltand pepper texture of a white lath mineral which isluecoxene.
228.09 229.01 (4EF, Py, PO Ep) [Iron Formation]There is a small interflow sediment of Iron formation is fine grained and medium green in colour. This sub unit is magnetic.
229.01 230.21 (2U, P, Var, Chl, Cv)[Variolitic Pillowed Volcanics] The unit is fine to medium grained and medium green in colour. Pillow selvages are present and are characterized by chloritic alteration. The unit has a variolitic structure near the selvages which are
. l - .5 cm in diameter. There is a weak foliation 64 degrees to the core axis.
DD239.21 241.74 (4FF, Gts, Py, PO, Qcv) D [Iron Formation]D The unit is dark grey to black in colour and fine D grained. It is magnetic and Qcv's are contorted D and convoluted . Garnets tend to form bands and D are amalgamated together to form blobs.
241.74 274.72 (2U, P,bx, Chl, Bi, bc, Ep) [Pillow Mafic Volcanics]The unit is medium green in colour and fine grained. Small there is a small brecciated zone at 243.45 possible flow top breccia. Up to is point the unit has moderate Epidote alteration. The unit the becomes more chlorite and dark grey to black in colour. With in increase in leucoxene and Bi down section. Some minor Pyrite stringers are also present.
274.72 279.04 (9QFP, Ser, qe, Bi, tour Qv.) [Quartz Feldspar Porphyry] The unit is light to medium grained with darker
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-2
FROM TO LITHOLOGICAL DESCRIPTION
brownish sections of the matrix. There is well developed quartz eyes. At the lower contact of the unit is a quartz vein that has tourmaline. The lower contact angle is 27 degrees to the core axis.
279.04 301.65 (2U,P, Lx)[Mafic Pillowed Volcanics] The colour of this unit is variable most of the unit is medium grey to dark grey in colour. There is a small silicified section from 293 - 295 that has a purplish hue to it. There is a small interflow sub unit from 298.40 - 298.8
301.65 305.55 (6U,por) [Gabbro]The unit is recrystallized and has large mafic pheno's. The unit is medium grey in colour and medium to coarse grained.
305.55 307.00 (2U.P , Lx)[Mafic Pillowed Volcanics]The colour of this unit is variable most of the unit ismedium grey to dark grey in colour
307.00 311.40 (9QFP, qe, Ser, qe, Py)[Quartz Feldspar Porphyry]The unit is similar to the above QFP with moderate
serialized near the upper and lower contacts and lessaltered in the middle of the sill
311.40 315 (2U, Lx, Po, Ep) [Mafic Volcanics]The colour of this unit is variable most of the unit is medium grey to dark grey in colour.
315.00 END OF HOLE
DDH Sample Record
Battle Mountain Gold
Property: Placer Hole No: Q97-2 Date: July 8,97 Option
The unit is a fine grained with a greyish purplish sheen. The unit is silicified with intense Qvs and Epvs Hematite and limonite staining is common along fractures. There is a small bullish quartz vein at 10.5 -10.6. Note there is no mineralization associated with any part of this unit. The lower contact angle is 56 degrees to the core axis.
13.70 21.5 (9FP, Hem,fx, Epv)[Feldspar Porphyry]The unit is medium to coarse grained with a
porphyritic texture. The matrix is dark grey to blackSome of the fx pheno's are hematized and the thereis minor hematite veining present.
This unit is a finer grained equivalent of the above. The unit is dark grey to black in colour with a weak
foliation 67 degrees to the core axis. There is minor hematite veining.
29.5 44.65 (9FP, fx, Bi, Qcv, Py)[Armond Lake Porphyry]The unit is feldspar phyric and medium grained to dark grey in colour with feldspar pheno's. The unit has some white mica associated with fractures. There is ^*Mi pyrite which is disseminated through out the unit. Locally the are small ^Ocm sections of weak sericite alteration bands and small injections of a light grey looking QFP.
44.65 48.15 (8U, Py, mag) [Diabase Dyke]The unit has a birds foot diabase texture to it and is weakly to moderately magnetic.
48.15 117.3 (9FP, fx, Hem.Sil, Ser,Qv, Bi) [Armond Lake Porphyry ] The upper contact of this unit is silicified and hematized. The unit is medium grained and dark
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-3
FROM TO LITHOLOGICAL DESCRIPTION
grey in colour. Pyrite within the unit is *:i"7o and disseminated and blebs. The unit is feldspar phyric and Small *^1 cm quartz veins are anastomosing through out the unit. Hematite straining is present around the edges of Qvs and around the rims of feldspar phenocrysts. Locally there is a variation in the diameter of the feldspar pheno's from coarse to fine grained. There is some sections of intense Sericite alteration laminations at 52.8 - 53 and 54.5 - 54.7. The mineralization with in these altered zones also increases to 20Xo. There are variation in the colour of the unit from 63.5 to 87.70 Silicification is pervasive and weakly serialized. Quartz eyes are rare. At 87.70 there is a quartz vein with large cluster of massive pyrite. There is multiple phase of the Armonad Lake Porphyry. From 90.5 - 96.5 the unit is coarse grained and biotitic. Feldspar pheno's are .5 l cm in diameter and have a weak foliation 63 - 65 degrees to the core axis and no mineralization is associated with this coarse grained phase of the9 FP (Armand Lake Porphyry). From 96.5 to 117.3 is the finer grained equivalent of the above this unit is dark grey to black in colour and more silicified with pyrite ^"/o. Quartz veins have hematite along the rims. At the lower contact the unit is silicified and there is minor stockwork fractures present.
117.30 121.10 (6U,Bi, Carb) [Gabbro]The unit is coarse grained with large mafic pheno's. The unit has medium green in colour and has a mottled appearance.
121.10 123.00 (9FP, fx, Bi, sw,)[Feldspar Porphyry]The unit is multi phased from fine to medium grained variations of the same Porphyry. The unit is light grey to black in colour. The unit is feldspar phyric in colour.
123.00 127.53 (9FP, Sil, Qv, sw, Epv, Hemv.alt'd)[Weakly Altered Feldspar Porphyry]The unit moderately to intensely silicified with stockwork fractures and quartz veins. The unit is fine grained and light grey in colour with a purplish hue. No mineralization is associated with this unit.
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-3
FROM TO LITHOLOGICAL DESCRIPTION
127.53 139.44 (9FP, fx, Py)[Feldspar Porphyry]Again the unit has variable phased porphyry which varies from fine to medium grained. The unit is dark grey to black in colour with fx pheno's. Pyrite is Wo and finely disseminated and blebs The Upper contact angle is 62 degrees to the core axis and the foliation is 66 degrees to the core axis. The lower contact is crushed.
139.44 142.76 (9QFP, massive, qe, PK, Bi, Hemv, Qv) (Quartz Feldspar Porphyry] This small QFP unit has a strongly hematized upper contact which fizzles out at 140 massive. The unit is coarse grained and qe's are l cm in diameter and well developed. The unit has a pink fleshy colour due to moderate alteration and fades out near the lower contact of the unit. The LCA is 70 degrees to the core axis.
142.76 152.12 (9FP, fx, Hemv.Epv) [Feldspar Porphyry]Again the unit is medium grained and dark grey in colour with fx pheno's. There is minor hematite micro veins which are a deep reddish colour while
Epidote veins are lime green in colour. There is asmall zone of 151.75 where intense hematite and epidote veins. The lower contact is at 55 degrees to the core axis. The foliation in this unit Is weak and 63 degrees to the core axis.
152.12 171.95 (2U/ 5St, Qcv, Py, Sil)[Mafic Volcanic with Interflow Sediments] Mafic Volcanics are moderately silicified with a weak foliation 66 degrees to the core axis. There are small interflow sediment sub - units with pyrite bands. These units look more altered than the
mafics and are equigranular. Some area look to beweakly developed calc silicate bands. There is a minor l massive coarse grained dyke at 170.95 - 171.95
The upper contact of the unit is a hematizedaltered "fragmental 1 from 171.95 -172.25 .The uppercontact is a deep pastel red colour with epidote
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-3
FROM TO LITHOLOGICAL DESCRIPTION
veins that are lime green veining the unit goes from being a "fragmental" to a silicified Iron Formation. The unit is greyish green in colour and banded. It is fine to mediummassive grained and weakly biotitic. There are minor garnets are associated with quartz carbonate veins and numerous pyrite and pyrrhotite stringers are sub - parallel to the foliation which is 67 degrees to the core axis. Locally semi massive stringers of pyrite .51 cm wide. The matrix is platy and looks to be a silicified argillite locally. There are minor alteration bands of sericite at 189.5 - 190.5 and 198.25 - 198.75. There is minor grey feldpathized bands from 190-195 metres. The sediments are intensely altered from 198 - 200.5 where sericite is moderate and there is weak feldspathization bands. The sulphide content decrease down section and the unit becomes more coarse grained SSt.The entire unit is moderately to strongly magnetic.
200.20 239.00 (2U, fol,Bi,Py,Qcv)[Weakly Foliated Mafic Volcanic]The unit is equigranular with fine pyrite stringers and small altered zones of semi massive pyrite epidote and quartz carbonate veins at 216.85 - 216.95 and at221.10 - 221.30. There is whitish feather looking pheno's that are not Carbonate Possible Lx or altered garnets. The unit is variable in both grain size and colour. It ranges from black in fine grained areas to medium green in medium grained area of the unit. And sometimes takes on a mottled appearance.There are weakly laminated alteration sections of the unit where the unit is sericitized and silicified. These alteration bands have a pink to purplish hue and are mineralized they occur at 226.8 - 227 and 227.87 - 228.09 Pyrite is 3 07o in these zones
239.03 241.94 (4IF, Qcv, Py, Mag, Epv)Chemical Metasediments Iron Formation.The unit is black in colour with Qcv and pyrite. The unit is magnetic and fine grained.
241.94 259.80 (2U, Bi, Ep ,Qv, Sw, Alt'd) [Mafic Volcanic] The unit has a mottled appearance and the biotite is
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-3
FROM TO LITHOLOGICAL DESCRIPTION
parallel to the foliation 63 degrees to the core axis. There is a small 4EF, Gts, Py, PO, Qcv section at 257.59 to 257.68 The unit is dark grey to black in colour and fine grained. It is magnetic and Qcv's are contorted and convoluted . Garnets tend to form bands and are amalgamated together to
form blobs. There is a good serialized zone oflaminations at the lower contact of this unit.
259.80 265.33 (9Fp, fx, Bi)Feldspar PorphyryThe unit is light to medium grained with dark grey sections. The feldspars are well developed in the matrix. With a foliation of 63 degrees to the core axis.
265.33 275.74 (2U, Epv, Qcv) Mafic VolcanicThe unit is a mafic volcanic with sub- units of 9FP and minor interflow sediments of dense magnetic iron formation with garnets and biotite. The unit is very dense between 267.07 and 267.21
275.65 286.91 (SstMIF, Gts, Bi, Mag.)Clastic and Chemical Metasediments The sediments are dark grey to grey in colour. And medium to fine grained the unit is very dense. There is a small feldspar porphyry sill between 286.76 and 286.91.
286.91 344 (2U, P.bx, Chl, Ep.Sil, PY, Po, Gts)[Pillow Mafic Volcanics]The unit is medium green in colour and fine grained. There are small brecciated zones that are possibly flow top breccia. These zones are lime green form intense epidote alteration and are mineralized with Py 207o - 3 0Xo and Po Wo - V/o. These sections are 10 - 15 centimeters wide and in some sections these breccia's look like fragmentals. There are some interflow sediments in the unit with garnets and Po. They are weakly magnetic
344 377.46 (9QFP, Ser, qe, Bi, Qv, svv) [Quartz Feldspar Porphyry]developed quartz eyes with greyish pale white
pheno's of quartz feldspar rims are washed out
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-3
FROM TO LITHOLOGICAL DESCRIPTION
by moderate sericite. In some areas the unit is a buff colour.
377.46 386 (2U, sil)Mafic VolcanicsThe unit is medium green in colour and fine tomedium grained and massive looking. The unit ismoderately silicified and has that purplish sheen toit
386 END OF HOLE
DDH Sample Record
Battle Mountain Gold
Property: Placer Option
Hole No: Q97-3 Date: July 14,97
Q97-3-001
Q97-3-002Q97-3-003
Q97-3-004
Q97-3-005
Q97-3-006Q97-3-007
Q97-3-008
Q97-3-009
Q97-3-010
Q97-3-011
Q97-3-012
Q97-3-013
Q97-3-014
Q97-3-015
Q97-3-016
Q97-3-017
Q97-3-018
Q97-3-019
Q97-3-020Q97-3-021
Q97-3-022
Q97-3-023
Q97-3-024
Q97-3-025
Q97-3-026
Q97-3-027
Q97-3-028
Q97-3-029
Q97-3-030
Q97-3-031
Q97-3-032
Q97-3-033
Q97-3-034
Q97-3-035
Q97-3-036
Q97-3-037
Q97-3-038
49
5051
52
53
54
55
5657
58
59
64
65
66
67
71
72
73
74
75
76
77
78
79
80
81
82
83
102
103.1
104
113.05
114
115
176
177
178
179
50
51
52
53
54
55
56
5758
59
60
65
66
67
6872
73
74
75
76
7778
79
80
81
82
83
84
103.1
104
105
114
115
116
177
178
179
180
1.00
1.001.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.001.001.00
1.001.00
1.00
1.00
1.00
1.01
0.99
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
^13
6
6
^^^9
8
^
9
^^
15
7
^
^
^
^
8
6
^^
7
^
8
^
7
^
^
^
^
^
^
^
8
^11
ii^iiliii
^
^
6
^
DDH Sample Record
Battle Mountain Gold
Property: Placer Option
Hole No: Q97-3 Date: July 14,97
llililiiilltliiilttilllfc
Q97-3-039
Q97-3-040
Q97-3-041
Q97-3-042
Q97-3-043
Q97-3-044
Q97-3-045
Q97-3-046
Q97-3-047
Q97-3-048
Q97-3-049
Q97-3-050
Q97-3-051
Q97-3-052
Q97-3-053
Q97-3-054
Q97-3-055
Q97-3-056
Q97-3-057
Q97-3-058
Q97-3-059
Q97-3-060
Q97-3-061
Q97-3-103
Q97-3-104
Q97-3-105
Q97-3-106
Q97-3-107
Q97-3-108
Q97-3-109
Q97-3-062
Q97-3-063
Q97-3-064
Q97-3-065
Q97-3-066
Q97-3-067
Q97-3-068
Q97-3-069
180
181
182
183
184
185
186
187
188
189
190
191
192
193
194
195
196
197
198
199
200
201
202
225.81
226.81
227.81
229.81
257.77
258.77
259.77
317
318
319
320
321
322
323
324
181
182
183
184
185
186
187
188
189
190
191
192
193
194
195
196
197
198
199
200
201
202
203
226.81
227.81
228.81
230.81
258:77
259.77
260.77
318
319
320
321
322
323
324
325
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
9
10
10
7
^10
7 ^
^7
8
6
8
^
^
^
12
^
^
9
9
^
^
13
13
11
^
^
^
11
^
^
15
^
6
^
6
13
11
^
^
*5
limit! iifiiiiptt JS^^^sSS^^SSS
DDH Sample Record
Battle Mountain Gold
Property: Placer Option
Hole No: Q97-3 Date: July 14,97
Q97-3-070Q97-3-071
Q97-3-072
Q97-3-073
Q97-3-074
Q97-3-075Q97-3-076Q97-3-077
Q97-3-078
Q97-3-079
Q97-3-080
Q97-3-081
Q97-3-082
Q97-3-083
Q97-3-084Q97-3-085
Q97-3-086
Q97-3-087
Q97-3-088
Q97-3-089
Q97-3-090
Q97-3-091
Q97-3-092
Q97-3-093
Q97-3-094
Q97-3-095
Q97-3-096
Q97-3-097
Q97-3-098
Q97-3-099
Q97-3-100
Q97-3-101
Q97-3-102
Q97-3-103
llliiliitllilllili
325
335
336
337
338
339
340341
342
343
344
345
356
357
358359
360
361
362
363
364
365
366
367
368
369
370
371
372
373
374
375
376
377
326
336
337
338
339
340
341342
343
344
345
346
357
358
359360
361
362
363
364
365
366
367
368
369
370
371
372
373
374
375
376
377
378
1.00
1.00
1.00
1.00
1.00
1.00
1.001.00
1.00
1.00
1.00
1.00
1.00
1.00
1.00
1.001.00
1.00
1.00
1.00
1.00
1.00
1.001.001.00
1.00
1.00
1.00
1.001.00
1.001.001.00
1.00
if^^^al^^^^^^^^^17
^9
22
14
9
41^
^
13
^
11
35
25
17
81
52
^
14
^^
^
^
^
^
illiiiifl^
23
wmmfc iippfpp
Note: There is a
The 1 m intervalDuplicate Sample Number Q97-3-103 The correct values are as follows
from 225.81 - 226.81 is 13 ppb and from 377 - 378 is ^ ppb
ACCURASSAY LABORATORIESJL A DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE. UNIT ?THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX(807)623-6820
Page l
BATTLE MOUNTAIN CANADA INC.40 MANITOU RD., P.O. BOX 100, SUITE 103MANITOUWADGE, ONTARIOPOT 2COFAX (307)826-4440ATTENTION: COLIN MACKENZIE
7.00 21.12 (7GD.6D Bi, py)[Granodiorite l Diorite]The unit is diorite looking with a mottled greyish white appearance locally weak alteration bands. There are flecks of pyrite. The groundmass is biotitic and the lower contact is cut by a quartz carbonate vein. There is a weak foliation, which is 63 degrees to the core axis
21.12 22.45 (5st74IF, PY)[Clastsic and Chemical Sediments]The unit is medium green in colour and vuggy locally. The unit is medium to fine grained and very dense There are several contorted and convoluted small altered section of chlorite stringers. Pyis3'Yo and blebs to disseminated. The sulphide content decreases at 22.59. There is a small-altered section between 23.31 and 23.40 of greyish pink feldspathic bands.
22.59 38.32 (9QFP, qe, fx, Epv, sw.Ser, Py) [Quartz Feldspar Porphyry] The unit is grey to medium grey in colour and fine to medium grained. It is porphyritic with feldspar pheno's, There are well developed quartz eyes and weak to moderate sericite alteration laminations. There is some quartz veins and minor stock work and Epidote veining. The foliation is 60 degrees to the core axis and the lower contact is 67 degrees to the core axis.
38.32 47.47 (SstMIF, Chl, Sil, Qcv, Py)[Interbeded Clastic and Chemical Sediments]The unit is dark grey to black, fine grained, and dense. There are small pyrite nodules, which are very rounded and minor Quartz carbonate veining The unit is locally thinly bedded but mostly massive looking. Locally the unit is magnetic
47.47 52.09 (2U, Bi, fol, Ser, alt'd)[Weakly Altered Mafic Volcanics]The over contact of the unit is marked by a maficfragmental. The unit is medium grained and weakly
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-4
FROM TO LITHOLOGICAL DESCRIPTION
to moderately serialized with weak alteration laminations. The unit is weakly foliated at 63 degrees to the core axis. Locally Py is along the alteration bands and Minor calc- silicate bands exist near the lower contact of this unit and a small dyke of Feldspar porphyry.
52.09 56.15 (5stX4IF, Bi, Gts, Py, Po)[Interbcded Clastic and Chemical Sediments]The unit is greyish brown colour with laminations and banding. There is pyrite along foliation massive Po and locally magnetic. The unit is well foliated 63 degrees to the core axis. It is weakly altered in areas
56.15 81.53 (2U, Var, Py.Epv, Py) [Variolitic Flow]The mafics are medium green to medium grey in colour the Py is associated with the foliation. The varioles tend to be concentrated along subtle more altered zones of the unit. They are less than .5 mm in diameter. There is also minor feldspathic bands at 60.5 to 60.60 the alteration laminations in this small zone are tan coloured and smoky grey in colour. Locally the unit is silicified
81.53 87.5 (9FP, Bi, fol, fx)[Feldspar Porphyry]
The unit is light to medium grey in colour andmoderately foliated locally the unit becomes coarser grained and feldspar pheno's are present.
87.5 93.66 (9QFP, qe, fx, Ser, kph, py sw) [Quartz Sericite Schist]The unit is moderately to strongly serialized. There is good alteration laminations. The unit is medium grey to buff coloured The unit has a wispy appearance and is moderately foliated at 63 degrees to the core axis.
93.66 94.90 (9QFP, SER, Bi, tour, kph, Py, MO) [Sericite Schist]The unit is blitzed. There is intense sericite alteration laminations bands 63 degrees to the core axis with a wispy appearance. There is tourmaline and possibly MO at the upper contact of this unit
94.90 101.70 (9QFP, qe, fx, Ser, Epv, py sw)
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-4
FROM TO LITHOLOGICAL DESCRIPTION
[Quartz Sericite Schist]The unit is medium to fine grained medium to light grey in colour. Quartz eyes are well developed and stretched out along the foliation There is a intensely altered section from 97.78 - 97.96
101.70 108.18 (9FP,fx, Bi, Ser, Py) [Feldspar Porphyry]The unit is medium to dark grey in colour and medium grained. It has a biotitic groundmass and porphyritic and feldspar phyric. Weak sericite locally with trace pyrite.
108.18 120.33 (6U)[Mafic Intrusive]The unit is medium green in colour and very coarse grained almost likes like a Pyroxenite. It has large mafic phenocrysts. Of an augen shaped mineral.
120.33 136.60 (9FP, fx, qe, Py)[Feldspar porphyry]The unit is dark grey in colour and medium grained. Quartz eyes are weakly developed and rounded. While feldspar pheno's are stretched out along the foliation 63 degrees to the core axis There is minor quartz veining and pyrite flecks.
136.60 171.5 (2U,P, bx, PY, PO Qcv, ser)[Mafic to Massive Pillowed Flows] The unit is pillowed to massive and medium green to dark grey in colour. The unit is fine grained and locally brecciated The unit is well mineralized in the upper portion of the section between (143-146) with Py locally 407o and PO locally 3 -4 "/o. The Mineralization steadily decreases down section and the unit becomes more medium grained down section starting at 156. Also minor quartz carbonate veins are present down section.
171.5 173.51 (9FP, fx.qe, ser, sw) [Feldspar Porphyry]The unit is light to medium grey. Sericite is locally weak at 172.80 - 173 sericite laminations. The lower contact of this unit is at 63 degrees to the core axis.
173.51 239 (2U, P.Qcv, Bx.Ser, Py) [Pillowed Mafic Flow] The unit is medium green in colour and fine to
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-4
FROM TO LITHOLOGICAL DESCRIPTION
medium grained there are several localized areas of minor sericite alteration associated with pyrite Mineralization. In some of the small breccia zones epidote overprints the unit. There is minor Quartz carbonate veins. The Py Mineralization was associated with the small breccia zones that occur in the unit.
4.0 6.5 (2U, fol, mot, Carb, Qcv )[Well foliated Carbonitized Mafic Volcanic] Mafic Volcanic: medium to coarse grained with a mottled appearance. Medium to dark grey in colour. Note, carbonate is part of the ground mass, and moderately pervasive.
6.5 19.30 (9QFP, Ser, fx, qe, Py, Bi))[Quartz Feldspar Porphyry] QFP: the unit has a porphyritic texture and crystalline. It is medium grained and light to medium grey in colour. The QE's are rounded and feldspar phenos and biotite with in the groundmass are elongated along the foliation
19.30 92.61 (2U,P,Bx, Qcv, Var, Py )[Carbonatized Pillowed Mafic Volcanic Flows] Mafic Volcanic: Fine to medium grained and medium to dark grey in colour. Again Carbonate is part of the groundmass and Quartz carbonate veins are present. There are pillow selvages and flow top breccia units which are variolitic. The unit has minor zones of sericite lamination alteration at 39 - 41 metres and at 66 66.5 metres. The lower contact of the Mafic unit has small lath to feather shaped white porphoblasts which may be carbonate. Note that this unit is weakly magnetic . There is a small 9FP at 70.2 - 71. The unit becomes more massivelooking down section locally some silicified sections are present near quartz carbonate veins. There is the loss of variloes down section. The pillow selvages and brecciated units are epidote altered.
92.61 113.19 (9QFP, fx, qe, sw, Epv, Bi, Ser, Py) [Quartz Feldspar Porphyry]The unit is variable in colour and is dependent on sericite and epidote alteration that is present. The unit is dark grey to light grey in colour with a biotitic groundmass. There is weak to moderate sericite alteration laminations that are light green and yellowish in colour. There is well developed quartz eyes. There is a weak stockwork present. The
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-5
FROM TO LITHOLOGICAL DESCRIPTION
foliation is 63 degrees tot h core axis. As you proceed down section qe increase in diameter and feldspar pheno's are non existent. The unit is dark grey with 2*Ki local pyrite. There is good sericite alteration near the Mafic contact at 112.03 -113.19. Note the tourmaline in this small zone at 111.02
113.19 124.25 (2U, Ep.Bi, Qcv, Py) [Mafic Volcanic]Mafic Volcanic: The unit is medium green in colour and medium to fine grained. There is a altered section from 117.03 - 117.25 of Epidote and Qcv that host 2 - 3 "/o Py. Qcv increase down section and become contorted and convoluted. Some Qcv's have pinkish carbonate associated with them.
124.25 130.70 (9FP, fol, fx, alter'd, Ser, Py) [Feldspar Porphyry]The unit is a dark grey with local laminations of sericite and pyrite mineralization. The foliation is 63 degrees to the core axis. The unit is feldspar phyric and with local pyrite 2 - 3 7o from 127.35 - 127.50. The unit is also intensely silicified in local areas.
130.70 135.70 (2U, Ep, Bi, Py) [Mafic Volcanic ]The unit is medium grained and light green in colour with minor Qcv's and local pyrite l - 207o
135.70 138 (9QFP, Sil, Py, Ep, Py)[Quartz Feldspar Porphyry]The unit is intensely laminated and banded with sericite and epidote wispy layers. These wisps are pale green in colour.
138 160.70 (9FP, Epv, fx, Bi, sw) [Feldspar Porphyry]The unit medium to fine grained and light to dark grey in colour. The unit has a biotitic groundmass and is feldspar phyric. There is a weak foliation which is 62 degrees to the core axis. There is minor Qcv's with some locally intense Epidotization and sericite alteration at 160.45 - 160.70
160.70 166.85 (2U, Qcv, Bi Py) [Mafic Volcanic ]The unit is medium grained and medium green in colour. It has a mottled appearance Very
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-5
FROM TO LITHOLOGICAL DESCRIPTION
similar to the above Mafic units.
166.85 182.79 (9FP, Ser, Sil,fx,Bi) [Feldspar Porphyry]The unit is weakly altered and dark grey to greenish grey. It is medium grained and weakly foliated with minor stockwork. There is weak sericite laminations locally. The unit is feldspar phyric and has a biotitic groundmass. In some areas the unit is vuggy in appearance.
182.79 201.5 (2U, M, Bi, Gts, Qcv.Py, Po) [Massive Mafic Volcanic] The unit is a massive volcanic. It is dark grey to black in colour. There are minor quartz carbonate veins l - 20X0 Py locally stretched out along the veins. Garnets are well developed at the upper contact.
201 212.04 (9QFP, fx, qe, Ser.Bi.Py) [Quartz Sericite Schist] The unit is a quartz eye sericite schist and is fine grained and light grey to greenish in colour. There is moderate to strong sericite alteration l - 2Vo disseminated pyrite and well developed quartz eyes with minor stockwork. The unit is moderately foliated and has a wispy looking appearance.
212.04 220.56 (6U)[Mafic Intrusion]This Mafic intrusion has large black pheno's and medium green in colour. There is some more carbonate veining.
220.56 232.90 (9QFP, Ser, fx, qe, Bi)[Quartz Feldspar Porphyry]The unit is light grey in colour and fine to medium grained. The quartz eyes are well developed quartz eyes and moderate sericite alteration as fine wispy laminations. The unit is well foliated 63 degrees to the core axis. The sericite laminations have a weak crenulation cleavage and a biotitic groundmass. Near the lower section of the unit it is finer grained.
232.90 278.0 (2U, P.fol, Qcv, Ep)[Pillowed Mafic Volcanics]The unit is medium grained and medium green to black in colour. The Pillow selvages and small flow top breccias are marked by an increase in epidote
Battle Mountain Gold
DIAMOND DRILL LOGPROPERTY: QUED (PLACER OPTION)
HOLE No.: Q97-5
FROM TO LITHOLOGICAL DESCRIPTION
alteration. Locally there are garnets present. The unit has a pale green hue to it and very similar to the Mafic units in Quartz phyric97-3
278 END OF HOLE
DDH Sample Record
Battle Mountain
Property: Placer Opion
Hole No: Q97-5 Date: July 16,97
. - - : . -. ; ' ,: : - ,. ;. -' -
Sample^Q97-5-001
Q97-5-002
Q97-5-003Q97-5-004
Q97-5-005Q97-5-006
Q97-5-007
Q97-5-008Q97-5-009
Q97-5-010
Q97-5-011
Q97-5-012
Q97-5-013
Q97-5-014Q97-5-015
Q97-5-016
Q97-5-017
Q97-5-018
Q97-5-019
Q97-5-020
Q97-5-021
Q97-5-022
Q97-5-023Q97-5-024
Q97-5-025Q97-5-026
Q97-5-027
Q97-5-028
Q97-5-029
Q97-5-030
Q97-5-031Q97-5-032
Q97-5-033
Q97-5-034
Q97-5-035Q97-5-036
Q97-5-037Q97-5-038
: ^.FrQm;iiJ!;!6.57.5
8.5
9.510.5
11.5
12.5
13.514.5
15.5
16.5
17.5
18.5
3839
40
41
64.73
65.73
66.73
92
9394
95
9697
98
99
100
101
102
103104
105
106
107108109
H^lo-!'; :47.5
8.5
9.5
10.5
11.512.5
13.5
14.5
15.5
16.5
17.5
18.5
19.5
3940
41
42
65.73
66.73
67.73
9394
95
9697
98
99
100
101
102
103
104105
106
107
108109110
: : : : : ^V ^
Width11111111111111111111111111111111111111
J : : ; : . ' :. . ; ; ; ' : ; ': : ; !; 3 : , . i f \ : ;| 1 i ;! ;| ; ;; :; s SSsASSaySf 1 W i 'l^':.'Au (ppb)
3U felsic to intermediate3R rhyolite3D dacite3A andesite3T trachyte
CHEMICAL META-SEDIMENTARY ROCKS
4U chemical sediments4IF iron formation4IC cherty iron formation4IFO oxide iron formation4C chert4GF graphite4G1F grunerite iron formation4B baritic sediments
Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.O. 1990
Transaction Number (office use)-WL
Assessment Files Research Imaging
Personal inform! Mining Act, the ii Questions atou 933 Ramsey La*
Instructions:
42C13SW0177 2.17606 WABIKOBA LAKE
Please type or print in ink.
900
and 66(3) ot the Mining Act. Under section 8 of the ent work and correspond with the mining land holder. ' of Northern Development and Mines, 6th Floor,
n Jaim, use form 0240.
1. Recorded holder(s) (Attach a list if necessary)/f
Name ~
i laC-t? i' Oc •^-eAddress
Name
(U. LW,
.X &-C
tU L^-Ucl9o iw*f*,SuiU we iMSH 3, P 5
•-eta LVclAddress
\o Wdyt. l Jo "JT tO ^W;r-\j^ ^4- Jcv^TU-
^Tv ^ \ ^ l/ M 7 T s^
Client Number
Telephone Number
Fax Number
Client Number l O ~2 *T ^ A
Telephone Number
(70s ) 'J* G8 - ^400Fax Number
(.To ~^ ) P- fc S ' Q "i T ̂
2. Type of work performed: Check ( s ) and report on only ONE of the following groups for this declaration.
D Geotechnical: prospecting, surveys, rpf Physical: drilling, stripping, l — l Rehabilitation assays and work under section 18 (regs) ' — ' trenching and associated assays ' — '
Work Type
Dates Work ^ ,. , .,,- . A Performed From ^ , ^^ 1^7 To ^7 C7 /q^/
Dty 1 Month Yor Oty | Month Yea'Global Positioning System Data (it available) Township/Area
M or G-Plan Number
^ 63c
Office Use
Commodity
Total S Value of Work Claimed
NTS Reference
Mining Division "//^rf y
Resident Geologist / District
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.
3. Person or companies who prepared the technical report (Attach a list if necessary)Name ^
nfr. __ __ — _________ , do hereby certify that l have personal knowledge of the facts set(Print Name)
forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.
iHIfiING CLAIM NUMBER. Or -T INUW3ER C- CLA.N:,ALUE D? '*3'A irfork .-as don* on o:h*r el^ibie ;jH!TS.F;r othr'CERFORME: " : ! mi nine land . znow in this columnlminin? '-and. :; 'air, or :-'S' Ithe location numaar indicated !:-st Hectares. -r,n; 'ar; Ion the claim mac. !
Qft t 13
OF WOPK B4NKoth*r to e
of
a fu"u': ' ""' "'""
TG "5i-:S y 14.324.00 !1 2 y f,,. 3 400.30 3.051,00
rork ulation . UnderPersonal information collected on this form is obtained under the authority of subsection 6(1) of J
section 8 of the Mining Act, the information is a public record. This information will be used to revfew the assessment work arlQ correspond with the mining land holder. Questions about this collection should be directed to the Chief Mining Recorder, Ministry of Northern Development and Mines, 6th Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.
Work Type
}:*~*~A YX.lU,,U.,
nS*ie.iAi.^M
Units of WorkDepending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.
((cOM vr\
•U , ___ ^ ^
M^fc^,Lv0
j
ssociated Costs (e.g. supplies, mobilization and demobilization).
]rA \ A \\ \ Mcp^r V^^ VY^V)
C~ "T Urc lr̂ V —— — ————
Transportation Costs
ReAA V-A 4 cus
urN vjo-^,i\riiFood and Lodging Costs
L^. ^ , w^ ro1
Cost Per Unit of work
a^/U") T 7 1 i i/ /-^l hr\U-v autt
\
(O-YO /W^l
Total Value of Assessment Work
Total Cost
?e ^y?.ooft.O^H-00
LfMoo
i77o-00
Sfcc -co
^/5-co
tooo
9^-00
/W.fi^-o)
Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at 10007o of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 5007o of the Total
Value of Assessment Work. If this situation applies to your claims, use the calculation below:
TOTAL VALUE OF ASSESSMENT WORK x 0.50 = Total S value of worked claimed.
Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.
Certification verifying costs:
, do hereby certify, that the amounts shown are as accurate as may(please print full name)
reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on
the accompanying Declaration of Work form as
to make this certification.(recorded hdlder, agent, or state company position with signing authority)
l am authorized
Signature
0212 (02/95'
Date
i/L
Ministry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines Ontario
October 17, 1997
PLACER DOME (CLA) LIMITED 130 ADELAIDE STREET WEST P.O. BOX 43, SUITE 3201 TORONTO, ON M5H-3P5
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.
If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at [email protected] or by telephone at (705) 670-5855.
Yours sincerely,
ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section
Correspondence ID: 11465
Copy for: Assessment Library
Work Report Assessment Results
Submission Number: 2.17606
Date Correspondence Sent: October 17, 1997 Assessor: Ste ve Beneteau
Transaction Number
W9740.00846Section:16 Drilling PDRILL
First Claim Number
1164418Township(s) l Area(s)
WABIKOBA LAKE
Status
Deemed Approval
Approval Date
October 17,1997
Correspondence to:Resident Geologist Thunder Bay, ON
Assessment Files Library Sudbury, ON
Recorded Holder(s) and/or Agent(s):PLACER DOME (CLA) LIMITED TORONTO, ON
George J. KoleszarBATTLE MOUNTAIN CANADA LTD.TIMMINS, ONTARIO
Page: 1Correspondence ID: 11465
Di-AV*i\ niven va - o o w51' 50 49' 48' 47' 85*45'
AREAS WITHDRAWN FROM DISPOSITION
M. P.O. - MINING RIGHTS ONLY
S.fT.Q. - SURFACE RIGHTS ONLY
M.+ S. - MINING AND SURFACE RIGHTS
Dweription Order No. Dit. Disposition File
__ - ,____
205284Lampson
RlLands subject to easement for tailings disposal(Bomby twp. landrail)- easement 384-10 12083
P l NE G ROVE_ Surface and mining rights withdrawn
from staking order W 33/85, 18/12/85.
Surface rights withdrawn from staking order W 38/83, 20/10/83.
2187218782-.—~l-.Surface rights withdrawn from staking order W 22/84, 14/09/84.
1217099^I^LfflSiwra
Surface rights withdrawn from staking order W 10/85, 02/10/85. 209920 203260 |6833M
RAILWAY AND RIGHT OF WAYUTILITY LINESNON-PERENNIAL STREAMFLOODING OR FLOODING RIGHTSSUBDIVISION OR COMPOSITE PLANRESERVATIONSORIGINAL SHORELINEMARSH OR MUSKEGMINESTRAVERSE MONUMENT
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENT SYMBOL
PATENT, SURFACE 8t MINING RIGHTS.._.............. W.SURFACE RIGHTS ON LY........................ O.MINING RIGHTS ONLY___.................... O
LEASE, SURFACE 4 MINING RIGHTS——————— B" .SURFACE RIGHTS ONLY._...................... H" , MINING RIGHTSONLY..._———.—..—.... B
LAND USE PERMITS FOR COMMERCIAL TOURISM. OUTPOST CAMPS ^NOTE: MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6.
1913, VESTED IN ORIGINAL PATENTEE BY THE PUBLIC LANDS ACT, R.S.O. 1970. CHAP 380, SEC. 63, SUBSEC 1.
SCALE.: 1 INCH = 40 CHAINS
FEETO 1000 2OOO 4000 6OOO 8000
O 200METRES
1000(1 KM)
2000(2 KM)
SOLONG LAKE SUBJECT TO FLOODING TO ELEVATION GSC 323.75 METRES
Land* Surrounded by This Marking v* Subjtct le " See. 189 EaMnwnt 084-IO.
3*4 Bomby Landrail
* * u y TNs MarW"9 "*? ?d 0K*,r rlftht'- M P*r s*c--14. S.. Whit* Lain N, Landroll.
NOTE.- Th* above Easements Run With Th* Land And Will Affect L*OMI And Patents.
42C13SW0177 2.17606 WABIKOBA LAKE 200
6 1997
The information that appears on this map has been compiled from various sources and accuracy is not guaranteed. Those wishing to stake MINING CLAIMS should consult with the MINING RECORDER Ministry of Northern Development and Mines for additional information on the status of the lands shown hereon.
cal cold*. carb carbonate di carbon dan carbonaceous
carouRvi
STB esmj MINERAL I CODE
runs*rtauroVtt
itaurolH* rt*nc* ctauroin* METAMORPHIC
l tAHSLATION
Cm CSn CCSHIH? CDn
i nor andaiKtt* rttnc* andalusite
M terate calc*twcat*s
cordkrrlte
snr ftuorttefu fuchstteat gamt9f 5-apMteon galenaos gravel and cand
DOtW GtH GTn CGTnl Sin - SLn ... tSLnl Stn
Ttense corolerlt kyanite
itense kyanitegarnet
-,- garnet itense garnit
Ix leucoxeneri nlcank nfcrolht^
nu Muscovite
1-3Z ankerite ve AV 5-1SX ankerite [AV] >ax ankerite C v 1-SI calcite CV 3-13): calcite CCV1 vat caldte Qav 1-5X quartz ai OAV S-ISX quartz i IOAV) )13X quartz
Ocv 1-R quart! OCV 3-13* quartz IOCVJ M3X quartz Epv I-n ephbte vi EPV 3-13X epidote i DZPVl )I3X epbtote ' Mtv 1-SX pwanetfte
MINERALS AND ELEMENTS onk onkeme•b olblte ok .cttioltte on upHboni oh anhydrite asp orstnopyrtte au gold ba barite U biotite cal catctti carb carbonate
GRANITES MAFIC TO ULTRAMAFIC INTRUSIVE 61 DIORITE, TRDNDHJEHITC f ———
9 CLASTIC SEDIMENTS SR ARGILLITE 5 RG GRAPHITIC ARGB-UTE 9 i CALC-SHJCATE BEARING SEDIMENTS ST SILTSTONE
CHEMICAL SEDIMENTS
4 : CHERTY IRON FORMATION 4] 'S SULFIDE IRON FORMATION
CHERT + F GRAPHITE3 FELSIC TO INTERMEDIATE VOLCANICS 31 RHYOUTC 3 DACITE 3 ANDESITE 3 TRACHYTE 3 MAFIC VOLCANICS Z THOLEIITIC BASALT
' RON THDLEimC BASALT a B MAGNESIUM THOLEIITIC BASALT S A CALC-AUAUNE BASALT 11 ULTRAMAFIC VOLCANICS If PUtlBUIlirc KOHATnTE U BASALTIC KOMATUTE Ut OVERBURDEN