52FI6SWe«S3 LAVAL 010

Diamond Drilling

Township of LAVAL Report NQ 1 0

Work performed by: Canadian Nickel Co. Limited

Claim NQ

K 2569U2

Hole NO

H2739

U2740

Footuge Date

430.0'

378.0'

So?

May/70

Hay/70

Note

(i)

(i)

Notes:

(1) #7-71 Brownridge Twp.

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BOREHOLE* 4?739-0

PROPERTY OINCRWIC

********•***••*•*****»***«

BOREHOLE R ECORD DATE PROCESSED JAN 07,1971

* ********•»**•»•**••**• ******* 4

NTS* SH» ANOM* DEPTH AZIMUTH QIP LATITUDE DEPARTURE ELEVATION LEVEL52F I6W 30 5 430 90 00 -50 00 N 400 W 470 DATE............

*•»»»**•*•* ******••••********••*••**•***»•***»****•***•*************•****»**••*»*»**•**•INCLINATION AND TROPftRI TFSTS

DEPTH AZIMUTH DIP DEPTH AZIMUTH DIP DEPTH AZIMUTH PIP300 -43 30 *00 -42 30

****** ******** ******* ******************* **************************

DEPTH0.0

17.0 22.8

LENGTH MNZN ROCK0.0

17.0 5.8 MVW OTE

"fcPTM AZIMUTH DIP DEPTH AZIMUTH DIP 10C -50 15 200 -45 45

*******••*••••***•**•********•***4

TOPS OF WEDGES*••»»» •***************»«**•»»******»** *********************** ************ ***************** A*************************************

COMMENTS irr.GEO BY..GJ KOLESZAR STARTED.-MAY 10,1970 COMPLETED..MAY 13,1970 MIDWEST DRILLING AXT ALL CASING PULLED

CLAIM K 256942 450 FT S t 400 FT E OF POST 4* ********* ********************* *************** »»***_******»***»**»***»»»***»»»«»»••»* SAMPLE ENTRIES --.--• -_——.-.

DESCRIPTION ANG COLLAROB SAND t CLAYGY FG IMP FOTN DISTORTED LOC CHTY

F£W OTZ VINS STRS C SPKS PY PO FEW _._._. ._._ .

MTSD GR TO BRWN FG HLY ALTD FOTD 40 OTZ 40 6IOT AMPB LOC HLY SLCS OCC OTZ STR LOC GARS LOC APPEARS VPLC FEW SPKS PY

AND GR FG WELL FOTD 40 OCC QTZ OR CARB. _ _40__ _.„...._ .STR LOC FEW GA3S FEW SPKS PY

OTE IMP GY FG TO VFG WELL FOTO C LOC 40 WELL BNDD 40 LOC BNOS BIOT OR AMPB OCC OTZ OR CARS STR LOC SPRS PY

227.0 10.5 MTSD GY FG FOTD 40 MORE IMPS THAN ABOVE 40SGNS BIOT ELONG PARALLEL FQTN STRS__ ____ _ __CHLR AMPP SPKLO WITH CARB OCC OTZ STR FEW SPKS PY

232.0 5.0 MVYW MTSD FEW SPKS PY 235.8 3.« MVW MTSD SPKS PY PO 4X PY PO 237.5 1.7 MW MTSD MO»E IMPS ALMOST CHLR-BIOT-OTZ SCH

STRS PO WITH BL8S PY 25X PO PY_ 4.5 MVW MTSD STRS C SPKS PO PY 9X PO PY

MTSD SPKS PO PY 5X PO PY CT SHARP 40

92.0 69.2

113.2 21.2

216.5 103.3

242.0246.9254.0

6.9 MVW5.1 MVVW OTE LT GY FG MASS LITTLE BIOT OR AMPB

IMPS SPKLD WITH CARB293.0341.0

342.9

363.8388.2

401.5

39.048.0

1.9

20.924.4

13.3

OTEOTE IMP BRWN TO GR ? G W ELL FOTD C WK.LY

BNOD 45 BIOT t CHLR-AMPB IMPS LOC BIOT SGNS ELONG PARALLEL FOTN LOC SPKLD WITH CARB FEW OTZ STRS FEW SPKS PY

PRPH FELD-OTZ WH MASS OTZ e WH FELD PHCRFEW SPKS PY

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AMPB IMPS AGLM GR CG FOTD 4O CO FLSC FRGS IN SCHD

4545

40

BQPFJHOtEf >2739-Hp OINORWIC PAGF«

DEPTH LENGTH HNZN ROCK DESCRIPTIONBIOT-4MPB MTX

402.9 1.4 DYKE INT COMP G« FG MASS FEW SPKS PY 419.8 16.9 AGL* AS TO 401.5 426.8 7.0 HVW PRPM FEIO IT GY MG MASS NOM HG HH FELD

PHCR IN MAINLY FELO MTX OTZ STRSSPKS MFCS SPKS PY PO RARE CP SPH 3%PY PO

430.0 3.2 HVVW PRPH FEW SPKS PY FOOT OF HOLE

ANG

APPENDIX "A"

McCOMBE MINING AND EXPLORATION. LIMITED

DIAMOND DRILL RECORD

LOCATION; 229' N.55 W. of 0/00 DRILL HOLE No. 1

BEARING: S.55 D. DRILLING DATE; November 1950

DIP: 45C DEPTH: 499

Depth feet Formation Sample No.

Width of Sample

Gold oz.

0-21 21-57

57-0-61.4 61.4-65.0

65-0-98.098.0-114.3114.3-141,0141.0-149.7 149.7-175.8 175-8-182.4 ?82.4-195.0 195-0-200.1 200.1-201.7

201.7204.8

-204.8 205.2

205.2-206.2

206.2- 343.6-

361.9- 366.6- 388.0-

34 3.. 6361.9

366.6388.0395.1

395.1-442.9442.9-454.9 454.9-499

499

CasingAgglomerate, scattered fine pyrlte & some barren quartz stringers. Flow altered andesite.Tuff. F. C. Diorlte Agglomerate chloritized andesiteTuff. F. C. Diorlte Feldspar porphyry. Diorlte Rhyolite porphyry Coarse grained tuff Variegated feldspar porpyry Rhyolite porphyry Coarse grained tuff Rhyolite porphyry (gray) Quartz vein, pyrite, chal- copyri';u, galena & sphale riteChlorite schist Quartz vein, galena, chal- copyrite, pyrite Chlorite schist, some quartz stringers with sparse pyrite Andesite, vesicular in places Feldspar porphyry. Diorlte porphyryAndesite vesicular Silicified andesite Fine grained quartZ'-porphyry, some fine disseminated pyrite Rhyolite 388-392 Andesite. Schisted Feldspar porphyry Variegated andesite END OF HOLE

Angle at 250' - 33 Angle at 499' - 23 (approx).

222

223

224

1.6

1.0

0.34

1.12

Tr.

225 4.0 Nil

- 8 -

APPENDIX "A"

McCOMBE MINING AND EXPLORATION LIMITED

DIAMOND DRILL RECORD

LOCATION: 131' S.55 E. of 0/00 DRILL HOLE NO.

BEARING:

DIP:

N.55 W.

45

DRILLING DATEt November, 1950

DEPTH: 248'

Depth feet Formation Sample No.

Width of Sample

Gold oz.

0-1616-16.716.7-17.017.0-13.118.1-62.362.3-63.3 63.3-178.6178.6-179.7 179-7-211.5 211.5-213.0

213.0-248 248

CasingAndeslteQuartz porphyryAndesiteQuartz porphyryLost coreAmygdaloidal andesiteLost coreAmygdaloidal andesiteChlorite schist with50$ quartz sparsepyriteAmygdaloidal andesiteEND OF HOLE

Angle at 248' - 4l

226 1.5 Nil

--'9 -

APPENDIX "A"

McCOMBE MINING ANI; EXPLORATION, LIMITED

DIAMOND DRILL RECORD

LOCATION; 140' No. 55 W. of 2/00.W.

BEARING; S.55 E.

DIP: 45

DRILL HOLE No.

DRILLING DATE: November 1950

DEPTH: 260°

pepth feet

0-1212-19.019.0-28.528.5-32.032.0-32.332.3-38.038.0-66.666.6-91.991.9-117.0

117.0-133.*113.4-161.4161.4-163.4163.4-179.6179.6-186.1186.1-187.8

187.8-191.8

191.8-192.8

192.8-194.5

194.5-204.9204.9-?0<S.6205.6--. ;.6206.6-&V. -;.2209.2-233.0

233.0-253-6

253-8-260260

Formation Sample Width of No. Sample

CasingAndesiteFeldspar porphyryFine grained quartz porphyryFeldspar porphyryFine grained quartz porphyryPorphyritized andesiteFeldspar porpyryAndesite, porphyritized inplacesAmydaloidal andesiteBasalt feldspar porphyryAndesiteBasalt feldspar porphyryAndesiteChlorite schist, silicified, 227 1.7sparse pyriteQuartz, sparsely mineralized i:28 4.0with galena, sphalerite,chalcopyrite & pyriteQuartz, heavily mineralized 229 1.0as aboveChlorite schist, silicified, 230 1.7sparse min.AndesiteQuartz, a little pyrite 231 0.7AndesiteQuartz, a little pyrite 232 2.6Amygdaloidal andesite, plainandesiteFeldspar porphyry, dioriteporphyryAmygdaloidal andesiteEND OF HOLE

Gold oz

Nil

Trace

0.44

Trace

Nil

0.04

Angle at 260' - 40

- 10 -

L. P. OAUVREAU, B ,A, So.,

Minine Engineer

Suite 310,6? Yonge Street,

TORONTO, Canada.

CERTIFICATE

I, LEVI FRANCIS OAUVREAU, of the Town of Alliston, in the County of Simcoe, hereby certifys-

1.

2.

3.

That I am a Professional Engineer, and reside at 112 Victoria Street East, Alliston, Ontario.

That I am a graduate of the University of Toronto, 1933. in Mining Engineering, and that I have prac tised my profession since graduation.

That I have no direct or indirect interest whatso ever in the mining claims the subject of this report, nor have I any direct or indirect interest in the securities of the Company, nor do I expect to receive any direct or indirect interest in the securities or property of the Company.

That the accompanying report is based on a report by B. M. Arnott, dated April 10th, 1952, from Government reports by Dr. Hurst in 1932 and E.O. ChidToljn in 1951, from a detailed geological explor ation program on the claims performed by the Company during July and August 1952, and from personal experience in the immediate area during the fall of 1950.

DATED this nineteenth day of May, 1953.

"L. F. Qauvreau"

Registered Professional Engineer

Mining

L. F. Qauvreau

Province of Ontario.

- 12 -

GROUP "B" MINING CLAIMS

REPORT

ON

GORDON CLAIMS

Echo Township

pi'Btrict of Kenora, Ontario

Dated at:- Toronto, Ontario May 18th, 1953

Report made for:-McCombe Mining & Exploration Ltd.,330 University Avenue, Toronto

SUMMARY AND CONCLUSIONS

1. The area in which the claims are located is favourable for the occurrence of' g61d-bearing sills of grano-diorite and therefore these claims have good chances to respond to exploration.

2. Due to excessive overburden regular prospecting is not performable. As geophysical surveys on neighbouring properties proved inconclusive in tracing the granodiorite, cross-section diamond drilling is therefore the only feasible method for preliminary exploration.

3. Definitely these claims should be brought to a patent. Therefore, the logical course to follow would be to lay out a cross- section and drill along it year after year for assessment work and also for geological information.

4. This assessment work might very likely lead to the intersection of a favourable zone along which intensive diamond drilling could be carried out.

RECOMMENDATIONS

It is hereby recommended that the claims be kept in good standing. To comply with this year's assessment work 360 feet of "EX" diamond drilling should be carried on*-.

A sum of $1400.00 should cover the cost of this work.

SCOPt: REPORT

This report is based on a report by B. M. Arnott, dated April 13th, 1952, from Government Reports by Dr. Hurst in 1932 and E.O. Chlsholm in 1951, from a diamond drill log by Robert McCombe in the summer of 1952, and from personal experience in the immediate area during the fall of 1950.

LOCATION AND EXTENT OF THK PROPERTY

The property is located in lots 3, 4 and 5, Concession III, Echo Township, Patricia Mining Division, District of Kenora, Ontario. Consisting of 9 unpatented mining claims bearing Claim Nos. KRL 30939 to KRL 30947, inclusive, the group comprises approximately 360 acres. Newlund Mines adjoins on the south boundary of KRL 30939 & 309^2 and East Lund Mines adjoins to the south and west.

" ' ''"" 1 ' '''- '<••'•'. ' ' • >' ' - - ' " ' ' ,. ' « ' '

COKD

,T.Li!'J J.''.L. Vll-.^I^^T. : Logging operations have been carried out in the.- area w7nY17fVe~5e"n ir"ye"arK with the result that there is no commerc lo 1 t. iruhe r left on the claims.

1 HI; onJ.y water on t,h^ claims As 9 small "pot-hole" lake in an undra ! tif.-'l area near 1 ho west boundary. However, a good supply of v;ater c;m be obtained from Franciscan Lake, which is locaved 3/J* f a mile you t. lie, -if, i. of the south boundary.

T.P.IL9 Rift. l-lllZ J* H j. T r a n a P r * a t.- ion. - The underlying rock isheavily h..i!'j."ed by a' layer of sand and bouldera. Most of the surface is level or gently rolling and there are no outstanding topographic features.

Provincial highway No. J 2 1 lot; about l£ miles to the southeast of the claims. Lumber roads direct from thehighway make the property ear-lly accessible. Sioux Lookout; ir. about 23 miles av.'ay to the northeast.

GEOLOGY

and perti heroin:- adjacent, heavy man exposures that the rocko gor. although steep 1,;; f.

Mr. B.M.Arm;tt, in his report; very ably covers the important nent, features of the local geology and the writer quotes him(Quo th

or.:! or '

) "With the exception of a small area of basic lavas e so'.ith-west corner post the claims are covered by a very f Band, gravel and boulder clay. However, from rock >:lr.i 11 results on adjoining properties it is possible to Infer

no 1 pal rock types are Intermediate to basic lavas. These U;/ strike in a direction approximately N.70 degrees E. , r-: are local deviations. The dips are either vertical or

The main interest centres on the recent developments on the adjoining property of Newlu.nd Mines, where underground work is in progress. At this property the ore bodies occur as quart?, stringers and accompanying zones of alteration in granodiorite and, of less importance, in quartz- feldspar porphyry, and a number of showings have been discovered and tested. These intruslves occur as sills, having been intruded along the strike and dip of the lavas. Work on the Newlund and adjoining properties has s-shown the granodlorltc sills to be very persistent on strike, and v.lthin the sill concentrations of the gold bearings quartz strlr.gorc occur as shoots or lenses. The gold Is concentrated in, or irTimediate.lv adjoining, the quartz stringers which lie normal to the strike of the ;; !i. Therefore, it has been found by experience that preliminary drilling should bo done normal to the strike of the formation, and that, subsequent, hole? .should be drilled to tho sill at an angle so as to also cut the crops 1'ractur'es with which the mineralisation is associated .

e pi ejected strike utheast, corner of

of t,he several ore zones on Newlund .he- Gordon group and, therefore, thecrosses ihc

two soul her.! y claims, KRL 30939 -ind 309^(2 are of the greatest potential interest,. However, since the intervening rock Is obscured by overburden it is not known .If the strike remains uniform. Also there is no reasonwhy parallel Jo m 1. ghv. not be expected to occur (Unquote)

DIAMOND

dri 1.1 ing war, hole wa,'=i dr I ?00 feet no-' reached a^i.e type i:« a nor

iu '.!> , August of 193? three hundred and sixty feet of EXT core c. r>n>[> '!etv. d for information and assessment work purposes. The .'ed on a bearing of N-40-W, dip 45 degrees and was collared hwest, of t!u No." 2 F o.st of Claim KRL 30939. Bedrock was casJnp. 103 feet through wand and gravel. The main rock

'}'.. ̂ , S everal intc-roect/.iona were cut of sheared feldspar- . r>rv are peveral very narrc>w int,e7'f.ecti.ons of unmineralized

quartz. The log of the core ie appended hereto.

Respectfully submitted,

"L. P. Oauvreau"

L.F. Qauvreau, B./.. So., Professional Engineer.

Seal of Registered Professional Engineer

MiningL. F. Gauvreau Province of Ontario.

APPENDIX "A"

McC.QMBB MINING AND EXPLORATION , LIMITED

QROUP "B", DIAMOND DRILL RECORD

LOCATION: 200 ft. N.W. No.2Poat, claim KRL 30939

BEARING: N-40-W

DIP! 45 degrees

DRILL HOLE: No. 1

DATE:

DEPTH:

Aug 2-12/52

360 feet.

Depth Ft. Formation

p. 0-303.0103.0-172.3172.3-17 1*.!174.1-174.7174.7-178.8178.8-181.8181.8-184.9184.9-188.0188.0-194.2194.2-197.3197.3-198.8198.8-222.3222.3-230.5230.5-2^3.0243.0-276.5276.5-280.5280-5-281.2281.2-283.9283.9-284.4284.4-295.0295.0-295.7295-7-298.6298.6-299.5299.5-303.0303.0-310.0310.0-360.0

Casing - sand and gravelAndesiteSlightly sheared fine grained granodioriteAndesiteSheared acid intrusive (grandiorite)AndesiteSheared acid intrusiveAndesiteSheared acid intrusiveAndesiteLost coreAndesiteTuffAltered acid intrusiveAndesiteSheared acid intrusiveQuartz, (approximately 20 deg to core)Sheared acid intrusiveQuartz (approximately 80 deg to core)Sheared acid intrusiveQuartz (approximately 20 deg to core)Sheared acid intrusiveBasic flioriteGreenstone schistAcid schist (sheared acid intrusive)Andesite

END OF HOLE

DRILLING:- Performed by Pelican Drilling Company.

- 16 -

L. P. OAUVREAU, B.A., So.,

Mining Engineer

Suite 310,67 Yonge Street,

TORONTO, Canada.

CERTIFICATE

I, LEVI FRANCIS OAUVREAU, of the Town of Alliston, in the County of Simcoe, hereby certify:-

1. That I am a Professional Engineer, and reside at 112 Victoria Street East, Alliaton, Ontario,

2. That I am a graduate of the University of Toronto, 1933, in Mining Engineering, and that I have prac tised my profession since; graduation.

3. That I have no direct or indirect interest whatsoever in the mining claims the subject of this report, nor have I any direct or indirect interest in the secur ities of the Company, nor do I expect to receive any direct or indirect interest in the securities or property of the Company.

4. That the accompanying report is based on a reportby B. M. Arnott, datc-d"April 13th, 1952, from Govern ment reports by Dr. Hurst in 1932 and E.O Chibholm.in 1951, from a diamond drill log by Robert McCombe in the summer of 1952, and from personal experience in the area during the fall of 1950.

DATED this eighteenth day of May, 1953.

"L. F. Gauvreau"

Registered Professional EngineerMining

Province of Ontario.

- 17 -

Report on the Property of McCombeMining and Exploration Limited

Long Township, Sault Ste. Marie Mining DiviBion Province of Ontario

INTRODUCTION

That area along the shore of the North Channel of Georgian Bay

including the townships of Striker, Lonj, Spragge, Lewis and Sheddon is of

interest at the present time becaune of the reported presence of a uranium

bearing deposit of considerable size. This deposit is situated in the south

nentral part of Long township. McCombe Mining and Exploration Limited has

obtained a group of mining claims in the area. The claims were acquired

by staking.

PROPERTY

The property owned by McCombe Mining and Exploration Limited

consists of a compact group of eighteen unsurveyed and unpatented claims

numbered as follows:

SdM-24559, SSM-24560, SSM-24584 and SSM-24561 to

SSM-24575 inclusive.

The property is rectangular in shape and approximately one and

one-half miles by three-quarters of a mile in extent.

LOCATION, ACCESS, ETC.

The property includes the southwest eighth of Lot 4, the south

quarters of Lots 5 and 6, and the southeast eighth of Lot 7, Concession IV;

and the northwest quarter of Lot 4, the north half of Lots 5 and 6 and the

northeast quarter of Lot 7, Concession III of Long Township. The south

boundary of the property adjoins to the north the property of Peach Uranium

and Metal Mining Company Limned on which the reported uranium bearing

deposit occurs.

Paved highway No. 17, connecting the cities of audbury and

Sault ate. Marie passes some two miles to the south of the property. The

main line of the Canadian Pacific Railway roughly parallels this highway- 18 -

route. The town of Blind River, Ontario is situated on these transport

ation routes, oome eleven miles to the west. Hydro-electric power lines cross

the township In an east-west direction, a short distance north of the highway.

The area is lightly covered with timber consisting of both hard and soft woods.

TOPOGRAPHICAL FEATURES

The topography of the area is moderately rugged and marked by

extensive rock outcrops. Between the outcrop areas the terrain is generally

flat to gently rolling. Many lakes of varying size are scattered throughout

the region.

GEOLOGY OF THE PROPERTY

The property is situated within but close to the edge of a large

mass of pre-Huronian granite. This batholithic mass has intruded a series of

pre-Huronian sediments consisting mainly of interbedded quartzite and grey-

wacke which it contacts approximately one mile south of the property. The

Mississagi series of quartzite, conglomerate a^d argillite overlies these

formations. This series is locally flat lying or gently dipping to the south.

The main mass of these, sediments is known to approach to within one thousand

feet of the property. A study of geological plans of the area shows sedimen

tary remnants over considerable extent within the main granitic area. It

may well be that such remnant masses occur on the property. A mass of diabase

intrudes the east and north parts of the claim group.

It is believed that the area has not been mapped in detail and

as a consequence the location of geological contacts assumed at this time may

not be accurate.

ECONOMIC GEOLOGY

Uranium occurs in the area in the form of very finely dissemin

ated pitchblende and in the mineral brannerite. The latter occurs associated

with a sulphide bearing matrix in the quartx conglomerate rock series. This

series has been traced at intervals in an east-west direction for some twenty-

four miles. It is believed to be locally flat lying or having a slight dip

to the south. Approximately one mile to the south of the property of McCombe

Mining and Exploration Limited an extensive surface exposure of the radioactive

- 19 -

il^j.,^: ,,^Afct J ̂ ^w^ . tkrfj'teiW :;-, -

conglomerate formation has been investigated by diamond drilling and an

indicated tonnage in excess of 1,000,000 tons of material grading approximately

0.12$ U^OQ is reported. Additional discoveries have been made in the

sedimentary formations as far as eighteen miles to the north and fifteen miles

to the east of the Company's property.

EXTENT OF WORK DONE

The claim group was staked during the late spring of 1953> just

prior to the announcement of diamond drilling results in the area. Thus, no

examination of the, surface exposures on the property has been made and no

radioactive occurrences are known to be present on it at this time.

CONCLUSIONS

The .property is situated within a distance of one mile of the

most important uranium bearing deposit in area at this time. Several other

radioactive occurrences have been found in the short time since active interest

has been taken in the district. The area is readily accessible. The cost of

a program of surface investigation of the property should be relatively low in

comparison to that of the majority of areas where the search for uranium

deposits is being carried out at this time. It is believed that the costs of

mining in this area would also be relatively low, consequently deposits of low

grade material would hold considerable attraction.

RECOMMENDATIONS

It is recommended that a surface examination of the property

be carried out. A system of picket lines should be cut at intervals of no

more than 300 feet along which marked pickets should be planed at measured

intervals of 100 feet. This should be followed by a program of geological

mapping giving special attention to any occurrences of sediments and, in

particular conglomerates. A detailed geiger counter or scintillometer

survey should accompany the program of geological mapping over the entire

property. The field work should be conducted under the supervision of an

engineer or geologist with previous experience in the search for uranium

bearing deposits.

Any radioactive occurrences found on the property should be

further exposed by stripping and rock trenching in preparation for sampling.

- 20 -

REFERENCES

Map entitled Blind River, Algoma District, Canada,

Department of Mines, Geological Survey, issued 1925

(scale 1" equals 2 miles).

Respectfully submitted,

"Frederick C. Knight"

Frederick C.Knight, B.Sc., P.Eng, Mining Engineer.

June 29, 1953-

- 21 -

r' CERTIFICATE

I Frederick C. ^night, cf the City of Toronto, In the

of Ontario, hereby certify as 'ollows : -

1. That I am a practising Mining Engineer, with offices at Suite 1405 - 330 Bay Street, Toronto, Ontario.

2. That I am a graduate of Quoen's University, Kingston, Ontario, hold the degree of B.Sc. In Mining, and am a member of the Association of Professional Engineers of the Province of Ontario.

3. That I have no interest either directly or indirectly and do not expect to receive any interest either directly or indirectly in the property covered in this report, nor in the securities of McCombe Mining and Exploration Limited.

4. That the accompanying report is not based on a personal examination of the property since its acquisition by McCombe Mining and Exploration Limited, but in part on a geological map of th^ area published by the Department of Mines, Ottawa, in 3925j which reference is incorporated in the report; and on general Knowledge based on personal oxaminations of certain radioactive deposits in the area in July and August, 1949, Including the large tonnage deposit less than one mile to the south of the company's property,

5. This certificate applies to McCombe Mining and Exploration Limited claims numbered SSM-2'1559, SSM-24560, SSM-24584 and SSM-24561 to SSM-24575 inclusive, all located in Long Township in the Sault Ste. Marie Mining Division in the Province of Ontario.

DATED this 29th day of June, A.D. 1953-

"Frederick C. Knight"

Frederick C. Knight, B.Sc., P.Eng.Mining Engineer.

- 22 -

INTRODUCTION

The company owns two groups of mineral claims in the County of

Restigouche on the Province of New Brunswick. These are situated on the

southeast Upsalquitch watershed, an area some thirty-five miles to the

northwest of the base metal area in the vicinity of the Town of Bathurst

and some forty mtJes southwest of the Town of Dalhousie.

The- area IB of some interest at this time because geological

and structural conditions are believed favourable to the occurrence of

base metal deposits.

A mantle of onow prevents a personal examination of the properties

at this time. Thus the report is based on a study of geological reports

and maps of the area, aerial photograohs and on discussions with the

company's technical staff.

PROPERTIES AND LOCATIONS

Both properties are located in the Parish of Balmoral in the

County if Restigouche, more particularly described as follows :-

Claim Group I. consists of twenty claims numbered 1823-1 to 1823-20

Inclusive, comprising an estimated 800 acres more or leus. The property is

situated on the south branch of Meadowbrook Creek. Its east boundary is

located approximately one and one quarter miles west of Meadow Lfkes.

Claim Group IT. consists of twenty-one claims of approximately 40

acres each. The claims are numbered 1823-21 to 1823-^1 inclusive. The

northeast corner of the property is located approximately one-half mile

west of Rarnsey Sheds at the Junction of Ramsey Brook and the Southeast

Upoa ] qu.l ten Rl ver.

All mineral claims in both Groups I and II were acquired by the

Company by staking. They are unsurveyed and unpatented and have been

registered ir. the name of McCombe Mining & Exploration Limited, with the

&i!^Jfci£.i^

Department of Mines, FrederJcto;, Now Brunnwlck.

ACCESS, ETC.

Both properties are accessible by road from thu Town of Dalhousie,

such roaos passing through Group J and through the central portion of

Group 11. The roads are owned by the International Paper Company (New

Brunswick) Limited. These are gravel surfaced and quite suitable for

truck trave1.

The area is well timbered, with spruce and to a lesser extent with

balsam and pine. Timber rights are held by the International Paper Company,

(New Brunswick) Limited. A good supply of water for development and

initial mining needs is available to both properties fiom nearby creeks.

Electric powi.r is present forty miles dlstart on the Bai du Chaleur.

The area is one of moderabely rugged relief, containing deep

valleys and high steep hills. The principal topographical feature of the

area is the deep valley marking the te&dow Brook regional fault which passes

through Group I.

GENERAL GEOLOGY

The area is underlain by rocks of the Lower Devonian Series of

Paleozoic Age. These comprise sedimentary and volcanic formations, the

former includ'ng prliclpally shales and limestones and the latter, andesite,

related pyroclastics, and to a lesser extent, rhyolites. In many places

the volcanics and sediments are interbedded. Monzonite float found along

the stream beds Indicate that such intrusives may be present in the area.

The lavas, including the andesltes and rhyolites are hard and

brittle. Should any base metal deposits be present it is expected that they

would occur at places where such rocks have been fractured and broken up.

STRUCTURAL FEATURES

The principal structural feature in the area is the Meadow Brook

regional fault. It has been traced for a distance of some forty miles

and Is considered one of the longest faults in the province. Group I

straddles this structure for a distance of one and one half miles.

Secondary faults paralleling the main structure are indicated

by the presence of other topographical depressions. A third set of local

'faults follow steep to vertical escarpments which strike at high angles to

the strike of the Meadow Brook structure.

MAGNETIC ANOMALIES

There is reason to believe that magnetic anomalies are present

adjacent to the trace of the Meadow Brook fault, while others roughly

parallel the fault pome distance away. One such anomaly of the latter

type is believed to pass through Claim Group II.

ECONOMIC GEOLOGY

No mineral showings are known to be present on either of the

company's claim groups. The recent discovery of deposits of copper and

zinc sulphide in very substantial amounts adjacent to magnetic iron form

ations, some forty miles to the southeast has lead to the present interest

in the Southeast Upsalquitch area where similar conditions are believed

to exist.

SUMMARY AND CONCLUSIONS

A regional fault which has been traced for a distance of some

forty miles is known to pass through Group I. It is considered that the

possible presence of magnetic anomalies adjacent to this structure presents

a favourable condition for the deposition of budies of sulphide ores

The presence of a strong magnetic anomaly, believed to traverse

Group II, presents geological condition which warrants a thorough

Investigation.

RECOMMENDATIONS

While detailed Information re. the local geology of the area

which includes the company's two groups of mineral c-aaims is vague, certain

conditions as outlined above have been observed which are considered

favourable to ore deposition. Therefore, detailed surface investigations

of both properties appear warranted.

The investigations of both Groups, I and II, should include

detailed geological mapping and prospecting. Some form of geophysical

ground survey including magnetic methods should be considered in conjunction

with the geological mapping program in order to check the location of

magnetic anomalies referred to above.

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Total No. of Claims: 32 Tctal No. of days filed: G40

January 7, 1971

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RKEtPT No.MINING DIVISION

Supplemantary List 'B'

AXT d.d. hole 42739, located on Cl. X 256942, Angle -50 E, 430 ft. - 4 30 daysAXT d.d. hole 42740, located on Ci. X 256942, Ang.\e -50 C W, 378 ft. = 378 days

Total work available - 809 daysWork recorded as per Supplerventary List 'A* - 600 days

Credits to remain en K 256942 for possible future filing - 168 dayo

Drilling dates for the above tvo

BH 42739T May 10-13, 1970 BH 42740: May 14-16, 1970

by: Midwect Die-raer.d Drilling Limited Winnipeg, Manitoba

January 7, 1971

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