3ioi5swaee3 a.2683 SNOWDON 010

fSUMMARY REPORT ON SURFACE SAMPLING OF RADIOACTIVE ANOMALIES ON THE VALENTINIIRANIUM PROSPECT, SNOWDON TWP., HALIBURTON co., SE. ONT. BY ALBERT HOPKINS, GEOLOGIST

INTRODUCTION

Radioactive granite pegmatites were discovered in Snowdon twp. by

prospector Fleming of Minden, Ont. in 1968. As a result, Miro Mines Ltd. of Toronto

acquired and ground-surveyed radiometrically 32 mining claims south of Fleming's

discovery group. Miro Mines' geophysicist, A.B. Fleming (no relation to the

prospector) reported 13 radioactive anomalies (Nos. A to M inclusive) which occur

on the present block of 10 out of Miro's original 32 claims. Mr. FLeming

recommended that these anomalies be sampled properly, and if warranted, be

diamond drilled. Miro Mines Ltd., to the best of our research and knowledge, never

did sample these anomalies, Miro subsequently lost its charter, and all the claims

lapsed and reverted to the Crown. The lack of interest in uranium at that time was

due to very low world prices, and to an embargo on U.S. imports.

Since then the U.S.A. has removed its embargo on uranium imports, and the

world price of urania has climbed from about $6 to $40 a pound. So the writer

(and his associate, John Haahti) restaked the 10 anomalous mining claims containing

these 13 radioactive anomalies for Mr. E.P. Valentini, who gave the writer a

contract to relocate and properly sample the best parts of the 13 anomalies. An

application was made by the writer for an M.E.A.P. (Ont. Gov't Mineral Exploration

Assistance Program) contract, as Snowdon twp. is in one of its designated areas.

A contract was subsequently granted and signed.

PROPERTY

This consists of the mineral rights on 10 contiguous mining claims, Nos.

EO.502199 - 502208 inclusive, comprising an area of about 475 acres. These claims

were recorded on 19 May 1977.

LOCATION NTS. ref. 31.D.15

The property comprises all or parts of Lots 16 - 21

inclusive, Concession VI, in the central SE. 1/4 of Snowdon twp. in the Bancroft-

Haliburton "U" belt of SE. Ontario. The property is l mile N. of Bow lake, 3 mi. W.

of Irondale hamlet, 3 mi. SE. of Gelert hamlet, 6 airmiles NE. of Kinmount village,

8 airmiles SE. of Minden town, and 12 airmiles SW. of Haliburton town, in Haliburton

county, SE. Ontario. This is about 70 airmiles due N. of Eldorado Nuclear's "U"

refinery at Port Hope, and 90 airmiles NE. of Toronto, Ontario.

ACCESS

From Toronto it is about a 125-mile drive to the property, taking no more than

2 1/2 hours, via superhighway 401 E. to Newcastle, and thence N. on No. 35 to Fenlon

Falls, and thence on No. 121 NE. to Kinmount, and E. on No. 503 to Irondale, and

finally 3 miles NW. on a county gravel road that joins Irondale and Gelert hamlets,

the latter on Highway No. 519.

In 1968 there was no road through this Miro property, but now there is a new

bush road along the N. boundary of the property and S. into its W. section, as well

as a new winter or skidoo access road going S. to Bow lake along the E. boundary of

the 10 claims. There is a 3rd old bush road trending W. along and near the S.

boundary of the 10 claims from a farmhouse on the Gelert-Irondale county gravel road.

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LOCAL GEOLOGY

The host rocks of the radioactive deposits of the Haliburton-Bancrof t

area are all of Precambrian age. There are two main groups of rocks present in the

area:- the Grenville-type metasediments, mainly marble, paragneiss and skarn; and

the later Archaen plutonic rocks, mainly granite, syenite, and gabbro, together

with their gneissic and hybrid equivalents.

The Valentini property is underlain by Glamorgan granite gneisses and pegmatites.

ECONOMIC GEOLOGY

To date all U production from the Bancroft area of SE. Ontario has

come from the pegmatites. However, on at least one of the properties optioned by

Imperial Oil Ltd. (that of Mandarin Mines Ltd. in Adjoining Glamorgan twp.), the

host rocks are large low-grade skarn or marble formations.

PREVIOUS WORK DONE

As mentioned in the above Introduction, the only work done on

this Valentini property prior to this systemmatic sampling by the writer, was the

radiometric survey performed by A. B. Fleming. His grid of 1968 picket lines has

disappeared, except for half a dozen widely dispersed unreadable lath pickets.

Therefore Fleming's anomalies had to be relocated by scintillometer.

There was no evidence of any sampling of outcrops, blasting or diamond drilling

on this 10-claim property, prior to the writer's presently-described sampling.

CURRENT SAMPLING PROGRAM

As the FLeming picket-line grid was unrecognizable to the

writer, the radiometric anomalies had to be relocated by pace and compass measure

ments from geographical landmarks, and the use of a scintillometer. This re-search

was made more difficult by a series of new ponds, swamps and flooded areas caused

by many new beaver dams and a very wet spring season, which created new landmarks

and obliterated old ones. However, all anomalous areas "A" to"M" were relocated except

for anomaly "I".

It is common knowledge that uranium oxide (urania) is very soluble in surface

solutions, especially if acidic, and the U is usually leached considerably from the

bedrock. surf ace to a variable depth, depending on the depth of the water table, the

porosity of the bedrock, structural and fracture patterns in the bedrock, the Ph

of the groundwater, and the type of rock formation.

On this property the radioactive areas are mainly underlain by fresh-looking

massive granite pegmatite dykes and plugs, with a minimum of shearing and fracturing.

Therefore it was concluded by the writer that fresh unleached representative rock

samples could be obtained from a depth of one foot or more below the smooth, hard

glaciated granite pegmatite bedrock surface.

Fleming's survey was performed with readings every 50 feet on a grid with

200' picket-line intervals, using a McPhar TV-3 scintillometer. This instrument was

carried at hip-level, and read the sum of U 4- Th gamma radiation in c. p. m. (counts

per minute). The writer used an Exploranium Corp. of Canada gamma ray scintillometer

model GR-101A, which gives the total U -t- Th radiation in c. p. s. (counts per second).

The intensity of a scintillometer ' s gamma readings depends on the radioactivity

of the bedrock, its distance from the target, the mass effect, the area of its

sodium iodide crystal, its high-gain photomultiplier tube, etc. Therefore it is

almost impossible to relate the readings of one survey to those of another, except

as their function of the local background radiation counts. The writer obtained an

-3-

backgrount count of 5 c. p. s with his instrument in Toronto, and 10 c. p. s.

TI the deeply overburdened areas of the property (away from granite outcrops)

in Snowdon twp. Therefore the 10 c. p. s. reading was used as the BG. (background)

count for this survey. No reading taken at hip level over bedrock outcrop of less

than 30 X BG. was considered significant in the writer's work on this property.

Up to eleven of the highest readings in each anomalous area "A" to "M"

(except for "I" which could not be pin-pointed) were marked with red flagging and

red luminous paint and labelled in the field by the writer, as shown on the

attached maps, for a total of 61 locations to be drilled and blasted by the

contractor, and to be sampled by the writer. The contractor, Mr. Chas. Mortimer

of Washago, Ontario, subsequently drilled and blasted each of the marked bedrock

(or very shallow oberdened) sample locations to a minimum vertical depth of one

foot, so that fresh bedrock samples could later be obtained by the writer.

In due course these 61 fresh bedrock samples were broken and collected by

the writer, the average being over 5 pounds weight. The writer delivered the

samples in batches to the assay laboratory of the Mineral Research Branch of the

Ont. Ministry of Natural Resources at 77 Grenville St., Toronto, for their uranium

determinations .

ASSAY RESULTS

The detailed assay reports on these 61 samples are to be found in

the Appendix to this report. The very highest assay was No. C-l, which gave only

D.024% urania chemically, or 0.48 Ibs. urania per ton of rock. The next best

were 6 samples which assayed only Q.02% urania equivalent (U + Th combined)

radiometrically . Almost all the samples assayed the equivalent of only a trace

of urania. Remember that only the very highest parts of each anomaly were marked

for sampling a t all (by the writer).

Therefore no uranium ore was indicated by this sampling, and no diamond

drilling or further work or expense is warranted on this property.

SUMMARY S. CONCLUSIONS

1. This 10-claim property in Snowdon twp. contains 13 radioactive anomalies caused

by uraniferous granite pegmatites located by A. B. FLeming's scintillometer survey

performed in 1968.

2. These anomalies were relocated by the writer using another scintillometer, and

their 61 "hottest" spots were well marked and labelled by luminous paint and

red flagging.

3. These 61 locations were subsequently plugger-drilled and blasted to a vertical

depth of from l' to 2' by a contractor and his men.

4. The 61 blast-holes were then sampled by the writer, and assayed by the O.M.N.R.

5. None of the 61 fresh samples assayed high enough to make uranium ore. The very

highest chemical assay was Q.024% urania.

6. No further work or expenditures are warranted on this property.

RECOMMENDATIONS

It is recommended by the writer that:-

No further work or money be expended on this property in the search for uranium.

All of which is respectfully submitted,

r ,Toronto, Canada. ,-, ^ T7 ,- , , mo Albert Hopkins.February 1978.

Consulting Mining Geologist.

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t REFERENCES:-

\, Uranium i Thorium Deposits of S. Ontario by D.F. Hewitt, in O.D.M.'s Mineral Resources Circular No. 4, 1967.

2. ODM.'s prelim, geol. whiteprint map No. P.972, on U ft Th Deposits of Ontario (S. sheet) by J.A. Robertson, 1975.

3. Canadian Mines Handbook, 1976, pp. 58, 192, and 206.

4. ODM.'s coloured geol. map No. 1957b"Haliburton-Bancroft sheet", scale : l'^2 mi.

5. Ont. M.N.R. Forestry Airphoto No. 69-4436-41-92, scale l" - 1/4 mile.

6. Ont. M.N.R. Forestry Basemap No. 447783, scale l" = 1/4 mile.

7. Ont. Dept. Mines' Snowdon twp. whiteprint No. M.153. Scale l" = 1 /2 mile.

8. ODM.;s 65th Annual Report, part 6, 1956,"Radioactive Mineral Occurrences in the Bancroft Area", by J. Satterly, p. 7.

9. Canadian Deposits of U S. Th by A.H. Lang, G.S.C.'s Econ. Geol. Series #16, 1952,p.149.

10. Various articles on Imperial Oil Ltd., Kerr-Addison Mines Ltd., Madawaska Mines Ltd., etc. in "The Northern Miner newspaper of Toronto.

11. Summary Report on 10-claim U prospect in Snowdon twp. by A. Hopkins, dated l June 1977,

APPENDICES:- (Xerox copies)

1. Road Map of part of Southeastern Ontario, scale l" = 1 8 miles.

2. Prelim Map # P. 972 of ODM. showing U 6. Th Deposits of Ont. (S. Sheet) Bancroft Area.

3. ODM. map # 1957b "Haliburton-Bancroft Area, Ont." Scale : l" = 2 miles.

4. Can. Gov't's Topo. map, "Minden sheet", NTS. 31.D.15, Scale : l : 50,000.

5. ODM.'s Snowdon Twp. claim whiteprint, No. M.153, as of 19 May 1977 and Feb. 1978.

6. Ont. L. fi F .'s Basemap # 447783 showing Valentini property, Scale : l" = 1 /4 mile.

7. Thin Section Examination report on Valentini radioactive pegmatite from Snowdon tp. by Mineral Research Branch of Ont. Ministry of Natural Resources, 13 June 1977.

8. Lab. Reports on 61 U Assays on Samples from Valentini Property, Snowdon Twp., by Mineral Research Branch of Ont. Ministry of Natural Resources, Aug. - Sept. 1977.

9. Various Descriptions and detailed locations and sketches by A. Hopkins on the 61Blast-Hole Drilling, Blasting, and Sampling of Valentini property, Snowdon tp., Ont.

10. Schedule "A" showing breakdown of Contractor's workmen's Names, Addresses anddates and times worked on the Drilling and Blasting of 61 locations, Valentini claims.

11. Schedule "B" detailing the dates and hours spent by A. Hopkins on technical professional work on the Valentini property, and some of his expenses

12. Summary of A. Hopkins' Expenditures for M.E.A.P. purposes, also Ont. Mining Act Assessment Work calculations re man-days work claimed, and Assay Report expenses.

13. Large map enclosed:- "Composite Plan of Howpins' Uranium Property, Snowdon Twp., SE. Ontario" by A. Hopkins, July 1977, Scale : l" = 200'.

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PRELIMINARY MAP P. 972 MINERAL DEPOSITS SERIES\?J\ i-*Q

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^^^—•j^} " ^ /f DEPOSITS OF ONTARIO

^W Ja C//? SOUTHERN SHEETSOUTHERN ONTARIO AND

Map No. 1957b

HALIBURTON-BANCROFT AREAPROVINCE OF ONTARIO

Scale l: 126,720 or l Inch to 2 MilesJ 3 4 i b 7

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THE TOWNSHIP OF

3/-D-/5"

SNOWDONCOUNTY OF HALIBURTON

EASTERN ONTARIO MINING DIVISION

SCALE' 1-INCH *40 CHAINS

IX

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31D15SW0893 2 .2683 SNOWDON 020

Ontario

LABORATORY REPORT

MINISTRY OF NATURAL RESOURCES MINERAL RESEARCH BRANCH

77 GRENVILLE STREET, 11TH FLOORTORONTO 181, ONTARIO

TELEPHONE: 965-1337

REPORT NUMBER

C 18626

DATE .......June; .13th,. .1977

ISSUED TO: A. Hopkins. 810 Duplex Avenue. Toronto, Ontario

Thin Section Examination

No. l

Hand Specimen - coarse-grain pink granite.

Thin Section - Mineralogy QuartzPotassic feldspar Sodic feldspar Muscovite Hematite

Texture The rock is massive with coarse-grains of microcline, slightly sericitized albite and interstitial quartz.

Fine-grained hematite is interspersed through the rock and is responsible for its pink colour. Muscovite is present as a minor component,

Classification - Granite.

No. 2

Hand Specimen - medium-grained granite with considerable dark-green mafic material.

Fees Received

Thin Section _ Mineralogy quartz feldspar chlorite carbonite.

Texture - The rock is medium to fine-grained and massive. It contains much anhedral feldspar,twinned and sericitized. In addition, chlorite occurs in acicular pseudomorphs after hornblende.

Cont'd.5 Coups. Card #2788 Inv. # 2-7006

,. P ADIRECTOR

..)..

MS.003 Except by special permission, reproduction of these results must include any qualifying remarks made by this ministry with reference to any sample.

-2-

Research Branch Attach to Certificate No. C18626 Ministry of Natural Resources June 13th, 1977

Issued to: A. Hopkins, 810 Duplex Avenue, Toronto, Ontario——^———.^———————————

Quartz is found as coarse interstitial granules. Carbonate occurs in minute narrow seams.

Classification - Altered granite.

No. 3

Hand Specimen - Medium to coarse-grained granite with considerable mafic material.

Thin Section - Mineralogy quartz feldspar biotite hornblende chlorite apatite

Texture - The rock has a weakly schistose texture produced as a result of a rough parallel alignment of the biotite.

Hornblende occurs as dark-green pleochroic anhedral grains.Feldspar occurs both as albite and microcline an is relatively fresh in contrast to the sericitized variety in No. 2.Chlorite is present as a minor component forming alteration rims around the biotite. Euhedral apatite in minute crystals are sparsely disseminated throughout the rock.

Classification Granite.

Sample No. Radioactivity Uranium Oxide __________________________Equivalent————^—-.^——^^—

//l Q.008%

#2 Q.002%

#3 0.0012

Fees Received

5 Coups. Card. #2788 j \ ^^ -Inv. #2-7006 (D.A.Moddle, P. Eng.

Director

Ontario

LABORATORY REPORT

MINISTRY OF NATURAL RESOURCES MINERAL RESEARCH BRANCH

77 GRENVILLE STREET, 11TH FLOORTORONTO 181, ONTARIO

TELEPHONE: 965-1337

REPORT NUMBER

B 11828DATE ......Aufl...B,.J.977...

Albert Hopkins. 810 Duplex Ave.. Toronto. Ontario

SAMPLE NUMBERGOLD02.

PER TON

GOLDVALUE

PER TON

SILVEROZ.

PER TON

#1977-1 Trace{from Shoal Lake Synd. DD. Hole)

first batch of Assays from the Valcntini n property, Snowdon Tp

Total Radioactivity (Uranium Oxide Equivalent

Anomaly "M"#M-1 D.01%

M-2 0.007M-3 0.005M-4 0.008M-5 0.005M-6 0.02

M-7 0.01

Fees Received8 Coupons Card #2872

(p.A.Moddle.P.Eng.)DIRECTOR

MS.002 Except by special permission, reproduction of these results must include eny qualifying remarks made by this ministry with reference to any semple.

31.D.15/^~~^\ Ministryof Mineral^^1 Natural Research LvV Resources Branch Ontario

77 Grenville Street 11th Floor Toronto, Ontario M7A 1W3 Telephone 965- 1337

Laboratory Report

Report No.

C 18737Date

Aug. 17, 1977

Issued to:Albert Hopkins 810 Duplex Avenue Toronto, Ontario

Assays of T " S amples collected Ly A. HopJ'.ins from the Valentini AnonalJ Snovrdon Tv;p. f 7 July 1977.

Sample No.

D-lD-2D-3D-4D- 5D-6D-7D-8D- 9D-10

6-16-26-36-46-5

L-l1-21-3L-4L-5L-6L-7L-8L-9L-10

Fees Received

27 Coupons, Card

Radioactivity (Uranium Uranium Oxide Oxide Equivalent)^ (U30g) 1

0.0030.020.0050.010.010.0050.010.010.0080.007

0.0050.0030.0070.0040.006

0.0010.0050.007

0.010.0050.0070.0070.0070.010.02

#2872,2873,2874

Director

Except by special permission reproduction of these results must include any qualifying remarks made by this ministry with reference to any sample.2091

®Ontario

Issued to:

Ministry of Natural Resources

A. Hopkins,

Mineral Research Branch

810 Duplex

77 Grenville Street 11th Floor Toronto, Ontario M7A 1W3 Telephone 965-1 337

Avenue, Toronto,

Laboratory Report

Report No.

C 18805Date

77/9/19

Ontario

Sample No.

A-lA-2A- 3A-4A-5A- 6A- 7A-8A- 9AIDB-lB-2B-3C-lC-2C-3E-lE-2E- 3F-lF-2H-lH-2J-lJ-2K-lK- 2K-3L- 11

Fees Received35 Coups. Card No. 2873,2875

RadioactivityUranium OxideEquivalent Z

u.003%0.0080.010.0060.0020.0050.004-0.010.0040.005-0.006-0.020.0060.010.010.0060.020.020.0030.0040.0070.0020.0050.0060.0050.004

&2S76

S&raniumOxide(U3o8)

--

-----0.003---0.005-0.024--------------

Director

(D.A.Moddle, P. Eng.;Except by special permission reproduction of these results must include any qualifying remarks made by this ministry with reference to any sample.2091

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GEOPHYSICAL - GEOLOG TECHNICAL DAT.

31D15SWTO83 2 .2683 SNOWDON 300

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey.Sampling S Assaying, Sec. 86 (18), Ont. Mining Act.

Township or Area.Snowdon twp., M.153, Haliburton county.

Claim holder(s) A. Hopkins, Lic.# E.12440.(EO.502199-203)J. Haahti, Lie. # S.1812. (EO.502204-208).

Author of Report. Address———

Albert Hopkins, B.A.Se.

810 Duplex Av., TORONTO, Ont. M4R 1W7.

Covering Dates of Survey. l June 1977 to 3 Feb. 1978.

Total Miles of Line cut. nil(linecutting to office)

SPECIAL PROVISION CREDITS REQUESTE

ENTER 40 days {includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

per claim

—Electromagnetic.—Magnetometer———Radiometric——

—Other——.———

Geological.Geochemical.

AIRBQRNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer .Electromagnetic. . Radiometric

DATE:. 3 Feb. 1978.

(enter days per claim)

SIGNATURE:.Author of Report or Agent

PROJECTS SECTION Res. Geol. -————. Qualifications.Previous Surveys

Checked by. .date.

GEOLOGICAL BRANCH.

Approved by. .date.

GEOLOGICAL BRANCH.

Approved by. -date.

MINING CLAIMS TRAVERSED List numerically

EO.502199'^'02200"

""""'502201'(number)

502202

502203

502204

502205

502206

502207

502208

TOTAL CLAIMS /O

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.all ten claims Nos. EO.502199 - 502208 incl.

Total Number of Samples- Type of Sample.

61Bedrock

(Nature of Material)5 Ibs.Average Sample Weight

Method of Collection- after plugger drilling 6 blasting.

Geologist's hammer St moil,

Soil Horizon Sampled. Horizon Development. Sample Depth

i'-2' below rock surface

Terrain.Undulating outcrops of radioactive

granite pegmatites

Drainage Development———————————— Estimated Range of Overburden Thickness.

0-1'

SAMPLE PREPARATION(Includes crying, screening, crushing, ashing)

Mesh size of fractionH-ised for analysis.

ANALYTICAL METHODSValues expressed in: per cent

p. p. m. p.p. b.

OD

Cu, Pb, Zn, Ni, Co, Ag, Mo, As,-(circle)Uranium

Others .———^—————————^—.^^^—.^^^^Field Analysis

Extraction Methdd. Analytical Method- Reagents Used ———

.tests)

Field Laboratory AnalysisNo. ___________ .tests)Extraction Method. Analytical Method .

Reagents Used ——

Commercial Laboratory (,61

.tests)Name of Laboratory.

Extraction Method—

Analytical Method —v

Reagents \Jsed —^—

O.M.N.R., Toronto.

Raciometric 4Chemical.

GeneraL General.

\

\

THE TOWNSHIP OF

SNOWDCOUNTY OF HALIBURTON

EASTERN ONTARIO MINING DIVISION

SCALE' 1-INCH =40 CHAINS

LEGEND

PATENTED LAND CROWN LAND SALE LEASES fc LOCATED LAND LICENSE OF OCCUPATION MINING RIGHTS ONLY

SURFACE RIGHTS ONLYitoAoeIMPROVED ROADS KING'S HIGHWAYS RAILWAYS PJ?WEK LINES MARSH "OR MUSKEG MINESCANCELLED TRAILS '

C.S.

c.

NOTES

This Mop Is Not To Be Used SURVEY PURPOSES

V!

Lot And "'Corifcewon Lines Shown Hereon Are Projected From The Best Information Available

#But Their True Position Is Not Guaranteed.#For Official S uryey Purposes Consult The , tffigmal Survey frans And Field Notes OfRecord ;ln The Oept.* Of Lands 8. Formats,

4pO v , Surface Rights Reservation Around M LAke* And Rivers.

'' The Acreages Shown Are The Amount That We/e Patented And Do Not Necessarily

f Represent The True Surveyed A/ea Of The Parcel.

DATE OE ISSUE

MAY 171978

SURVEYS AND MAPPING ^ JHjATO——

r

PLAN NO.- M. 153

3ioiss#eeo3 s.aees SNOWDON 200

Minden Twp. ( M.I633)I2 13 14

16, 17 18 ,I9 20 21 22 23 24 25 26 27 28 29 30 31 32 3389 10 II Lake Canning

2 3 4 5 6.7

Conning 15

lOOoc© 32

-,—si

ml 100 ac (g) 13

Rf 99 ac.© B

469642 469641 169634 469613 469668 469687 ^

. HOWLAND I00\ac.(g) l 5 1 469679 4696781 j.

50397^ ^0^3752 503753 503794

503976 503973503979 503980

12 13 K/ 15 16 17 18 l 22 23 24 25 26 27 28 29 30 31

Galway Twp.( M. 94)

3! -O- 15 COMPOSITE PLAN

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