31D16SW8064 63A.298 ANSTRUTHER 010

TECHNICAL REPORT

GARLAND MINING AND DEVELOPMENT CO,

Anstruther Township Property Peterborough County, Ont*

(A.E.C.B. Exploration Permit: MX 93/55) (Ontario Mining Licensei A-29082)

-by-

"

L.Oermain,P,Eng,

REPORT No, M - 8g

DATEt- November 30th t 1955

E IX BOULEVARD TE-. RAYMOND 2-3771

Heonarfc Germain,/XA.. A R C. S

CONSULTING ENGINEER

MINING A CHEMICAL

MEMBER OF THE CORPORATION OF PROFESSIONAL ENGINEERS OF QUCBfC

MEMBER OF THE C l. M. M. AND A A. A. S.

Montreal, Novenfcer 30th,

8U MM A R T

Th* property, consisting of 27 raining claims located In

Anstruther township, Peterborough County, Ont., was purchased out

right last winter aa a piece of virgin mining land* It was saleo-

tod on account of the possibility that It night Ile along the south

western extension of the radioactive tones found on Blue Book Ct-

rium Mine, In Monmouth township, at a distance of about U miles.

To Investigate this possibility, a preliminary explora

tion program was executed at the property during the period pf A-

pril to August inclusive. This program consisted Int

(a) Line cutting at 300-foot Intermit over the entire property}

(b) Geological mapping of the surface on a seal* of 200 feet to l inch|

(c) A scintillometer survey with readings at 100-foot Intervalsi

(d) Some 2,000 linear feet of stripping, trenching In overburden, bulldozing and rook blasting, followed by sampling)

(e) Survey of the south boundary of the property by a qualified land surveyor.

As a result of this work it was decided to abandon the

9 easterly claims which had been found to be underlain by granite

intruded by pegmatite dykes and ireegular masses which, however, had

not revealed any radioactivity.

(2)

Mining and Development Con^any Ltd. (Cont'd)

One single radioactive zone was detected with the scintillo

meter, running entirely across the property in a northeast-southwest

direction. The radiometric anomaly is interrupted about the center

of the property by a swampy area but, there is every reason to belie

ve that the radioactive zone is continuous across the low area. Its

total length would then be in excess of one mile with the highest

readings recorded in the southwesternraost 1,1*00 feet. This is where

all surface work has been done to date.

This work has exposed an anastomosis of pegmatite dykes cut

ting crystalline limestone near its contact with a large granitic

mass underlying the eastern half of the property. Eighteen chip sam

ples were cut and assayed radiometrically and chemically for uranium

oxide indicating that most of the radiation is due to uranium oxide.

No petrographic work has been done yet and the radioactive mineral

or minerals have not been positively identified. Most of the values

obtained so far are below O.OlJf U^Og with the exception of one point

located on an off-shoot to the main pegmatitic mass where an assay of

O.U956(C) UoOg has been obtained.

Three maps are attached to the present reportt

(a) A surface map of the entire property, on a scale of 200 ft. to l inch, showing geology and scintillometer results as well as some topography}

(b) A sketch on a scale of 100 ft. to l inch showing detailed bulldozing and rock trenching on claims E.O,lliU88 and 1UU91J

(c) A plan on a scale of 5*0 ft. to l inch showing locations of samples and assay results.

(3)

^i 11 i Hi Mining and Development Company .Ltd* ^Cont' d)

GONG L US I O N S

The mining work executed to date at the property has been

t6o lindtod to justify any conclusion as to the prospective value

ox the property. Some encouragement has been experienced in this

initial prospecting but, no ore-shoot is yet indicated of a grade

that could be considered commercial under present economic condi

tions.

A limited amount of additional surface work might be exe

cuted to find out if values will imporve in certain directions but,

it is suggested that results be constantly reviewed before proceed

ing to large expenditures.

-o-o-o-o—o-o—

^k^X^i ssfe&s'

(U)

Qarland Mining and Development Company Ltd* (Gont'd)

PROPERTY

Initially, the property consisted of mining claims E.0.1UU83 to lli^OO inclusively, and, E.0.110^2 to 11060 inclusive, located on lots h to 12, Concession XVIII, Anstruther township, Peterbo rough County, Eastern Ontario Mining Division.

Recently, mining claims E.0.1105(2 to 11060 incl. have been al io wed to lapse so that the property consists now of only 18 claims of 1)0 acres each for a total area of 900 acres. These claims are unpatented.

TOPOGRAPHY

The entire surface -*f the property is surprisingly flat com pared to the rest of t /region. The relief generally does not ex ceed 50 feet with the J iption of some higher hills found towards the northwest corner of the property. But even these hills do not exceed 100 feet in elevation.

Overburden covers about 2^ of the property area and, consists mostly of sand on the higher ground, with a large swamp occupying the center of the property and extending for a distance of about 3,l|00 feet in an East-West direction and, 1,000 feet North-South. An alternation of hills and valleys imparts a northeast lineation to the topography.

Considerable second growth hardwood and spruce covers a lar ge part of this area making lumbering an important industry.

ACCESSIBILITY

The property is located some 6 miles soufehwest of the vil lage of Tory Hill and, twenty-eight miles west of Bancroft which is located some 16^ miles northeast of the City of Toronto.

The property can be reached by automobile as far as Blue Rock Cerium Mine. Thence, by Jeep for the remaining distance of a- bout li miles.

OEOLOQf

With the exception of a large low area about the center of the property, rock outcrops are very numerous. It may be stated that bedrock outcrops over about 7S# of the property area. Most of the outcrops are small but, some large ones are found on the eastern half of the property.

No laboratory petrographic work has been done yet although some is planned for the near future. In field geological mapping, Satterly's rock classification has been used as shown on Map No.5*2A

garland Miningandi Development Co.Ltd.(Cont'd)

(5)

of tho Ontario Department of Kines entitled "Haliburton Area".

The property is located within the Grenville sub-province of the Precarabrian, and not far from their contact with Paleozoic limestones. The rock formations identified are as follows:

(a) Oranite pegmatite;(b) Granite, granite gneissj hybrid gneisses of igneous

origin and also of sedimentary origin;(c) Syenite, hornblende syenite gneissj(d) Metagabbro, amphibolite, hornblende plagioclase

gneissj(e) Limestone, lime silicate rock}(f) Paragneiss.

All these rocks have been briefly described by Satterly in "Mineral Occurrences in the Haliburton Area"j Ont. Dept. of Mines, Vol.Lil, Fart II, 1?U3.

The Haliburton-Bancroft area is largely underlain by pink to grey granite and syenitic rocks which are now largely exposed by e- rosion. These acid intrusive masses and related pegmatites once in vaded thick beds of sediments, now classified as the Hastings- Orenvillo series. Only relatively small areas of the sediments re main as highly altered and infolded bands betwen the many outcrop- pings of the intrusive masses.

The l? easternmost claims are underlain by granite and gra nite gneiss intruded by many pegmatite dykes and other large irre gular masses. A small circular roof-pendant of paragneiss is found close to the southeast corner as well as a small remnant of lime stone.

Proceeding towards the northwest from the above-mentioned gra nite mass, wo find that it is flanked by limestone whose average thick ness approximates 1,000 ft.(horizontal) towards the south and some 600 ft. towards the north. A large tongue of raetagabbro intrudes the limestone towards the north boundary of the property and, numerous pegmatite dykes and irregular masses cut through the limestone where ver it is exposed on the property,

A total thickness of about 3,UOO ft,(horizontal) of paragneis- ses follow the limestone towards the northwest. These paragneisses ex hibit fairly uniform composition and, are intruded on mining claim E.0.1iiU89 by a wedge-shaped mass of syenite 1,200 ft. in legnth by J?00 ft. in width at the north boundary of the property.

Both paragneisses and limeteone together underlie about the western one-third of the property. They trend N-U!?O-E. and dip on the average 60 degrees to the southeast. No faulting has been obser ved yet although some topographical features would suggest some.

Garland Mining and Development Company Ltd.(Cont'd)

(6)

SCINTILLOM.flER SURVEY ft RESULTS

During, the months of May, June and July 1955* the property was completely grfidded in a north-south pattern with lines at 300- foot intervals. This was followed by a scintillometer survey by Mr. Ernile Leblanc under the fiold supervision of D.E,Cameron, Mining Engineer. The instrument used \jas a C.A.E.Model 963 scintillometer and readings were taken at hip level at every 100 feet along the picket lines with occasional readings taken at ground level when ever possibly significant deviations were obtained. All field obser vations have been recorded on the accompanying map on a scale of 200 feet to one inch.

The writer has not computed the statistical averages over the different rock formations present at the property but, a glance at the readings would tend to sh'ow that there is no significant dif ference in radioactivity over the different rock formations encoun tered. The average background over the entire property at hip level is approximately 15 counts per second with a range of 8 to 25.

Some highly scattered and quite isolated readings were ob tained amounting to about 5 times background here and there but, no length was found in connection with these anomalous results with the exception of a band in the limestone which was traced intermittently almost in a straight line right across the property coinciding in direction with the strike of tho contact between intrusive granite and the sedimentary formation. No very nigh readings were recorded along this band, the maximum being about 50 times background but, this band is definitely radioactive and more intensely so between a central low ground area and the south boundary of the property where the highest readings were obtained.

This radioactive band consists of limestone which follows and has been intruded by a large granitic mass lying to the east. The limestone itself is found intruded in an irregular manner by several dykes and irregular masses of acidic pegmatites within which the ra dioactive mineralization is found. Towards the northeast, past the low central area, the radioactivity could again be traced but, the readings are weaker and not so persistent although they are found a- cross appreciable widths which has reached 300 feet at some points,

To summarize the foregoing, it may be stated that the scin tillometer survey has Indicated a radioactive zone striking northeast across the entire property for a distance of over 5*000 feefc with a gap at the center where a swamp interrupts the rock formations. This radioactivity is found to be due to radioactive mineralization, not otherwise identified at the present time, but occurring within peg matitic material cutting and intruding limestone in irregular fashion.

Although the radiometric observations are not, on the whole, too strong, as terrain conditions would have a tendency to reduce the radioactive emission if not masking it completely, in vidw of the fore going results, it was decided by the Company to execute a limited a- mount of surface work to probe that section of the anomaly which had given the strongest radiometric results with the scintillometer.

(7)

A Garland Mining and Developgient Company Ltd. ^Cont'd)

SURFACE W3RK AND RESULTS

Consequently, during the month of August 1955* some 2,000 linear feet of trenching, bulldozing and blasting in rock was exe cuted along and on both sides of a sub-base line extending in a northeasterly direction for a distance of 1,000 feet from the south boundary of the property across mining claims E.0.1UU88 and part of E.O.lUU91.(See Sectional Plan No.l attached hereto.)

This work was followed by some preliminary sampling to as certain radioactive values and also to correlate results with scin tillometer readings. Eighteen chip samples and one grab were taken and assayed both radiometrically and,chemically when results exceed ed 0.03* uranium oxide equivalent, the laboratory work being execu ted by the Toronto Testing Laboratory at Bancroft, Ont.

All assay restilts are shown on attached Sectional Plan No.2 and could be tabulated as follows:

RADIOACTIVITY SAMPLE No.

313233 3U3536373839 UO hi U2 U3 UU 1*5

U8 U9

TYPE OF SAMPLE WIDTH

Chip U.O'Chip 3.0'Chip 3.0'Chip 3.0'Chip U.O'.Chip U.O'Chip U.O'Chip 3.0'Chip 3.P 1Chip U.O'Chip b.O'Ehlp U.O'Chip U.O'Chip U.O'Chip U.O'Chip U.O'Chip U.O'Chip U.O'Grab ~~

CHEMICAL" ii^ba

o.o5U* 0.030* O.OU9*

0.061* 0.063*

0.032*

o.oiU* 0.019*

O.U90* 0,087* 0.621*

RADIOMETRIC

0.018* 0.082*o.oUi*0.069* Trace 0.010*0*029* 0.052* 0.07U*o.oiU*w 9 ^r^^+pr0.038*O O91*o.ouo* 0.039* Trace 0.010*0.508* 0.08U* 0.6U9*

It will be seen from the foregoing results that, if in cer tain cases both radiometric and chemical assays agree very well in other cases there is a very significant difference which is interpre ted as reflecting the presence of thorium in the sample. On the who le, however, it is apparent that the sampling has tended to confirm the indications obtained with the scintillometer.

In addition, this surface work has revealed that the ra dioactivity was due to pegmatite dykes cutting the limestone in quite irregular fashion.

(8)

Garland Mining and Developmnt Company Ltd, (Cont*d)

CONCLUSIONS

One thing became quite obvious during the work which has been previously described: it was the almost complete absence of ra dioactivity over the large granitic intrusive occupying the eastern half of the property. It was therefore decided by the Company to al low the nine eastern claims bearing Nos.E.0.11052 to 11060 incl. to lapse. As these claims became due on September 30th,1955* to all in tents and purposes, these claims should be considered as aVandoned although included on the surface map of the property.

The scintillometer survey combined with the geological work indicated a fairly promising set of conditions for the presen ce of a radioactive ore-body on the property, if of low-grade. The surface work completed to date is inconclusive i# this respect. In my opinion, some additional work is warranted to a limited extent and, depending on the results obtained, if such course is found Jus tified, an expandod development program involving perhaps some dia mond drilling could then be considered by the Management.

Respectfully submitted

l 31D16SW0064 63A.298 ANSTRUTHER

B A, ARCS (t.,——r,.,.,,

CONSULTING ENGINEER jMINING ft CHEMICAL ;

MONTREAL, QUE.

020

TECHNICAL REPORTON

GARLAND MINING AND DEVELOPMENT CO. .LTD.

Anstruther Township'Property Peterborough^ Cfonnty ? tjO*vE*

(A.E.C.B. Exploration Perndtt- MX 93/55) (Ontario Mining License:- A-29082)

titw"''"J*4Cfo*

REPORT NO.M...w 8?

DATE ..January 2lith, 1956

TECHNICAL REPORT

-on-

OARLAND MININ3 AND DEVELOPMENT CO. LTD.

Anstruther Township Property

Peterborough County, Ont,

(A.E.C.B. Exploration permit: MX (Ontario Mining License: A-29082)

-by-

L.germain,P,Eng.

j*

e* ̂v^StiSrREPORT No. M -

DATE i -January aUth, 1956

JU.EVARP .TEL RAvuoND 2-3771

Heonarb (Sermam*e.A. A R,c s (FNGIAND)

CONSULTING ENGINEER

MINING (k CHEMICAL

MEMBER O F T HE CORPORATION O F P ROFESSION AU ENGINEERS OF OUEBcC

MEMBER OP THE C.l.M.M. AND A.A.A.S.

Montreal, 2J4th ' 1956

OF QUALIFICATION

I, LEONARD GEHKAIN, Professional Engineer of the City of Montreal, Province of Quebec, do hereby certify as follows:-

1.- That I ara a Consulting Engineer, with office at 706? Pie IX Boulevard, Montreal, Province of Quebec, Canada}

2.- That I have graduated in arts at the University of Montreal, in 1921 and, that I hold the degree of Bachelor of Arts(B.A.)j

3*- That I have graduated in chemical engineering at the Imperial College of Science and Technology, London, England, in 192U, and that l hold the degree of Associate of the Royal College of Scienoe(A.R,C.S,)j

U.- That I have been duly admitted a member of the Corporation of Professional Engineers of Quebec on May ?th, 1926, and, that I am a member in good standing of the said Corporation}

J),- That my experience in mining covers a period of 30 years during which I have been continuously and actively engaged in various phases of the industry}

6.* That I hold fifty thousand(50,000) pooled shares of OAKLAND MIN'lNO AND DEVELOPMENT CO. LTD,, acquired in payment of sy pro* fesslonal services at the inception of the Company. I have no further interest, either directly or indirectly, in the property mentioned in the present report, or, in the securities of the Cojqpany, nor do I expect to receive any interest, either direc tly or indirectly, in the property concerned or in the securities of the aforementioned cowpany}

7.- That my present report is based upon personal knowledge of the property, and, upon general information gathered in the courts of supervising the work done thereupon.

TEL RAYMOND 2 -3771

Heonarb GermainB.A. ARCS (ENGLAND)

CONSULTING ENGINEER

MINING S. CHEMICAL

MEMBEfi OF THE CORPORATION OF PROFESSIONAL ENGINEERS CF QUEBEC

MEMBEFi OF THE C l.M.M. AND A A.A.S.

January 2Uth, 1956

FOREWORD

In a previous report (Report No. M-85) dated Noventoer 30th.

1955* the work done and remits obtained up to the end of August

had been described and coianented upon.

On the basis of information gathered in surface geological work

and during a scintillometer survey of the property, it was then recom

mended to drop the Eastern part of the property consisting of mining

ciaim Nos. E.O.11052 to 11050 inci, located on lota 9 to 12 inol, of

Concession XVIII of Anstruther township, and, to retain the balance

ooneieting of mining claims Nos. E.0.11^83 to 1U500 inol. covering

lota 1; to 9 inol. of the same Concession* This has now been done and,

the Atomic Energy Control Board Exploration Permit MX 93/55 has been

amended accordingly.

No work was done at the property during the months of Septem

ber and October 1955 but, the Company executed some additional surface

wrk and sampling during the months of November and Deoewber. It ia

the purpose of the present report to describe this work in detail,

give the results obtained and make appropriate recommendations re

garding the future of the property* Maps showing the location* where

the work was done have been attached hereto.

Garland Mining and Development Co.Ltd. (Cont'd)

WORK DONE

(2)

During the months of November and December 19i#, a total of

210 man-days of actual work was executed which, after correction

for certain allowances of the Ontario Mining Law depending on the

nature of the work, yields a total of 1*28 statutory man-days applicable

as assessment work. This and the previous work completd leaves a ba

lance of 11 days per claim to complete two years' assessment work,

The work done during the period has consisted in the following:

1.- Trenches Ea and G have boen deepened an additional 2 to 3 ft. by rock blasting} Ea being now 6 feet deep and G being h feet}

2.- Eleven additional rock trenches have been dug for a total li near footage of l8|? feet: three of these trenches being loca ted on cltiras Nos. E.0.1liU93 and 114*92. The average depth of all these trenches is 2 feet;

3*- Power stripping amounted to 8 days' work in addition to manual labor;

It,- Approximately 3?,000 square feet of bulldozing was performed to strip parts of the radioactive zones one continuous length of Ii50 feet has been exposed thereby in addition to intermit tent trenching. All trenches were blasted to fresh rock before saraplingj

5.- Six thousand seven hundred feet (6,700 ft.) of picket lines were cut on each side of the sub-base line,

6.- All trenches dug wore geologized;

7.- An additional 2,000 feet of bush road was bulldozed to facilitate the workj

8.- Twenty-five (25) chip samples were taken distributed over 8 sec tions roughly eighty (80) feet apart. These samples were tested both radlometrically and chemically for uranium at the Toronto Testing Laboratories in Bancroft, Ont,

All the foregoing work, with the exception of three trenches

mentioned in (2) above, was done on mining claims Nos.E.0.11*1*88 and E.G.

tiarland Mining and Development Co.Ltd. Cont d)

RESULT S

(3)

Plan No, 2 attached hereto shows the locations of all samples taken

and their percentage uranium oxide content, with samples taken in pre

vious work being shown above the trenches and those taken during the

present period appearing below the trenches. Altogether 25 chip sam

ples were taken during recent work,

Whereas previous sampling had given an average grade of 0,0385S u-

t

raniura oxide across an average width of 6.75 feet for a length of 3UO ft,,

the present sampling has yielded an average grade of 0,066^ U^OQ, or,

S9.57 per ton across 9.0 ft, for a length of U50 feet. This is equiva

lent to approximately 350 tons per vertical foot.

COMMENTS

In connection with the foregoing results the following remarks

would seem warranted.

1.- Although values have been low for the remaining section, the total

length of the radioactive zone amounts to approximately 800 feet

altogether. Should values improve in depth, there would be a fair

possibility of dcseloping an ore tonnage of 500 to 600 tone per

vertical footj

2.- On account of possible leaching of uranium minerals from the sur

face -and re-precipitation at depth, surface sampling is not consi

dered a too reliable criterion of the mine-making possibilities

of the? zone.

3.- It should also bo rationed that radioactive emission is complete

ly arrested by l foot of rock, 2 feet of overburden and roughly

3 feet of water. Consequently, scintillometer readings should not

be considered too reliable an indication of the grades to be ex

pected at depths in a radioactive zone.

It,- VJhen present samplinc results are treated by the statistical method

of standard deviation it is seen that for the number of sections

taVen across the radioactive zone, namely 8, and considering the

fluctuations in values from section to section, the true grade may

be ae low as 0.029J6 and as high as 0.105# uranium oxide with a

probability of lOOJfifcXn other words, assuming a break-even point

(x) that it lies between these two limits.

.(h)

Garland Mining and Development Co.Ltd, (Cont'd)

of 0.10^ and a price of #7.?!? per pound for uranium oxide, there

is a possibility that this radioactive zone might yield a profi

table grade in small tonnages.

cal study:The following basic data have been used in onr ststisti-

SAMPL1NG DATA

LOCATION

Trench "D"....Trench "F,K".Trench "F"....

Tiwnrh "H"

Trench "1",...

WIDTH (n.).... 6,0.... 1.2.0.... 6,0

"c? o.... 6,0..., 12.0

VALUE (^ UiOft

0,0580.0180,0620.073

0.065

) WIDTH X VALUE

0.3U80.2160,3720.8760.98U0,780

As some of the above sections are compounded, It should

be possible to rai.se the average grade somewhat by taking narrower

widths.

CONCLUSIONS AMI i RECO'^iENTJATIOMS

Although the results obtained to date at this property could

not be considered commercial, they are too close to commercial gaades

and the possibility of better results under further exploration IB too

distinct to allow the property to lapse without further work,

It is, therefore, recommended that a series of holes be drill

ed across the zone to out it at a vertical depth of about 100 feet, such

holes to be spaced not more than ^0 feet apart. It is estimated that some

13 holes at least will be necessary totalling about 2,000 feet,

In addition to uranium, the core should be tested also for

thorium, zirconium and rare earths as the radioactivity of some spe

cimens tested by the Radioactivity Laboratory of the Dept. of Mines

and Technical Surveys showed the presence of uraninite, uranothorite,

allanite and cyrtolite, v^uch additional elements might raise the grade

sufficiently to make it attractive.

Respectfully submitted

L. .Eng,

SECTIONAL PUN No.l

310165*8864 63A.298 ANSTRUTHER 200

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STE

RN

O

NT.

Sur

face

pl

an

of

radi

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ive

zone

show

ing

loca

tions

of

sa

mpl

es

in

rock

tr

ench

es

with

as

say

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lts

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le:

l in

ch

* 4

0 fe

et.

Dra

wn

by;

Dat

e:

Jahu

ary

^45,

1956

_______

PL

AN

N

S 2

A.

LEGEND

Granite pegmatite

Granite gneiss

Bulldozed area

Rock trench

Claim ( Lot) line

Strike and dip of contact

Strike and dip of sediments

GARLAND MINING 8 DEVEL. CO. LTD.,ANSTRUTHER TWP.- EASTERN ONT.

NOTE:

-Area cleared io bedrock by bulldozer

is approximately 17,000 square feet.

-The rock trenches are generally 4' to 6' deep

-The picket lines are blazed and chained

SURFACE PLAN showing nature and extent of assessment work

carried out on claims E.O. 14488 ft E.0.14491

Claim N2

E.G. 14488

Claim N2

E.G. 14491Lot6

Con. XVIII

Lot 5

Con. XVIII during November and December, 1955.-*— ̂ \Scale; l inch - 40 feet.South B oundary Surveyed

Drawn by31DI6SW0064 63A.a9S ANSTRUTHER

o o o

vtfr.

J

T

T

l

sto

3 S

(

(O10 l

\

Claim N*

E.0.14492Lot 7

Con.XVIII

NOTE

T

l

\

II

LEGEND

l. G ranite pegmatite

Limestone

Granite gneiss

i O pen swamp

Rock outcrop

Bulldozed area

Rock trench

. -— - Claim line

Picket line

Claim N2

E.G. I4493Lot 7

Con.XVIII

roMain base line

4-

I

O rOi

Note: Area cleared tobedrock by bulldozer is approx. I5,000sq.ft.

The picket lines were cut prior to below period

w

The. scintillometer readings obtained over

the rocks exposed in the trenches did 4l

not justify sampling.

31D16SW0064 63A.298 ANSTRUTHER230

GARLAND MINING S DEVEL.CO. LTD.,

ANSTRUTHER TWP.- EASTERN ONT.

SURFACE PLAN

showing nature and extent of assessment wor

carried out on claims E.O. 14492 ft E.0.14s,

Drawn by:

during November and December, 1955.

Scale: l inch * 1 00 feetD a t e i 'PLAN

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24,

1955

f

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fig.

IND

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100

200

400

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