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
oact
ive
zone
show
ing
loca
tions
of
sa
mpl
es
in
rock
tr
ench
es
with
as
say
resu
lts
Sca
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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MIN
ING
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, Tr
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Mo n
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Twp.
A
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Twp.
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Gra
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p
eg
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Gra
nite
, gr
anite
gne
iss;
h
ybrid g
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of
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ous
and
sedi
men
tary
or
igin
Sye
nite
, ho
rnbl
ende
sy
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ne
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lite
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nde
plag
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ase
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ss* *
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est
on
e,
lime
si
lica
te
rock
*-P
arag
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s
SY
MB
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Str
ife
and
tfip
of
sedi
men
ts
Str
ike
and
dip
of
schi
stos
ityan
d gn
eiss
osity
S
wam
p,
low
gr
ound
Geo
logi
cal
con
tact
(
defined)
Geo
logi
cal
con
tact
(a
ssu
me
d)
Bus
h ro
ad
Rig
ht s
ide
' hi
p le
vel
Sci
ntil
lom
ete
r re
ad
ing
s:
. ^
^ ,
Left
side
: g
roun
d le
vel
Bou
ndar
y lin
e
(Pro
pe
rty)
Lot
line
s
Cla
im
line
s
Tre
nch
Cre
ek
Roc
k tr
en
ch
Dra
wn
by:
App
rove
d by
:
Dat
e: S
ept.
24,
1955
f
i '
Z..
Germ
ain
P.
E
fig.
IND
EX
M
AP
l in
ch -
20
mile
s
: l
inch
*
2OO
fe
et
20
0
100
200
400
60
080
010
00
FEE
T
CO
N^
XV
IH
CON.
XV
~I l
RA
RE
E
AR
TH
M
INE
S
BLU
E
RO
CK
M
INE
S
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NC
RO
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Min
ing
a
Dev
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men
t Co
. Lt
d
nstru
ther
Tw
p.
LIND-
SAY
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TE
RB
OR
OU
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LL
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ILL
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31D
I6S
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64
63A
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AN
STR
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24
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