december - british columbia
TRANSCRIPT
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B y R. H. JANES, P .Eng.
REPORT ON MINERAL LEASE 94,
SIMILKAMEEN M I N I N G D I V I S I O N
B R I T I S H COLUMBIA
49" 25 ' , 121" 05' ( 9 2 H - 6 E )
.FOR
S I L V E R SADDLE M I N E S LTD.
December 18, 1985
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CONTENTS
SUMMARY J
INTRODUCTION /
CONCLUSIONS
RECOMMENDATIONS J
HISTORY AND WORK DONE
REGIONAL GEOLOGY .-
GEOLOGY OF MINERAL LEASE 94 AND SURROUNDING AREA J’
GEOTECHNICAL SURVEYS
V E I N SYSTEMS
REFERENCES
CERTIFICATE
APPENDICES % J
I D r i l l logs, H o l e s 85-2,-3 a n d -4 I 1 A s s a y C e r t i f i c a t e s d
FIGURES
LOCATION
PROPERTY
REGIONAL GEOLOGY
GEOLOGY OF SUMMIT CAMP
VLF CONDUCTORS AND SURFACE WORKINGS
GEOCHEMICAL S O I L ANOMALIES AND SURFACE WORKINGS
LOWER SHOWING EAST, D R I L L HOLES & GEOLOGY
LOWER SHOWING EAST, GEOLOGY
LOWER SHOWING WEST, GEOLOGY
PORTAL SAMPLE D E T A I L
2,
21
2L
F igu re 1 /’
II 2 /
3 /
4,
I‘ 5,
I’ 6 ,/
I’ 7 /
I’ 8 .
g J
10,
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SUMMARY ~ ~~
The Summit Camp i s charac ter ized by severa l rough ly east-west t r e n d i n g f a u l t
systems which a r e l o c a l l y and v a r i a b l y m ine ra l i zed w i t h s i l v e r , z inc , l ead
and i r o n sulphides, qua r t z and carbonates. Treasure Mountain hos ts severa l
smal l (30m. x 0.5m. x ? ) w e l l m ine ra l i zed "shoots" which were mos t l y h i g h graded. A l a r g e r p o t e n t i a l o reshoo t i s be l i eved t o have been found t h i s year .
Previous exp lo ra t i on on Minera l Lease 94 i n d i c a t e s t h e presence of t h r e e minera l i zed f a u l t systems.
De ta i l ed surface e x p l o r a t i o n o f these f a u l t systems employing VLF surveys and t rench ing t o search f o r t he poss ib le occurrence o f a d d i t i o n a l p o t e n t i a l
oreshoots i s mer i ted. f i r s t phase o f $100,000 inc ludes d e t a i l e d sur face e x p l o r a t i o n and diamond
d r i l l i n g o f the p o t e n t i a l o re shoot. d r i l l i n g o f any a d d i t i o n a l p o t e n t i a l o r e shoots found.
Current work has uncovered a p o t e n t i a l o reshoo t .
A two phased e x p l o r a t i o n program i s recommended. The
The second phase o f $110,000 i s fo r diamond
INTRODUCTION ~~
Peter N. Wrede, Pres ident o f S i l v e r Saddle Mines Ltd. , requested Janes t o examine and r e p o r t on Minera l Lease 94 and surrounding ground.
the lease and area f o r t h r e e days, 17 t o 19 October, 1985. H i l d i n g J . Rodstrom
acted a s guide. i n Vancouver.
Janes v i s i t e d
Rain f e l l most o f t h e t ime. One day was spent l ogg ing co re
The lease i s l oca ted 26 k i lomet res eas t nor theas t o f Hope i n t h e Hozameen Range o f the Cascade Mountains. Access i s v i a an a l l -wea the r f o r e s t r y road runn ing between t h e Coqu iha l la Highway and Highway 3* i n Manning Park and a good prospect road 1.1 k i l omet res
long. The nearest se t t lement by road i s Tulameen, 36 k i lomet res west, v i a
the f o r e s t r y road and t h e Tulameen R i v e r road.
E l e v a t i o n i s between 4,400 and 5,200 fee t .
Topography i s rugged, t h e r e s u l t o f a l p i n e g l a c i a t i o n .
i n the va l leys . Creeks and smal l lakes a r e f requent . Annual p r e c i p i t a t i o n i s 200 cms. o r more, a t l e a s t a t h i r d o f which i s snow. F i e l d work can be conducted from June t o October i n c l u s i v e . T imber - l ine i s between 5,500 and 6,000 f e e t
i n e leva t i on .
Overburden i s ex tens i ve
* The road connect ion t o Highway 3 i s n o t y e t es tab l i shed.
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CONCLUSIONS
Fault s t ructures hosting mineralization in the Summit Camp a re extensive. The Treasure Mountain Fault i s t raceable l a t e r a l l y fo r 2,700 metres and ve r t i ca l ly for 300 metres. The Bluebell Fault i s t raceable l a t e r a l l y f o r 1,000 metres and ve r t i ca l ly f o r 300 metres. Ore shoots found to date a r e confined t o Treasure Mountain except f o r the sulphide vein recently exposed by Si lver Saddle Mines L t d . on Mineral Lease 94. Government reports suggest t h a t the biggestoreshoots a re about 30 metres l o n g by h a l f a m e t r e wide, d i p o r plunge dimension i s unknown. varied between 10 t o 25 02s. Ag per t o n (340 to 860 grams Ag per tonne ) , 5-10% Pb and 5-10% Z n .
Grade of these shoots i s believed t o have
Application of up-to-date exploration methods has led t o the discovery of new veins. Foremost of these methods i s VLF-EM. I t i s inexpensive and when done i n de t a i l can provide a n exact "on the spot" location of conductors. Also i t i s not so susceptible tomaskingby overburden a s i s s o i l geochemistry.
Mineralization found t o d a t e merits continued exploration of Mineral Lease 94. Specifically,continued d r i l l i n g of the Lower Showing sulphide vein and explor- a t ion of the three vein systems f o r the presence of potential oreshoots i s
warranted.
The Lower Showing i s c lose t o the property boundary.' Consequently acquis i t ion of ground in t h i s area i s a p r io r i ty .
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RECOMMENDATIONS AND BUDGET
A two phased programe i s recomended.
on t h e d iscovery o f a d d i t i o n a l p o t e n t i a l o re shoots.
The s i z e o f t h e second phase i s dependent
Phase I
a.
b.
Obtain o p t i o n on the Amberty and Southern No. 8 1978 F r a c t i o n minera l c la ims.
Run d e t a i l e d VLF survey over conductors l oca ted by MPH Consul t ing.
l i n e s t o be no t more than 25 metres a p a r t and se lec ted f o r ease of t renching.
Where p r a c t i c a l each conductor l o c a t i o n should be t renched as o re shoots
a r e shor t . Where a p o t e n t i a l o re shoot i s i n d i c a t e d t h e v e i n t o be s t r i p p e d and sampled a t i n t e r v a l s o f one and a h a l f metres.
D r i l l Lower Showing su lph ide v e i n on r e g u l a r p a t t e r n t o determine ex ten t and approximate grade, cons ider i n t e r s e c t i o n s a t no more than 15 metres a p a r t i n plane o f ve in .
Survey
c.
d.
Phase I 1
e. D r i l l a d d i t i o n a l p o t e n t i a l o re shoots as found by s t r i p p i n g .
f. Consider open p i t t i n g and h igh-grading o f o re shoots t o p rov ide working
c a p i t a l .
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Phase I , Budget
VLF survey, opera tor and inst rument
Trenching w i t h c raw le r mounted back-hoe and
St r ipp ing , Lower Showing su lph ide v e i n p lus
Analyses Engineering
Crew: Transport , 8 weeks O i amond d r i 11 i ng , Lower Showing ,
Camp costs, 8 weeks Admin i s t ra t i on and o f f i c e
b u i l d i n g access roads.
say 2 p o t e n t i a l o re shoots
prospector and ass i s tan t , 8 weeks
300 metres NX core @ $100/m.
TOTAL
Say
Phase 11, Budget
Diamond d r i l l i n g two p o t e n t i a l
Analyses Engineering D r i l l roads Transport, 6 weeks
Crew: prospector and ass i s tan t , 6 weeks Camp costs, 6 weeks Admin i s t ra t i on and O f f i c e
o re shoots, 600 metres NX core @ $100/m.
TOTAL
$ 3,000
7,000
3,000
2,500 5,000
12,000 5,500
30,000 8,500
15,500
$ 92,000 $100,000
$ 60,000
1,000 7,000 4,000
4,000
9,000 6,500
18,500 $110,000
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PROPERTY
Relevant p roper t y data i s l i s t e d i n Table I . surrounding c la ims. o b t a i n an o p t i o n on some o f t h e surrounding ground.
I t covers Min ing Lease 94 and P. Wrede advises t h a t nego t ia t i ons a r e i n progress t o
HISTORY AND WORK DONE
I n 1894 Chas. Connel ly s taked the f i r s t c l a i m o f the Summit Camp, t h e Eureka, on Treasure Mountain. Fred S u t t e r i n 1895 d iscovered m ine ra l i zed outcrops t o t h e west on what i s now Min ing Lease 94 and w i t h John Amberty i n t h e f o l l o w i n g year staked t h e Vigo, Lulu, S u t t e r and Sky l i ne c la ims f o r people o f Terre Haute,
Ind iana. A. Jensen staked the S i l v e r Ch ie f on Treasure Mountain i n 1906.
The f i r s t work o f consequence was done on t h e S i l v e r Ch ie f group by t h e Treasure Mountain Min ing Company formed i n 1909 o r 1910 by W. Oornberg.
775 f e e t o f crosscuts ( two) and 395 o f d r i f t s were completed by about 1912.
Several o f the ve ins t o t h e west i n c l u d i n g those on t h e Morning S t a r and Blue B e l l c la ims had been explored by t rench ing and s h o r t a d i t s e.g. the upper
a d i t ( a d i t A, F igures 5 and 6) on t h e B l u e b e l l ve in . work ceased du r ing the Great War. w i t h t h e Mary E. M in ing Company which i n 1926 was taken over by J u l i a n Merger
Mines, Incorpora ted o f Los Angeles which c o n t r o l l e d Cascade Consol idated S i l v e r Min ing Company (Mary E. M in ing Company) and Blue B e l l S i l v e r Mine (Cap i ta l M in ing Company). These companies cont inued underground development a t Treasure
Mountain ( restaked as t h e Cascade group) and s e t up machinery a t the B luebe l l a d i t . Dur ing 1927 on Treasure Mountain a t about 1,000 f e e t below v e i n outcrop
a c rosscu t was begun and d r i v e n 1,258 f e e t t o t h e ve ins, 300 f e e t o f c rosscuts exp lo red the ve ins . Resu l ts were d i sappo in t i ng . On t h e Blue B e l l c l a i m a
c rosscut and d r i f t t o t a l l i n g 379 f e e t explored t h e B l u e b e l l v e i n ( a d i t D, F igures
5 and 6 ) . suspended work.
exp lo red on t h e N icke l P la te , Queen Bess and Morning S t a r c la ims, a l l w i t h i n t h e immediate area o f t h e present min ing lease.
Some
Development Dornberg i n s t i g a t e d a r e v i v a l o f i n t e r e s t
Resul ts here were a l s o d i sappo in t i ng and J u l i a n Merger Mines A t t h i s t ime repo r t s were made on m ine ra l i zed ve ins being
Some 196 f e e t o f t unne l i ng
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llWFRllD LO. YIVERAL C W Y
AL wnam WST
SILVER SADDLE MINES LTD. MINERAL LEASE 94
SIMILKAMEEN M.D., B.C. PROPERTY MAP
Figure 2 R J . Janes Dec.1985
eio R ~ N G E II P U S f4l
--
r"".
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TABLE I CLAIM DETAIL
NAME
Minera l Lease 94 (Lo t 130, Summit - 0. 2 M.C. and
e o t 132,Blue B e l l M.C.)
L o t 94, Sky1 i n e
L o t 93, Su t te r
h b e r t y
Southern No. 8 1978 F rac t i on
s kY
Spike
Argen tum
Queen Bess 2
RECORD NO.
738(9)
737(9)
1671 (7 )
461(10)
1128(8)
121 5 ( 10)
2562( 11 )
2654(6)
DATE OF LEASE E X P I R Y DATE AREA (HECTARES) OR RECORD
12 Jan. 1971 Rental pa id 28.46 up t o 12 Jan. 1986
27 Sept.1979 27 Sept.1990 18.02
27 Sept.1979 27 Sept.1990 20.92
9 J u l y 1971 9 J u l y 1990 N 75
12 Oct. 1978 12 Oct. 1989 ?
18 Aug. 1980 18 Aug. 1990 'v 175
27 Oct. 1980 12 Oct. 1990 N 175
5 Nov. 1984 - 437.5
10 June 1985 10 June 1986 500
OWNERSHIP
S i l v e r Saddle Mines L td .
Unicorn Resources L td .
Unicorn Resources Ltd.
Unicorn Resources L td . I
and/or Tarbo Resources Ltd. m
Ar thur 0. Thomas, Pr ince ton ,
Unicorn Resources L td .
Unicorn Resources Ltd.
S i l v e r Saddle Mines L t d
Dan Cardinal , Hope
Note: - = approximately
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was repor ted on t h e Morning Star . Mines Ltd. t o f u r t h e r develop the Queen Bess c la im.
( a d i t C (?) , F igures 5 and 6 was dr iven) . I n 1929 S i l v e r King Mines L td . acqui red c la ims he ld by Dornberg. C. J u l i a n and associated companies.
development and s top ing was done and th ree car- loads o f s o r t e d o re were shipped t o t h e T r a i l smelter. Summit Camp Mines Ltd. drove 237 f e e t o f c rosscut and d r i f t s f o l l o w i n g a v e i n on the Queen Bess claim, s i t u a t e d west of the Blue B e l l c l a i m and restaked a t a l a t e r da te as t h e Rook Eleven c la im. This i s
known as the H a l l ' s o r Tula prospect. d r i l l i n g was done on the Blue B e l l c l a i m i n an e f f o r t t o t r a c e t h e Treasure
Mountain Fau l t . Resu l ts were inconc lus ive . S i l v e r King Min ing Co. e rec ted a smal l m i l l us ing W i l f l e y tab les i n 1930, e s s e n t i a l l y t o e l i m i n a t e s p h a l e r i t e f rom t h e concentrates. F l o t a t i o n c e l l s were in t roduced i n 1931 and a b a l l m i l l i n 1932. About 130 tons o f l ead concentrates were shipped i n 1932.
I n 1928 A. Jensen formed Summit Camp
A c rosscu t 150 f e e t long
Underground
A t some t ime i n the 1920's diamond
A c t i v i t i e s decreased from 1932 t o 1950 when S i l v e r H i l l Mines L td . op t ioned
the S i l v e r Chief and Eureka c l a i m groups and d i d a l i m i t e d amount o f work. This company erec ted a 50 t o n per day m i l l near t h e p o r t a l o f t h e lowest a d i t on t h e S i l v e r Chief c la ims. cont inued dur ing 1955 and 1956. The m i l l s t a r t e d up i n December 1956. There was no produc t ion i n 1957 and t h e m i l l was removed. I n 1970 Copper Range Exp lo ra t i on
Company, Inc. conducted an ex tens ive appra isa l i n c l u d i n g underground mapping and sampling o f t h e Treasure Mountain p roper t i es .
P. Wrede acqui red Minera l Lease 94 i n 1971. conducted an e x p l o r a t i o n program on t h e western sec to r o f t h e Summit Camp which inc luded Minera l Lease 94 on opt ion.
o f a g r i d w i t h f lagged l i n e s a t 50 metre i n t e r v a l s (22 k i l omet res o f l i n e ) , geochemical s o i l sampling a t 20 metre i n t e r v a l s and magnetic and VLF surveys w i t h s t a t i o n s a t 10 met re i n t e r v a l s . Geological mapping and some t rench ing
was done. completed. lease i n 1984.
Underground development work was commenced and
I n 1983 Unicorn Resources L td .
This program inc luded establ ishment
E igh t diamond d r i l l ho les t o t a l l i n g 1,641 f e e t o f BQ w i r e l i n e were
Unicorn d i d n o t con t inue work and r e l i n q u i s h e d the o p t i o n on t h e
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Si lver Saddle Mines Ltd. commenced work on the lease in 1984 carrying ou t prospecting, s t r i p p i n g , b u l k sampling, road construction and engineering s tudies for an expenditure of $75,000*. Work continued i n 1985, w i t h a n expenditure of $45,000* on diamond d r i l l i n g , s t r ipp ing , prospecting, road building and engineering s tudies .
Production from the area i s as follows:-
S i lver Lead Zinc Property Tons Gold ozs . l l b s . l l b s .
**Silver Chief ? Ni 1 39,558 379,532 88,455 **Eureka 43 N i 1 873 12,825 13,624
***Mining Lease 94 42.25 30 180 1,850 6,930
Note: Production from ML94 i s a bulk sample by SSML, f igure f o r metals are approximate.
REGIONAL GEOLOGY
The Summit camp straddles the nor th northwest trending Pasayton Fault , a s t r i k e s l i p s t ruc ture which forms the contact between two terranes each separately accceted on t o the North American continent d u r i n g Mesozoic time. terrane i s t o the eas t o f the f a u l t . Methow-Tyaughton terrane. and deposited a f t e r accretion i s the Pasayten Formation of Lower Cretaceous age composed of some 2,500 metres of sandstone, conglomerate and pe l i t e . d i o r i t e of Lower Cretaceous or older age intrudes these sediments. o f the Tertiary Coquihalla Group, some 1,200 metres th ick , overl ies the Pasayten Formation and the Pasayten Fault . comprises the Lower t o Middle Jurass ic Ladner Group, some 1,800 metres of p e l i t e and volcanic sandstone, conformably overlain by the Upper Jurass ic Dewdney Creek Group, some 3,350 metres of volcanic sandstone and pe l i t e . Coarse grained massive grani te and granodiorite of the Mid-Tertiary Needle Peak Pluton and apophyses intrude the l a t t e r groups. T h i s in t rus ive and the Coquihalla Group may be p a r t o f the same igneous event.
The Quesnellia To the west and thrust against i t i s the
Lying unconformably upon the Quesnellia terrane
Quartz Volcanics
Here the Methow-Tyaughton terrane
* as advised by P. Wrede ** J . M . Black, BCMM, A n n . Rept. 1952
*** From Analysis Ce r t i f i ca t e 10 10281, dated 28 Sep. '84, Cominco, on shipment o f 12.56 tons from Si lver Saddle Mines L td .
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101.11,,*.....L..-dn.r.lrdI..I,,la.o'-. ........... m0ne.l- . M. . . . . . . . . . . . . .a ........................... wub,. . . . . . . . . . . . .................. ,oh".-. I.-. ............ "8
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TABLE I1
HISTORY OF EVENTS IN SUMMIT CAMP AREA
AGE
Pleistocene -
Miocene or
earlier
Eocene
Middle Cretaceous
Lower Cretaceous
Lower Cretaceous or older
Age ?
EVENT
Glaciation, Cordilleran ice sheet. Small scale faulting offsetting vein systems. Sulphide - quartz - carbonate mineralization along reactivated faults.
Intrusion of Needle Peak granodiorite pluton and extrusion of Coquihal la Group volcanics. Intrusion of feldspar dykes along ENE-WSW to E-W striking faults.
Development of ENE-WSW to E-W striking faults, may be related to Fraser River Wrench Fault System. Pasayten Fault System.
Transportation of western terranes, including Quesnellia, north on Kula plate t o approximate present position. Coincident major strike slip faulting. Folding and development of slaty cleavage. Accretion of Methow-Tyaughton terrane, which includes Dewdney Creek Group, onto Quesnellia terrane of North American land mass. Development o f Pasayten Fault.
Deposition of Pasayten Formation on Quesnell ia terrane.
Dislocates
Intrusion of Eagle granodiorite, member of Mount Lytton Complex, into Quesnellia terrane.
Intrusion of diorite bodies into Dewdney Creek Group.
Upper Jurassic
Deposition of Dewdney Creek Group on land mass to south and west (? ) and separate from North American land mass.
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Two o the r min ing camps l i e w i t h i n f i v e m i l e s o f t h e Summit Camp.
northwest a r e the Emancipation,Morning S t a r and o the r prospects, p a r t o f t h e
Coquihal la Camp. To t h e n o r t h severa l occurrences a r e s i t u a t e d near t h e
head o f Jim K e l l y Creek.
Small amounts o f su lph ides occur w i t h values i n g o l d and s i l v e r .
To t h e
These c o n s i s t o f qua r t z ve ins i n sch is tose rocks.
GEOLOGY OF MINERAL LEASE 94 AND SURROUNDING AREA
The Summit Camp was f i r s t mapped by C. E. Cairnes i n 1922. Add i t i ona l mapping
was done by J. M. Black i n 1952. D e t a i l e d mapping o f the lease area was done
by MPH Consul t ing L im i ted f o r Unicorn Resources L td . i n 1983.
i s based l a r g e l y on t h e above data.
Minera l Lease 94 i s l oca ted i n the western sec to r o f t h e Summit Camp. For
convenience the Pasayten F a u l t i s taken as t h e d i v i d i n g l i n e between eas t
and west.
The f o l l o w i n g
A h i s t o r i c a l geology t a b l e i s presented.
The Dewdney Creek Group u n d e r l i e s t h e western sec tor .
o f l i g h t grey weather ing vo l can ic sediments i n c l u d i n g t u f f , b recc ia and
agglomerate which amount t o approx imate ly 75 per cen t o f the group.
g e n e r a l l y up t o one metre t h i c k . Fragments range i n s i z e f rom a f r a c t i o n o f
a cent imet re t o a decimetre. Most a r e angu lar b u t the l a r g e r ones tend t o be
rounded. The fragments a r e f i n e gra ined and vo l can ic i n o r i g i n . A r g i l l i t e
and conglomerate a r e in terbedded w i t h t h e vo l can ic sediments. The a r g i l l i t e
i s genera l l y dark grey weather ing t o a l i g h t grey. I t i s t h i n bedded, many
beds a r e less t h a t n one-quarter o f a cent imet re t h i c k .
a r e common.
format ion. Most a r e greenish. These comprise rounded and subangular pebbles
and cobbles i n a tu f faceous m a t r i x . Pebbles and cobbles c o n s i s t most ly o f
t u f f s , f lows and f i n e gra ined i n t r u s i v e s . Disseminated p y r i t e i s
present throughout the format ion.
I t comprises a v a r i e t y
Beds a r e
S o f t sediment s t r u c t u r e s
Conglomerates a r e present ma in l y i n t h e eas tern p a r t o f the
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Figure 4 - GEOLOGY OF SUMMIT CAMP From BCMM, Ann.Rept., 1952, by J.M.Black
Approximate boundaries of Mineral Lease 94 outlined
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D i o r i t e s i l l s and dykes i n t r u d e the Dewdney Creek Group. a l t e r e d and show development o f c h l o r i t e and carbonate. The l a r g e s t body,
a s i l l , occurs j u s t west of t he Pasayten F a u l t , under l y ing the Why Not F r .
( L o t 1209) and Eureka ( L o t 1210) c la ims.
These a re genera l l y
A f t e r a c c r e t i o n o f t he Methow-Tyaughton te r rane, which inc ludes the Dewdney
Creek Group, t o Quesnel l i a eas t nor theast -west southwest t o east-west s t r i k i n g f a u l t s developed.
and a r e p e r s i s t e n t both l a t e r a l l y and v e r t i c a l l y . One o f these, the Treasure
Mountain F a u l t i s t raceab le on sur face f o r 2,700 metres and v e r t i c a l l y on the S i l v e r Ch ie f c l a i m f o r 300 metres. Width i s up t o s i x metres. Feldspar
prophyry was i n t r u d e d a long some o f t he f a u l t s .
sulphide-quartz-carbonate m i n e r a l i z a t i o n as f r a c t u r e f i l l i n g s and wa l l rock
replacements du r ing r e a c t i v a t i o n o f these f a u l t s .
These may be r e l a t e d t o t h e Fraser R ive r Wrench F a u l t System
A l a t e r igneous event produced
M i n e r a l i z a t i o n cons is t s o f one o r more s t r i n g e r s o r ve ins, p lus v e i n m a t e r i a l
i n pockets and d isseminat ions i n v e i n w a l l s . Veins branch and s p l i t and vary
cons iderab ly i n w id th and a t t i t u d e . I n d i v i d u a l v e i n w id ths r a r e l y exceed
severa l cent imetres b u t do vary up t o around h a l f a metre.
i s genera l l y l e s s than about 30 metres.
veins, m ine ra l i zed w a l l rock, gouge and sha t te red rock may approach two metres.
Sulphides comprise the g rea te r p a r t o f t h e v e i n m a t e r i a l . I r o n r i c h s p h a l e r i t e
and galena a r e prominent, p y r i t e and p y r r h o t i t e a r e l e s s abundant, cha lcopyr i te ,
magneti t e , arsenopyr i t e , t e t r a h e d r i t e and s t i b n i t e a r e sometimes present i n
minor amounts. B lack r e p o r t s t h a t t h e s i l v e r l ead r a t i o i s between two and
th ree ounces o f s i l v e r t o one per c e n t lead.
occurs as a r g e n t i t e conta ined i n the galena. i n s p h a l e r i t e t h a t shows a cadmium t o z i n c r a t i o o f about 1 t o 100.
va lues a r e repo r ted t o be genera l l y l e s s than 1 g. per tonne.
Vein c o n t i n u i t y
An aggregate w i d t h o f minera l i zed
Cairnes suggests t h a t the s i l v e r
B lack r e p o r t s a cadmium conten t Gold
L a t e r f a u l t i n g caused minor o f f s e t t i n g o f t h e ve ins.
systems a r e considered separa te ly i n a f o l l o w i n g sec t i on .
The i n d i v i d u a l v e i n
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GEOTECHNICAL SURVEYS
MPH Consul t ing L i m i t e d under c o n t r a c t w i t h Unicorn Resources L td . c a r r i e d o u t
geochemical s o i l , magnetic and very low frequency e lect romagnet ic (VLF-EM) surveys
on most o f Minera l Lease 94, no r the rn h a l f o f L o t 93, eas tern p a r t o f Amberty
minera l c la im,par t of Sky minera l c l a i m and Lo ts 1213 and 1214.
S o i l samples were analysed f o r lead, z i n c and s i l v e r us ing atomic absorpt ion.
MPH Consul t ing s ta tes t h a t lead, z i n c and s i l v e r values i n excess o f tw ice
th resho ld are considered d e f i n i t e l y anomalous and a minimum f o r a contour ing
i n t e r v a l .
responses and low z i n c response. Four zones w i t h anomalously h igh values i n
lead, s i l v e r and z i n c were o u t l i n e d and a f i f t h h igh e x i s t s a long an ou ts ide
l i n e . These a r e summarized i n Table 111.
S o i l samples over known and t e s t e d showings showed lead and s i l v e r
The a p p l i c a t i o n o f VLF surveys t o l o c a t e su lph ide m i n e r a l i z a t i o n i n ve ins and
f a u l t s t ruc tu res i s a proved and acceptable method.
s t a t i o n loca ted a t C u t l e r , Maine were measured us ing a Geonics EM-16 r e c e i v e r . Data was p l o t t e d i n p r o f i l e format showing the in-phase d i p angles i n percent .
Anomalies o f l ess than 10% peak t o peak response were ignored unless these
received support f rom anomalies on ad jacent l i n e s o r f rom o the r geotechnica l
in format ion. Two complex conductor systems were o u t l i n e d . The system A-B o u t l i n e s the v e i n system on which were d r i v e n a d i t s A, B and D and t o the west
co r re la tes w i t h geochemical anomaly Zone 8.
i z a t i o n fo l lowed by t h e C a d i t and i t s form suggests an o f f s e t system of
severa l m inera l i zed east nor theas t s t r i k i n g s t r u c t u r e s which form an east-west
t rend ing zone. Conductor E may represent a separate s t r u c t u r e o r poss ib l y
the no r th nor theas t s t r i k i n g Ridge F a u l t (Black, 1952). A t h i r d conductor
system, t rend ing east-west, t raverses the midd le o f t he eas tern s e c t i o n o f
L o t 130.
and the ve in r e c e n t l y exposed a t t h e Lower showing c o r r e l a t e w i t h t h i s conductor.
A d i t E, Lo t 130,may be o n a c o n t i n u a t i o n o f t h i s v e i n system which has been
o f f s e t t o the nor thwest .
Transmissions f rom t h e
The system C-D o u t l i n e s m ine ra l -
Old dumps, near the c l a i m boundary, c o n t a i n i n g galena and i r o n su lph ides
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LOT 130
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TABLE I11
ANOMALY NO. (MPH CONSULTING)
Zone 5
6
SUMMARY OF GEOCHEMICAL SOIL ANOAMLIES I N AREA OF MINERAL LEASE 94
LOCATION CLAIM S I Z E
8+50W t o 9+50W Amberty 100m. long 1+50S t o 1+75S M.C. 25m. w i de
DESCRIPTION
I n area o f extens ive overburden. Weak and d i s j o i n t e d pa t te rn .
11tOOW t o 13+50W M.L. 94, 250m. long, Out l ines Queen Bess v e i n otoo t o 2+00s L o t 132 25m. wide, system ( a d i t C). Pa t te rn suggests
open t o southwest presence of another v e i n t o south 1
9+oow t o 11+oow M.L. 94, 200rn. long, 0+50N t o 1+50N Lots 132 l O O m wide
& 130
I
Out l ines B luebe l l v e i n system ( a d i t s A, B & D)
14tOOW t o 19tOOW L o t 93 500m long, Out l ines and extends v e i n system 2+00N t o 2t50N 50m. wide, t o east though extens ion may i n
subs id ia ry zone t o the southeast o u t l i n e s the Ind iana ve in .
open t o the west p a r t be a drainage a f f e c t . A
13tOOW 3+60N t o 3+80N L o t 130 40m. long S i tua ted a t edge o f g r i d .
c o r r e l a t e w i t h conductor t o east . May
Note: Data f rom r e p o r t by MPH Consul t ing, dated 20 September 1983.
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The weak ccnductor F ,s i tua ted t o t h e eas t on L o t 1214,correlates w i t h the
Treasure Mountain F a u l t .
Geometrics 6-816 and S c i n t r e x MP-2 magnetometers were used f o r a magnetic survey. This showed a un i fo rm background f i e l d f o r t he area i n the range
57,400 t o 57,500 gammas punctuated by l i n e a r east-west t r e n d i n g anomalies.
A concen t ra t i on o f these occurs i n the no r the rn h a l f o f L o t 132. Here the
anomalies s t r i k e northeast-southwest and p a r a l l e l the s t r i k e of o u t l i n e d
conductors. MPH Consu l t ing i n t e r p r e t s these anomalies as caused by t h i n .
shal low, s u b v e r t i c a l d ipp ing bodies w i t h a v a r i a b l e magnetic minera l content .
Th is i s subs tan t i a ted by the observed presence o f p y r r h o t i t e as a v e i n sulphide.
V E I N SYSTEMS
The combined evidence f rom a d i t s , s t r i p p i n g , geo log i ca l mapping and geotechnical
s tud ies i s i n t e r p r e t e d t o have demonstrated t h e presence o f t h ree v e i n systems
t r a v e r s i n g Minera l Lease 94.
The B l u e b e l l v e i n system i s i n t e r s e c t e d by a d i t s A , B ( Ind iana) and D and has
been fo l l owed on sur face f o r 1,000 metres.
c l e a r l y de f i ned ve ins between l i n e s 10+00 W and 11+50 W. The system has been
o f f s e t t o t h e n o r t h o r r o t a t e d an t i c lockw ise by a se r ies o f n o r t h northwest
s tri k i ng f a u l t s .
S t r i p p i n g by S i l v e r Saddle Mines
The Queen Bess v e i n system t rave rses L o t 132, has been i n t e r s e c t e d by a d i t C
and f a r t h e r t o t h e west probably i n t e r s e c t e d by H a l l ' s (Tu la ) a d i t , a poss ib le
l a t e r a l e x t e n t of 750 metres.
A t h i r d v e i n system t raverses the midd le o f L o t 130.
f rom exposures on t h e Southern No. 8, 1978 Frac t ion , through t h e Lower Showing
ve in, d iscovered by S i l v e r Saddle Mines, t o a d i t E on L o t 130.
I t i s be l i eved t o cont inue
Black shows the Treasure Mountain F a u l t t r a v e r s i n g the southeast corner o f
L o t 132. L i t t l e e x p l o r a t i o n work has been done i n t h i s area.
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0 30 60 - S C A L E I N FEET
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r
0
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\O 5 0 1 0
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1 1
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Assays and v e i n desc r ip t i ons a r e l i s t e d i n Tables I V , V & VI.
I n fo rma t ion on t h e a t t i t u d e and s i z e o f o reshoots i n the Summit Camp i s
meagre. The M i n i s t e r of Mines, B . C . , Ann. Rpt., 1926 r e f e r r i n g t o Level 2 , S i l v e r Chief working, Treasure Mountain, mentions two ore shoots o c c u r r i n g
e i t h e r s ide of a porphyry dyke. inches wide, t h e o t h e r i s 30 f e e t long, 10 inches wide and extends up d i p f o r
a t l e a s t 25 f e e t . mentions a f o o t w a l l o reshoot 120 f e e t long and about a f o o t wide.
another o re shoot ,cu t by a ra i se , extends 100 f e e t up d i p and i s 2 f e e t wide.
One i s 160 f e e t long and between I and 12
Black (7952) r e f e r r i n g t o Level 3 o f t h e same working West o f t h i s
Surface e x p l o r a t i o n work dur ing 1985 on Treasure Mountain by Huldra S i l v e r I nc . i s be l i eved t o have loca ted oreshoots more ex tens ive than those mentioned.
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TABLE I V
CURRENT CLAIM
L o t 132 (91 uebel 1 )
L o t 93 ( S u t t e r )
LOCATION
Stream c u t , between upper and lower a d i t s
Upper a d i t, e l . 5,205 ft.
I n t e r s e c t i ons e a s t o f upper a d i t ( A )
Upper a d i t ( A ) p o r t a l
Lower a d i t (D) e l . 4,990 ft.
Ind iana a d i t ( B ) e l . 5,360 ft.
REFERENCE
Black, 1952 P. 131
I I
MPH I V Table Sept. '83
Janes Oct. '85
Black, 1952 P. 131
Black, 1952
BLUEBELL V E I N SYSTEM
WALL ROCK DESCRIPTION OF VEIN SYSTEM (LODE)
Ag Pb Zn Au Width o z ( s ) / t o n $- % o z / t o n
Q v e i n 1 ft. 1.8 1.1 14.4 - Q s t r i n g e r 1 f t . 2.1 0.6 1.7 - A r g i 11 i t e 4 f t . no sample
Agglomerate Fol lowed f o r 90 ft. Two Q lenses seen, each up t o 3 i n s . wide and few f e e t long, some sulph ides present , low grade, n o t sampl ed.
Brecc ia , cong. DH 83-1: 0.5 metre 2.0 1.1 4.7 - Cong 1 omera t e 83-4: 0.3 I' 0.3 0.2 0.7 - cn
I
d Cong. a rg . 83-2: 0.5 I' 1.1 0.6 7.0 - I I 83-5: 0.3 I ' 21.2 4.4 10.7 - I
Aggl omera t e 7 f t . 7 i n s . 5.5 1.0 4.6 0.001
A r g i 11 i t e S t r i p p i n g by SSM suggests t h a t a d i t passed t h r u main v e i n s t r u c t u r e and d r i f t f o l l o w e d a p a r a l l e l sub- s i d i a r y v e i n marked by gouge, i n c h o r so wide and sparse ly m i n e r a l i z e d . Vein m o s t l y 1 i n . wide i n western s e c t i o n .
Lode p a r t l y exposed f o r 100 ft. up s lope f rom p o r t a l . Vein system c o n s i s t s o f severa l narrow s t r i n g e r s separated by gouge and bleached p y r i t i s e d r o c k . S t r i n g e r s c o n s i s t o f su lph ides and minor carbonate and Q.
P o r t a l : Au - Zn - Pb - - ! ! % Width
41 i n s . 5.8 3.6 7.6 -
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TABLE I V (Continued)
CURRENT CLAIM LOCATION REFERENCE WALL ROCK
L o t 93 Ind iana a d i t (B), Black, ( S u t t e r ) 1952 ( Con t I d ) e l . 5,360 ft.
Underneath MPH A l te red dyke Ind iana a d i t Table I V ,
Sept. '83
I nd i a na Janes T u f f ( ? ) a d i t p o r t a l Oct. '85
Rock c u t Janes above Ind iana Oct. '85 a d i t
Shaf t Black, Agg 1 omera t e e l . 5,790 ft. 1952 w i t h t u f f
P. 133 & a r g i l l i t e
DESCRIPTION OF V E I N SYSTEM (LODE)
- ! 9 Width Zn & - Pb - Vein system fo l lowed f o r 240 ft. Veins a few i n s . wide, i n places on ly gouge f i l l e d s l i p s . p y r r h o t i t e ) :
Sampled i s o l a t e d su lph ide lens ( inc ludes
17 i ns . 8.5 4.2 5.3 - Sample 12 ft. from face:
24 i ns . 2.6 1.9 5.0 - DH. 83-6 2.5 metres 0.7 0.5 1.2 -
83-7 0.5 I' 0.4 1.4 0.4 - and 0.9 I' 0.1 1.2 0.2 - I
-1
w
5 ft. 8.4 5.7 11.3 0.010 I
4.5 ft. 8.4 7.7 3.7 0.005
Vein system 15 ins . wide. s t r i n g e r s composed o f sulphides & Q. Gouge and w a l l rock amount t o 50%. Vein system t raced west f o r 500 ft. i n open cu ts . Composed o f v e i n a few ins . wide o r gouge f i l l e d f r a c t u r e . 300 ft. east o f s h a f t a r e several narrow s t r i n g e r s i n zone up t o 3 ft. wide.
Consists o f several
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TABLE I V (Continued)
CURRENT CLAIM LOCATION
L o t 93 Trench, 1 OOm. (Shu t te r ) WNW o f
Ind iana a d i t (B) p o r t a l (1 4+70W ,
2+05N)
Trench, 125rn. WNW o f Ind iana a d i t (B) p o r t a l (1 5+00W , 2+1 ON )
4
I I
REFERENCE
MPH Drawing 14, J u l y 1983
WALL ROCK
Volcanic sands tone & a r g i l l i t e
Volcanic sands tone
DESCRIPTION OF V E I N SYSTEM (LODE) Pb - t l s Width -
F a u l t 1.2 metres 16.0 10.6
F a u l t 0.2 metres 5.5 4.8
Zn 1.7 -
1.7
Note: Elevat ions a r e those g iven by Black, 1952.
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TABLE V
QUEEN BESS V E I N SYSTEM
CURRENT CLAIM LOCATION
L o t 132 Upper a d i t (B lue B e l l ) e l . 5,435 ft.
II Lower a d i t e l . 5,250 ft. East o f lower a d i t
II
II Lower a d i t
, h b e r t y , west o f L o t 132
II
REFERENCE
Black, 1952 P. 131
MPH Table I V Sept. '83
Janes Oct. '85
Black, 1952
WALL ROCK DESCRIPTION OF V E I N SYSTEM (LODE)
- Fol lowed f o r 15 ft. Not m i n e r a l i zed
A r g i 11 i t e Fol lowed f o r 125 ft. Not m i n e r a l i z e d , about 2 i n s . gouge i n s l i p .
Conglomerate - 1 1 9 - Width Pb - An &I PPm PPm PPm PPb
DH 83-8 0.6 metres 0.8 52 1060 10
A d i t s t a r t e d on two m i n e r a l i z e d shears, 4 f t. a p a r t . Dump m a t e r i a l composed o f a r g i l l i t e , and a l t e r e d i n s t r u s i v e ( d i o r i t e ? ) . s p h a l e r i t e and d isseminated p y r i t e and galena a r e present .
Massive p y r r h o t i t e and
- P i t s show v e i n 12 i n s . wide, i n one p i t s u b p a r a l l e l s t r i n g e r s inc rease w i d t h t o 36 i n s .
Above Hal 1 ' s o r Tu la a d i t 1952
Black,
P. 132
- F a u l t zone 3 ft. wide, severa l s l i p s and v e i n 6 i n s . wide. Vein c a r r i e s su lph ides, p y r i t e i s abundant i n w a l l s o f some s l i p s .
II H a l l ' s o r A r g i 11 i t e Fol lowed f o r 65 f t. Tu la a d i t 84 t u f f Cent ra l p a r t 12 i n s . wide, c o n s i s t s o f v e i n m a t e r i a l e l . 5,530 ft. and p y r i t i s e d bedrock.
East f a c e o f d r i f t : - Pb Zn Au
Width oz(s 7 - t o n X $- oz/ton 10 i n s . 7.6 3.9 15.2 -
Toward west l o d e s p l i t s and l e s s w e l l m i n e r a l i z e d .
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TABLE V I
CURRENT CLAIM
L o t 130
L o t 130
Probably on L o t 130, c lose t o eastern boundary
II
L o t 130
LOCATION REFERENCE - WALL ROCK
Lower showing Janes Arg i 11 i t e 3+30N, 8+59W
Lower showi ng , DH 85-2
Dump A 3+30N, 8+80W
Dump B, 3+45N, 8+67W
A d i t E 4+40N, 14+20W
Janes Arg i 11 i t e
MPH , ? Table V I I , Nov. '83
II ?
MPH ? Table V I I , Nov. '83
Southern Vein i n Black, No. 8, 1978 creek bed P. 130 F rac t i on e l . 4,630 ft. ' 52
Arg i 11 i t e ?
DESCRIPTION OF V E I N SYSTEM (LODE)
Sulphide vein, 8-12 i n s . wide, exposed f o r 115 f t . , i n f l o w i n g creek, n o t sampled. Main ly spha le r i t e , galena and p y r i t e w i t h minor quar tz .
I n t e r s e c t i o n a t 80 ft. below surface, Q ve ins and disseminated sulphides, low grade, n o t sampled.
Grab sample, h igh grade galena m i n e r a l i z a t i o n .
I t II II
Galena, p y r i t e 5 p y r r h o t i t e , c h a l c o p y r i t e i n minera l i zed f a u l t zone, approx. 15 cms. wide, grab sample.
Zn Au % oz/ton - Pb Width
0.15111. 0.72 0.5 3.7 0.04
Vein 4-6 i n s . wide, s t r i k e s 20°, d i p s teep ly eastward, composed o f wh i te carbonate, galena and minor spha le r i t e , cha lcopy r i t e , qua r t z and p y r i t e .
5 i n s . 99.4 50.3 5.0 -
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REFERENCES
Cairnes, C. E., 1922
Monger, J . W . H., 1969. Geol Sur. Can., Paper 69-47. Monger, J . W . H., 1985 Geol Surv. Can., Paper 85-1A, p. 349-358.
Geol. Surv. Can., Summary Report, 1922, Pa r t A, p. 88-107.
MPH Consul t ing, 1983 P r i v a t e r e p o r t s f o r Unicorn Resources Ltd. , dated September 20 and November 24, 1983.
M i n i s t e r o f Mines, B. C., Ann. Repts. 1899, p.742; 1901, p.899; 1914,
p.226-232,245; 1918, p.208; 1920, p.172; 1922, p.180; 1923, p.166; 1924, p.188-189; 1925, p.210- 211; 1926, p.233-28; 1927, p.254-255; 1928, p.265-
268; 1929, p. 278-279; 1930, p.214-215; 1931, p.129- 130; 1932, p.139; 1952, p.119-134; 1953, p.103; 1954, p.111-113; 1955, p.39; 1956, p.71; 1957, p.32; 1970, p.381.
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- 22 -
CERTIFICATE
I, Richard H. Janes o f Vancouver, B r i t i s h Columbia do hereby c e r t i f y :
1. That I am an independent q u a l i f i e d min ing g e o l o g i s t w i t h an o f f i c e a t 418 - 602 West Hast ings S t ree t , Vancouver, B. C. V6B 1P2
2. That I am a r e g i s t e r e d Pro fess iona l Engineer i n the Province o f B r i t i s h Columbia and Member o f t he Canadian I n s t i t u t e o f Mining and Me ta l l u rgy .
3. That I have p r a c t i s e d my p ro fess ion f o r t h i r t y years.
4. That I have no d i r e c t , i n d i r e c t o r con t ingent i n t e r e s t s i n Minera l Lease 94 nor i n any minera l p r o p e r t y w i t h i n t e n k i lomet res o f t h i s lease nor do I have any i n t e r e s t i n nor any assoc ia t i on w i t h S i l v e r Saddle Mines L td .
5. That I spent th ree days examining the Minera l Lease from 19th t o 21st October, 1985.
6. That I hereby consent t o t h e p u b l i c a t i o n o f my r e p o r t e n t i t l e d "Report on Min ing Lease 94, Similkameen Min ing D iv i s ion , B r i t i s h Columbia", dated December 18, 1985 i n a prospectus o r statement o f ma te r ia l f a c t s .
R. H.
I .
Vancouver, B. C. December 18, 1985
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APPENDIX I
D R I L L LOGS,
HOLES 85-2, -3 and -4
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Silver Saddle Mines Ltd. (1985) DIAMOND ORILL RECORD Hole NO. Sheet No. *.d. :
,
,
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Silver Saddle Mines Ltd. (1985) DIAMOND DRILL RECORD ,.e*+-- - *n Hole No.
Sheet No. . - ’ sf
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I I I I I I I I
1
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Sllver Saddle Mines Ltd. (1985) DIAMOND DRILL RECORD
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Silver Saddle Mines Ltd. (1985)
fk-0 from To DL 3CAIPTlOH
DIAMOND DRILL RECORD I
&tern Au Ag Cu Pb 2n From 10 L.wh oz/ t o r / t x x x
Hole No. c?5- /#. Sheet No. 6 At3 ,
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Silver Saddle Mines Ltd. (1985) DIAMOND DRILL RECORD Hole No. RY-- Sheet No. ,f. *,f-'*
!
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APPENDIX I 1
ASSAY CERTIFICATES
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ACME ANALYTICAL LABORATORIES LTD. DATE RECEIVED: NOV 18 1?85 E52 €.HASTINGS ST.VANCOUVER B.C. V6A 1R6 FHONE 25:-3158 TELEX 04-53124 DATE REPORT MAILED:
ASSAY C E R T I F I C A T E
TTFE: RCCK CHIPS ~ u t 10 S R A ~ FEGULAR ASSAY
.DEAN TOYE OR TOM SAUNDRY. CERTIFIED B.C. ASSAYER
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Analysis Certificate Analytical Services. Trail. I3 C
SN87 840831 6837 SILVER SADDL LOT C t Y E ORE (2 TRUCK)
HZO AU AUCCORR) AG A G ( C 0 R R ) CU Pa ZN x OZ/TON OUTON OZ/TON OUTON % x x 4 .a 8.817 8.817 - 4.25 4.25 8.20 2.2 8.2
s102 AL203 FE CAO sa AS a1 x x x x x x x
__ 26.7 -~ 8.1 22.s ~ e.8 . (0.8% 8.75 8.845
Cenllicate Number 10 10281 Page 1 END CERTIFICATE
Original
corninno c Y r Ma Dy 8 4 09 28
S x 17.5
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December 20, 1985
In Account With: Silver Saddle Mines Ltd. 16 -2971Qu-Appele Street Victoria, B. C. V9A 1V3
Professional fees for field examination of Mineral Lease 94, logging core from drill holes 1985-2,-3 and -4 , preparation of report on property and travel time.
Nine days at $350 per day Report Expenses: Draughting
Other Expenses as listed: Typing and Copying
Advance Account Outstanding
$3,150.00 270.00 200.00 194.49
$3,804.49 4
1,500.00 $2,304.49
Thank you for your patronage,