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I I I I 1 1 1 1 1 I I 0 I I I c I I I
BAPTY RESEARCH LIMITED 606 Trail Street
Kimberley, B.C. V1A 2M2 Fax (604) 427-2006
Tel (604) 427-7631 Tel (604) 426-6277
ACTION:
F?tE NO:
GEOCHEMICAL SURVEY REPORT
ON THE
LAPOINTE CREEK PROPERTY
BOB AND ROSE MINERAL CLAIMS
F T . STEELE/SLOCAN MINING D I V I S I O N
NTS 8 2 F / 1 0 E // 1 5 E
4 9 O 4 5 ' N L a t i t u d e 1 1 6 O 37' W L o n g i t u d e
PREPARED FOR OWNER AND OPERATOR
I I 1
December 12, 1990
( 4 ) ( 6 )
(2)
Copies - Greenstone Resources - Dragoon Resources - Assessment Reports (EMPR) (4) - File
.. ... . .. . ~.~ . . . . . ~ ~
TABLE OF CONTENTS
1
SUMMARY OF WORK AND RECOMMENDATIONS
INTRODUCTION
2.10 Location and Access
I 2.20 Physiography
. ,
2.30 Property
2.31 Geological Target
2.32 Claim Group and Status
2.40 History
2.50 1990 Program
3.00 GEOLOGY
1 1 , 3.10 Regional Geology
3.20 Property Geology
3.30 Mineralization
4.00 1990 GEOCHEMICAL SURVEY E .I 4.10 Zinc
4.20 Lead
4.30 Other Elements
4.40 Rock Samples
CONCLUSIONS
STATEMENT OF COSTS
QUALIFICATION STATEMENTS
8.10 Consulting Geologist and I Qualification Author I s
8.20 Engineer and Program Supervisor's Qualification
Page
1
2
2
2
3
4
4
4, 6 8
9
9
12
13
14
15
16
17
17
18
19
.20
21
LIST OF TABLES
I I 1 I 1 I
Table 1 Formations & descriptive lithologies of the Rose Pass area
Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7 I I
LIST OF FIGURES
Property Location Map
Claim Map and Index Map
Regional Mineral Occurrence Map
Regional Geology
Plan of Surface Features, Geology and Grid
Plan of S o i l Survey for Zinc
Plan of S o i l Survey for Lead
LIST OF APPENDICES
Page
10
3
5
7
11
In Pocket
In Pocket
In Pocket
APPENDIX I Bibliography
I APPENDIX I1 Petrographic Report by Vancouver Petrographics Ltd.
APPENDIX I11 Geochemical Analyses Certificates
APPENDIX IV Statement of Work I I 1 I 1 I I
_. ...... ” ._...,, . ._._.._.,___I: .,._,.._....._ ., ...... .. . . _ . ^ _.. d.*4...*-.4..L.-&r
1
1 1 - 0 0 - SUMMARY OF WORK AND RECOMMENDATIONS
The Lapointe Creek property, consisting of the 12 unit Bob and 6 unit
Rose claims, is located at Rose Pass 4 4 kilometers west of Kimberley and
2 4 kilometers east of Ainsworth in British Columbia. The property is
located within the Kootenay Arc, a geologic sub-province which has seen
numerous historic mineral producers. The claims cover an old
silver-lead-zinc showing known as the Macrob prospect and selected
samples from these workings have returned assay values up to 26.8 oz/ton silver, 13.1% lead and 7.2% zinc.
Work in 1990 has partially outlined a strong and continuous lead and zinc soil anomaly some 1300 meters long and up to 250 meters wide.
Other smaller and discontinuous soil anomalies in lead and zinc occur
within the surveyed area one of which coincides with the Macrob shaft
area. The cause of the main large anomaly, which is still open on both
ends, has not yet been determined.
A program of geologic mapping, expanded s o i l geochemistry, geophysics,
backhoe trenching and diamond drilling will be required to properly
evaluate the very favorable results obtained to date.
. ... .
2 . 0 0 INTRODUCTION
. ... - . .. . ..-- -. .̂ . . , . . , _. . . ,-,_-,.
2 .
2.10 Location and Access
The Bob and Rose mineral claims are located at Rose Pass, 4 4 kilometres
west of Kimberley and 2 4 kilometres east of Ainsworth. The
claims straddle the height of land which separates the Fort Steele and
Slocan Mining Divisions (Figure 1).
' The claims are geographically situated at Longitude 116O 37' W, Latitude
4 9 O 4 5 ' N.
Access is by good gravel logging roads west from Kimberley or east from
Crawford Bay on the east side of Kootenay Lake.
2.20 Physiography
The Rose Pass summit forms the divide for Kootenay Lake and Lake
Koocanusa, both of which are part of the Kootenay River drainage.
The Bob and Rose mineral claims have alpine and subalpine terrain with
forests of larch, pine, fir and cedar to 6500 feet (1981 m).
Rainfall and snowfall levels are above average with reported snowfall
reaching 5 . 0 metres. The property is typically free of snow between May
. and October.
S C A L E 100 0 100 400 km
0 200 miles
3
PROPERTY LOCA TION
I ' LOCATION MAP
4
1 Bob I 12 I 3618 1 Ft. Steele Rose 6 6124 Slocan
2 . 30 Property
2 1/ 09/8 9 2 51 09/89
2.31 Geological Target
-The Lapointe Creek property is located within the Kootenay Arc mineral
province where silver-lead-zinc vein systems typically have grades of
300-900 gm/t silver, 4-8% lead, and 2-4% zinc (Sangster, 1984) and sizes
up to one million tons. The nearest producer is Cominco's now dormant
Bluebell operation, 17 kilometres west of the claims, which produced a
total of 4.7 million tonnes of lead/zinc ore grading 14% combined metal.
L
-
2.32 Claim Group and Status
The Bob and Rose mineral claims (Figure 2 ) were staked by C. Kennedy and
S. Sanders in October, 1989 and were subsequently transferred to South
Kootenay Goldfields Inc. Claim data is summarized as follows with the
due date reflecting the work already filed and covered by this report:
I NO. I RECORD I MINING RECORD I CLAIMNAME U N I T S NO . D I S T R I C T I DATE
~~~ ~
2.40 History
--The West Kootenay region of British Columbia has a long mining
4 1992
history,
with most of its production from the Kootenay Arc, an arcuate shaped
structural zone which includes numerous former mineral producers and
showings.
I I I I I I I I I I I I I I I I 1 I I
5
49O42'
SCALE
0 500 2000 3000
metres 5 I--- CLAIM
I MAP BOB & ROSE MINERAL
CLAIYS N.T. S. : 82 N 10E // 15 E I SCALE: 1'60,000
.. . .
I 6
I The north section of this arc includes the Ainsworth and Bluebell
deposits.
Production in the Ainsworth camp between 1892 and 1964 involved some 50 I I properties totalling almost 700,000 tonnes. Mineralization typically
I ' consisted of native silver, argentiferous galena and sphalerite in
fissure veins. Tin and fluorite are mentioned as accessory minerals
(Schofield, 1920).
'In 1890, the Bluebell limestone deposit was discovered on the east shore
of Kootenay Lake across from Ainsworth Hot Springs. Argentiferous
galena and sphalerite in fractured lower Cambrian Badshot - Mohican Formation was the target of extensive exploration and underground
development by Cominco Ltd.
14% lead and zinc ore before closing in 1975 due to the high cost of
pumping water from the workings.
East of Crawford Bay, lead-zinc veins similar to those at Ainsworth
were the target of small scale operations in the Canyon Creek and Rose
Pass areas.
Just northeast of Rose Pass on the Bob claim, a 0.3 m quartz vein is exposed in a small creek. Some 30 meters to the south, this vein was
explored by the old Macrob Shaft. During 1989, South Kootenay
Goldfields' personnel examined the vein showings and shaft dump, and
completed limited geological mapping. The shaft is full of water and
I I I
This deposit yielded 4.7 million tonnes of
I 1 I I 1 I inaccessible. This work established that silver-galena-sphalerite
mineralization occurs within a metamorphosed argillite immediately
1 adjacent to a unit of rhyo-dacite crystal tuff.
1 I -f-
rr)
SCALE I O 2 4 6 8 IO 12 14 16
k i lometres
2 m , m IW ...: ..................... h. h.4
Y ILC uw IAGUI.'OU'R YmJ... 4.4.11*1 $4 IOLYS CPltD., R44 ........... i h. L.
'Y "Ukm m u m fGol ........... b.4. h
0 l a y 1 ............................... h . 4 Y Io*y. VILLn w ................. *..I)
s -'w nuI ..................... c
....................
. .
I . . 'n )ICO ..._ ~ ......................... .. w m VAL us Po. M q ............. *. L n muon. ulnwetu ................ 6. n YO ~vvco, 08 .................. L. 1.
.............................. h.L.
A G U Y Ultl ......................... f. .
s n.l-. mom a m UUQ ..: ..................... ..................... 4.h.L. 4.b.2. s )u11001 ............................ A(i h. L rn warn Cows ............ : ......... 4. Am. h. za
...(............. L . . . G . X
....
iia c u w m m u. munun sum... D.W-
114 cuwmm a. owrain awuv .. &r.i*
11s KGUG .............................. m
'III m w nm .......... :..: ..... 1 ..... h..lr
118 umP*mn# ....... ! ................ NI. c.. n. N 11s WIS rmo ......................... br . C.
ia mslyli - 1 y u o r ...... h . L . . b ( l
'I, 1IUI*mII.: ....I ................... 4.h. ?a
11s w DO," ........................... y. im YO 3 ............................... f.
111 sim .................................. L*
in NU ....; ............................ 4. 6. L.
....... ...... IP UwUL-ulm ...... % , L . . . & . . C .
111 lllt DfANlALL OVfR). ....... %.h& 136 t C W Y ................ h .I37 )(RYAN1 ............... .cu
SOUTH KOOffNAT OOCOFlLLOS IUC.
REGIONAL
MINERAL OCCURENCE MAP
BOB & ROSE MINERAL CLAIMS
N.T.S. :82 N N E SCALE: 1:125,000 M.D. : Ft. Steele/Slocon O N E : Oct/89 t10. :3 DRAWN: B. K.
1 I I 1 I D I I I I I I 1 I I I D D I
8
2 . 5 0 1990 Program
I
The 1990 Program was designed to geochemically prospect the area
surrounding the old showings and workings at the Macrob shaft and
consisted mainly of a geochemical soil sampling survey totaling 375
samples. There were 10.4 kilometers of lines established by flagging
while the soil samples were being collected. Seven rock samples were
collected and assayed and two of these are the subject of a petrographic
study and report which is-included in this report.
of reconnaissance work completed on the property by consulting
geologists.
soil sampling program and collect the rocks for the petrographic study.
One day was spent on the property in October by the writer to assist in
preparing the maps and text for this report. The program was done under
the supervision of Michael Bapty, P.Eng. of Bapty Research Limited which
was the consulting and contracting firm.
There were two days
One day in July was spent by Peter Klewchuk to plan the
1 I I 1 I I I I I I I I I I I I 1 I
9
3 .00 GEOLOGY
!
3.10 Regional Geology
In the Crawford Bay - Rose Pass area, intensely deformed Precambrian metasedimentary clastic and carbonate rocks of the Dutch Creek, Mount
Nelson, Toby and Horsethief Creek Formations form a linear northeast
trending belt (Table 1).
Cretaceous quartz monzonites to diorites are in part responsible for the
levels of deformation and metamorphism evident in the Rose Pass area.
Foliation in the sediments follows batholith margins with metamorphic
and deformational intensity increasing towards the batholith contacts.
The contact zones are generally gneissic with included lineated
fragments of metmorphosed sediments.
Numerous minor felsic and lamprophyric intrusions are prevalent
throughout the region, typically in silicified structures which parallel
foliation; their occurrence is commonly coincident with galena,
sphalerite and tetrahedrite.
1 I 1 I I I I I I I I I I I I I I I I
PRECAMBRIAN
WINDERMERE
0 limestone, arkose, pebble conglomerate HORSETHIEF CREEK FORMATION Green, argillaceous quartzite; blue-gray
TOBY FORMATION Conglomerate
UPPER PURCELL
0 quartzite MOUNT NELSON FORMATION Laminated argillite, magnesian limestone,
DUTCH CREEK FORMATION Laminated argillite, magnesian limestone, U quartzite
LOWER PURCELL
U and argillite; calcareous quartzite KITCHENER-SIYEH FORMATION Chiefly vari-coloured magnesian limestone
T a b l e 1 Formations t descriptive lithologies of the Rose Pass area
i r ,
. .
.Y
., . ,- i _. .I,
. . . . . . . . ' e ' ' , . , .. ., . . . . . . . . . . . . . . . .
0 500 2000 3000
metres 9
CRETACEMIS?I
CRETACEOUS
JURASSIa?)
i
Dolomite, 11110 Q d u k grey, buff or bram wearharng
Black ugrulte .rd u g r l 1 v c o u s grey Y I U l m e . Uun-beaded
Dolomite, dolomitu ulutone. ugilhre
while a green. ~hlc*-bCddd quutrae
I F LOVER CRESTON; thm-bcdded dark ugillrte W grey s~ltstone chuacnrlred ay wregulu pinching d iwellrng beds. ripple cros-I.miNiiOn. mUI-crvks. mimr c u i and Lll feanueu green d u l w wilh Uun mrerbmi of ugrulre. - Au.wxemRnAno*; d i v i d e 4
regular. white lunirue of siltston.
UlDDLE ALDRIDGE: light grey wearhering. grey quutrrre W IDIOM UI beds
LOWER ALDRIDGE rusty weathering, laminated or c r o u - W e d quutrrre. argillrte W ulw argtllrte.
........ CI--*O.LIm..N-..-.rO.. . . . . . 9. - _-' I
I*)~Uc".ul.TULl.rr-rm.. - + i + f ync"-(.dl.. i
LIul"(rL -0. . . . . . . . . . . . . . . . . + I '
............... - (LL .n.& . . . . . . . . . . . . . . . . .
...................... t W I I
RinU.O.L-.-O ..... i ....... ...,e-
h . , * U . O . L L 9 m , ~ .......... - & A - .-L
u - u - . I L M L I L . I d Y ) . .... ,..--n-.tr*ry.) ........... ++ *.. . .*l .n-.t . .~u~.~. . ......... + --f - U L L . l . l m , ~ * U l r - . l . . .... -ft- -e- ----. lrYIY.(.. . . . . -+ * . . . . . . .
REGIONAL GEOLOGY BOB 8, ROSE MINERAL
CLAIMS #.T" : 82 F/lO E /ASE
a0. : Ft.Steele6loCan OUTg : oct/89 SCALP: I: 50,000
ma :4 DRAWu: B:K.
12
I 3.20 Property Geology
I I I
The Bob and Rose claims straddle the geological boundary between the
- Mount Nelson Formation and the Horsethief Creek Group (See Table 1,
p.10).
4 .
has been noted on Figure 5.
The contact trends NNE through the property as shown in Figure
The property has not yet been geologically mapped but some outcrop
An outcrop of flat lying phyllite belonging to the Horsethief Creek
Group occurs at 4+00S, 0+60W where an old side hill cut has exposed a
conformable 15 cm quartz vein carrying sphalerite.
outcrops of black argillite belonging to the Mount Nelson Formation
which form very steep bluffs trending N25OE along the entire 1400 m
length of the grid, and lying east or down slope from the baseline.
Bedding in the argillite is variable from N20°-400E.
-1 I 1
There are prominent
The dip varies
steeply to both the northwest and southeast.
contains up to 2-3% disseminated pyrite giving it a gossanous appearance
on weathered surfaces.
3+10S, 1+80E, presumably interbedded with the argillite unit.
A unit of rhyo-dacite crystal tuff occurs near the Macrob shaft
and may be related to sulphide mineralization seen at the site.
Locally the argillite
One outcrop of white dolomite was noted at I ’ I
It
I ~ weathers a chalky white color, is weakly calcareous and contains 2 mm
diameter quartz eyes, specular hematite and spots of limonite and
manganese stain. A thin section of this rock type is described by the
Vancouver Petrographics Ltd. report in the Appendix, Sample No. 52757. I
13
I 3.30 Mineralization
The main known showing on the property is located at the Macrob Shaft
which is situated at 1+20N, 0+45E on the grid (See Figure 5).
is exposed in a small creek about 30 meters on strike N24OE from the . shaft. The shaft is full of water and an old sloughed-in hand trench
The vein
I 1 trends from the shaft to the creek showing. Highgrade lead-zinc
mineralization in quartz on the dump attests to the vein's presence in '1 the shaft.
The vein in the creek bottom is up to 0.3 meters wide and occurs just
within argillite adjacent to the felsic tuff described above.
Mineralization there and from the Macrob shaft dump consists of
sphalerite, galena and pyrite with minor arsenopyrite and chalcopyrite.
Gangue minerals are mainly quartz with minor sericite.
Petrographics Ltd. report in the Appendix provides a detailed
description of the minerals and alteration in sample No. 52756 from the
shaft dump. Selected samples from 1989 sampling returned assays up to
26.85 oz/ton silver, 13.11% lead, and 7.18% zinc. Traces of bismuth,
tin, tungsten and cadmium were also found to be present. The galena
occurs along vein fractures and in fracture fillings up to 1 cm thick.
Disseminated to massive sphalerite is concentrated in the vein at the
I I
The Vancouver
I I I hangingwall contact.
1 The geologic contact between the rhyo-dacite crystal tuff and the
argillite may be an important control to mineralized vein systems.
..,_ " . .. ... '~..>*,.
14
I 4.00 1990 GEOCHEMICAL SURVEY
The 1990 program consisted of a soil sample survey over a 600 x 1400
meter grid centered near the Macrob shaft. The baseline had a bearing
of N25OE, parallel to the bedding and formational contacts. Silver,
lead and zinc mineralization occurs at the Macrob shaft and the program
was designed to explore for parallel and on strike ore deposits.
Soil sampling was conducted on lines 100 meters apart and at stations
every 25 meters along the lines. Samples were collected from
approximately 15-20 cm deep where possible with the object being to
collect below the grass roots. horizon was normally sampled. Sampling was done on September 12-14,
1990, by qualified soil samplers, Stephen Sanders and Gerard Roy.
The samples were placed in paper soil envelopes and delivered to Acme
Analytical Laboratories Ltd. of 852 Hastings St., Vancouver, B.C. The
375 samples were analyzed by ICP for 30 elements. Geochemical analysis
for gold was done by fire assay preconcentration followed by an atomic
absorption (AA) determination on 308 samples. Gold analysis on the
'other 67 samples were done by acid extraction followed by AA.
samples were dried at 6OoC and sieved to -80 mesh.
was digested in hot dilute aqua regia in a boiling water bath and diluted to 10 ml with demineralized water. Then 30 elements are
determined by inductively coupled argon plasma (ICP) . With acid
extraction of gold a 10.0 gram sample is ignited overnight at 6OO0C and
then digested with 30 mls of hot dilute aqua regia.
clear solution obtained is extracted with 5 mls of methyl isobutyl
ketone (MIBK). Gold is determined in the MIBK extract by AA using
1 I
Due to poor soil development the C soil I 1 'I
I '1 ' m 1
The
A 0.5 gram sample
A 75 mls portion of
. ... ."<. .-*... -
I I I ,I I 1 I I 1 I 1 I 1 I I I 1 1
I 5
background correction to a detection limit of 1 ppb.
!
In the other gold determination a 10 gram sample is subjected to fire
assay preconcentration technique to produce a silver bead.
1 - bead is dissolved and gold is determined in the solution by graphite
furnace AA t o a detect ion l i m i t of 1 ppb. the Appendix of this report.
The silver
A l l r e s u l t s are included in
4.10 Zinc
The most extensively anomalous element of the survey is zinc.
metal forms a continuous moderate anomaly for 1300 meters through the
eastern part of the grid for its entire length, except for the last line
north (L600N). Results are shown on Figure 6 and the anomaly has been
contoured at 100 and 200 ppm. This anomaly is open at both ends,
running off the grid to the south at L800S and off the east edge of the
grid at lines 400N and 500N. Values above 200 pprn form a more or less
This
continuous anomaly along its entire length and contouring at the 100 ppm
level results in widths up to 250 meters. Seven stations returned
results higher than 400 ppm and these are fairly well distributed along
the anomaly.
zinc soil anomaly and the prominent steep sloping outcrops of black
argillite trending along the eastern side of the grid. The cause of
this main anomaly has not been determined, however a narrow +lo0 ppm
contour spur splits off the anomaly at LlOON, 0+50E, trends through the
Macrob shaft showing and parallels the north part of the main anomaly
for 400 meters.
There appears to be a spatial relationship between the
4.20 Lead
A lead soil anomaly, as defined by
generally with the 100 ppm contour
generally weaker in the north half
16
the 50 ppm contour, coincides
of the zinc soil anomaly but is
of the anomalous zone (See Figure 7 ) .
The southern 700 meter portion of the lead anomaly exceeds 100 ppm and
the southern 200 meters is sharply defined and exceeds 200 ppm.
This lead anomaly generally lies over the southeastern and downslope
half of the zinc anomaly.
the upper portion of the zinc anomaly.
Several isolated 50 ppm contours'lie along
A trend of parallel but erratic values as defined by the 50 ppm contours
lies just northwest of the main anomaly.
spur of the zinc anomaly which passes through the area of the Macrob
Shaft showings, but appears to discontinuously trend through the whole
grid. The lead anomaly is open to the south at L800S and trends weakly
off the northeast edge of the grid at lines 400N and 500N.
is less mobile than zinc the strong values at the south end of the grid
may indicate the area of greatest potential.
Valley, centered about 1,000 meters to the southeast, is an old cirque
with the dead glaciers direction down the Lapointe Creek Valley to the
north-northeast, parallel to the anomalies. The weakening values in
lead to the north-northeast may be due to glacial dispersion.
This trend coincides with the
Since lead
The head of Lapointe Creek
17
4.30 Other Elements
Low but anomalous values in cadmium as defined by +1 ppm coincide with
the southern half of the main lead anomaly. Two erratic spots of
anomalous arsenic values from plus 4 0 ppm up to a high of 136 ppm occur
at L500S, l+OOW and LlOOS-L200S, 0+50W. These lie along the trend of
discontinuous low lead anomalies just west of the main lead and zinc
anomalies. There were a few erratic one station highs in other metals
but no other anomalous trends were disclosed by the survey.
4.40 Rock Samples
Seven rock samples were taken in July, two of which were sent for
petrographic study. The two petrographic samples were discussed under
Property Geology and a report from Vancouver Petrographics Ltd. with a
complete description is in the Appendix.
character samples taken from the Macrob Shaft dump, checking for any
unusual elements and high precious metals.
lead and zinc values were returned as expected but nothing of interest
was disclosed by the assay results. Complete assay results are in the Appendix on these samples, B52751-5.
The remaining five were
Some minor anomalous silver,
18
5.00 CONCLUSIONS
Coincident zinc and lead soil geochemical anomalies have been disclosed
by a 375 soil sample survey over a 600 x 1400 meter grid which surrounds the old Macrob Shaft and vein showings.
to the northwest and uphill from the main anomalies, but coincides with
a narrow low order anomalous trend which parallels the main anomalies.
The Macrob Shaft lies outside
The main anomalies coincide with extensive and prominent outcrops of
black argillite belonging to the Mount Nelson Formation which may be the
source of the metals. These anomalies have been defined for 1300 meters
and trend off the grid along both strike directions, approximately
N25OE. The northeast ends of the anomalies are weakening and may
reflect glacial dispersion. The southwest ends of the main anomalies are
getting stronger. Further exploration is warranted to trace the
anomalies beyond the present grid and determine their source.
r
19
6 . 0 0 STATEMENT OF COSTS I I $
Labour: Soil Sample Collection Stephen Sanders - Rate at $17.00/hr. Gerard Roy - Rate at $225/day September 12-14, 1990: Cost includes overtime amounting to one extra day for both men plus Employers payroll carrying costs plus general overhead (8 effective Man days)
2,152.50
I Transportation: 3 days x $50/day 150.00
I
Assaying : 308 x $10.10 per 3,110.80 67 x $ 8.60 per 576.20
Freight 55.65 5 (rock) x $10.75 per 53.75
3,742.65
Consultants: Peter Klewchuck - July 26, 1990 Sampling and Program design 300.00
Vancouver Petrographics Ltd. August 1990 Report 197.50
H.H. Shear - October 10, 1990 Property Examination, Map Physical Features. Data Review - October and December - 1 day 2 days x $300/day 600.00
M. Bapty - September and October, 1990
I I 1 1 I %:
3 hr. supervision x $70/hr 210.00 1,307.50
Report - Map and Text H.H. Shear - Dec. 10 and 11,1990 2 days x $300/day 600.00
I TOTAL PROGRAM $7,952.65
8.00 QUALIFICATION STATEMENTS
I I I I I 1 I I I I 1 I 1 I 1 I I I
20
8.10 Consulting Geologist and- Author's Qualification I I, Henry Herbert Shear, of 325 S. Copper Street, Greenwood, British Columbia, do hereby certify:
1. That I am a graduate of the University of Arizona with B.Sc. degrees in Geological Engineering (1959) and Mining Engineering (1960).
2. That I have been actively pursuing my profession as an exploration geologist for the past 30 years, starting as a field geologist and advancing through to the senior geologist , pro] ect manager and consulting level.
3. I am a member of the Association of Professional Engineers of
4. I examined the Lapointe Creek Property on October 10, 1990, and made
British Columbia.
a thorough review of all data prior to writing this report.
Dated at Cranbrook, British Columbia, this 12th day of December, 1990.
I I I 1 1 I I I I I I I I I I I I I 1
21
8 . 2 0 Engineer and Program Supervisor's Qualification
I, Michael Bruce Bapty, of the City of Kimberley, in the Province 0.f British Columbia, hereby certify that:
1.
2.
3 .
4 .
5.
6.
I am a Consulting Mining Engineer and Contractor at 901-Industrial Road #2, Cranbrook, B.C.,
I am a graduate of the University of British Columbia with a BASc in Mineral Engineering, and have been active in mine exploration, development, operations and administration for twenty-two years,
I am a Member of the Association of Professional Engineers of British Columbia,
This report is based upon property fieldwork conducted by our staff and consultants, under my supervision, from the period July, 1990 to October, 1990,
I have an indirect interest in this property through a senior consultant's (employee) stock option to acquire 45,000 shares in Draqoon Resources Ltd., and further, that my company, Bapty Research Limited directly owns 40,000 shares of Dragoon Resources Ltd. Dragoon is a 50% owner and Managing Partner of South Kootenay Goldfields Inc. which has staked the property.
I do not expect my interests to change as a result of submitting this report.
I authorize Dragoon Resources Ltd. or Greenstone Resources Ltd. to use this report in a Statement of Material Facts, or as supporting documentation as may be required by any Securities Exchange, Financial Institution, or Superintendent of Brokers.
Dated at Cranbrook, British Columbia, this 12th day of December, 1990.
A
I I I I I I I I I I I I 1 I 1 I I I 1
APPENDIX I
Bibliography
I I
1 .Kiesman, W. 1990: A Summary
Property; of Work and Recommendations on Lapointe Creek Bapty Research Ltd. Report.
Rice, H.M.A. 1944: Geology and Mineral Deposits at Ainsworth, B.C., G.S.C.
I Paper 44-13.
Sangster, D. 1984: Canadian Mineral Depo7it Types: A Geological Synopsis ,
Economic Geology Section Report #36, Eckstrand, O . R . , a. I
'Schofield, S.J. 1 I 1920: Ainsworth Mining Camp, G.S.C. Mem. 177.
"I
I I
I I I I
APPENDIX I1
Petrographic Report by Vancouver Petrographics Ltd.
r, I' I mI Vancouver Petrographics Ltd.
:I 1 I I I
JAMES VINNELL, Manager
JOHN G. PAYNE, Ph.R (3dogist
CRAIG LEITCH, Ph.D. Cieotogist
JEFF HARRIS, Ph.R ~eo~ogist I KEN E. NORTHCOTE, P1I.D. Geologist
PO. BOX 39 8080 GLOVER ROAD, FORT LANGLEY, RC VOX 1JO PHONE (604) 888-1323 FAX. (604) 888-3642
Mike Bapty Bapty Research 901 Industrial Road Cranbrook B.C. V 1 A 4 C 9 august 23, 1990 (604) 426-6277 Our file #40
Dear Mike, Re: Samples #52756 and 52757
Petrographic descriptions have been completed on Samples #52756 and 52757. (Received August 21, Completed August 22). The petrographic reports are attached.
Two unidentified (traces) metallic grains associated with chalcopyrite and galena require SEM analyses for positive identification. I suspect pyrrhotite (too brown in colour) and cubanite (birefringent lamillae). It would be o f interest to know what trace elements are anomalous in ICP analyses. If you wish SEM analyses please return the polished thin section, attention KEN.
Yours very truly,
(604) 796-2068 1 E.E. Northcote Ph.D., P.Eng.
I : - I I I I
Sample t52756 (Polished thin section) I
.I : m ; , . .
I :. ..........
' ,".I . . .
. . . . . .
. . . . .
Y I 1 I .'
Sphalerite, galena, lesser pyrite in quartz gangue.
General description
Irregular fracture controlled infilling partial replacement of quartz (sericite) gangue. Gangue is predominantly weakly crushed quartz with minor sericite partings. Very minor to traces biotite with associated feldspar(?).
Opaques include sphalerite, galena, pyrite, arsenopyrite, chalcopyrite, cubanite(?) and unidentified brown (pyrrhotite?).
I
Transmitted light Gangue; 55% (in section)
Quartz; >45%, anhedral, (to >3.0 mm), irregular interlocking crystals. Strained mottled extinction. Replaced by and containing fracture controlled galena and sphalerite.
Sericite; 5%, anhedral, (<.01 to > O , i mm), +elted to weakly foliated irregular masses.
...... .Sphene; trace,' anhedral, (0.2 mm) , subhedral. Imbedded in galena. , ,& ; . . . . . . . .
. . . . . 'Biotite; <lX, anhedral, ( ( - 0 1 to >0.1 m m ) , irregular felted .:...;;.;:-,.
. . . . . . . . . . . . . . , > ' . . . . . jl clusters associated with galena, feldspar (?I and in
' feltedlfoliated partings associated with sericite.
Feldspar/plagioclase; <<lX, anhedral, ((0.1 mm) associated with metallics.
I . Undetermined "A"; <lX, anhedral, ( ( - 0 5 to 0.2 mm), clusters of . . . . grains associated with metallics. Biaxial ( + j with 2 V .about
. , 50 degrees or less. Moderate ( + I relief. Low birefringence :'
. ' (first'order yeilow). , .
"'B"; ' trace,'' anhedral, (0.2 mm) , low relief, ' very . ' . , .
. . , . .
. ' ', .. high birefr'ingence. . . . ., . . . . .
* Reflected light
Pyrite; lo%, euhedral/anhedral ( ( - 0 1 to several mm).,As single crystal, clusters of crystal and grains and larger granular masses .
I a , I
Arsenopyrite; 5%, euhedral/anhedral, (<.91 to 0.5 mm) as euhedral grains. A s euhedral crystals in galena. Close association I with pyrite.
Galena; >lo%, anhedral ( < . 0 1 to several mm). Generally large irregular masses enclosing sphalerite, chalcopyrite, I arsenopyrite. Cutting pyrite.
Sample #52756 Continued .I
,. 'Sphalerite; >15%, anhedral, (<.01 to >1.0 cm). Irregular grain ontains blebs of chalcopyrite, galena and irregul replaced (?I masses of galena.
<lX, anhedral, ((-01 to 0.3:mm) . . in . 'sphalerite, .locallized in specific sses. Crystallographic controls.
' . %./.
(b) Blebs in galena, very local, associated with chalcopyrite-bearing sphalerite.
(c) Free grains in gangue
(d) Blebs in pyrite *-
Undetermined ? metallic E l l ; pyrrhotite(?) (traces), anhedral, (<.a1 to .04 mm) Pale brown blebs in pyrite, associated wi g a l e n a , chalcopyrite- Cut by p a l e pinkish c r e a m laths (cubmite?). Pleochroic pale brown/darker brown. Intense anisotropism. [Too deep a brown colour +or pyrrhotite1
th
Undetermined ? metallic C23; cubanite(?) (traces), anhedral, * " (<.a1 mm). Minute pinkish cream laths in undetermined
metallic 1 1 1 cutting across boundary into chalcopyrite. Not obv i ocisl y p 1 eochrr, i c . Strong ani sot rap i c .
$1 3 " . ' _ I
lerite ' ' .
entified metallic 2
Sample t52757 i
Rhyo-dacite crystal tuff I' , . I .
. ' . General description I
... . Weakly layered. Consists of two sizes, coarse and fine, feldspar . and quartz crystal fragments in a'very fine (tuffaceous) matrix . . with weak to moderate sericitic altered plagioclase and lesser
-Stained slab indicates no K-feldspar but remnant twinning e5 Na-rich plagioclase.
. .
Hicroscopic description
: Coarse crystal fragments
-.'Plagioclase; lo%, euhedral/subhedral, (0.3 to 2.0 mm), many
1 ; .i. . . . I
.; ,.. .
grains fragmental. Weak radiating sericite alteration and microgranular alteration dusting. Remnant twinning indicates composition in albite range. Also s h o w s mottled twinning pattern but no K-feldspar indicated by stained slab.
I .:. ,
*I ; . /
r .
Quartz; lo%, anhedral/subhedral, (0.3 to >1.5 mm), many grains .rounded (resorption), unstrained to weakly strained.
Lithic fragments; <5%, felted feldspathic grains, generally ((1.0 mm) . . .
. . .. .
, " Fine crystal fragments
Plagioclase;, 15%, ,anhedral, '(-05 to 0.3 mm), generally (0.1 mm), preferred orientation producing subtle
. I
layering . . , , i '
1, . ( - 0 5 to' 0.3 mm, generally <0.1 mm), fragmental. E , digseminated throughout matrix.
.!
, . . . . .
lagioclase; 30%, anhedral, ( ( - 0 5 mm), tuffaceous. flssociated with felted sericite.
. ..
.' Quartz; lo%, anhedral (X.05 mm), tuffaceous. Clearly visible as unetched grains in the etched feldspathic tuffaceous groundmass in the stained slab.
i , ,I I
Sample #52757 Continued
Alteration i
. . . . . . . . . . . Sericite; lo%, anhedral((0. 1 to ,0.1 m , .
. . . . . . . . . . . . G . ( ' . , . . . .
. . ,. e . . . : .:.
'.' (a) Groundma :bl'ades, (ge al'ly <..os mm) , ;'
feltedlweakly foliated,. Clusters o'f.grains as discontinuous foliated :partings. Masked by iron staining. Few scattered . .
. . . . .
. . . _ I :
coarser grains (to 0 . 1 . m m ) . , . '
(b) Clusters o f bladed grains (to 0.1 mm) in plagioclase fragments. .
Opaques; <l?, anhedral,, (-01 to 0.5 mm), single grains, clusters
Leached pits associated with hematite and iron 'staining.
. . . . . . . . .
of grains. . . .
'
. . . ~.
- . . . . .: . .
1 . c . . , . .
. . . i .. . .
.,' . ' . . . . , . ._
? . . ."(
. . . . ...
I I 1
APPENDIX I11
Geochemical Analyses Certificates
ACME ANALYTICAL LABORATORIES LTD. 852 E. HASTINQS ST. VANCOUVER B.C. V6A 1R6 PHONE(604)253-3158 FAX(604)253-1716 GEOCHEMICAL ANALYSIS CERTIFICATE
Bapty Research L i m i t e d F i l e # 90-2957 901 Industr ia l Road #2, Cranbrook BC V1C 4C9
B 52751 B 52752 B 52753 B 52754 B 52755
22 4 .02 40 6 .U .01 .19 11 15 .01 42 2 .19 .01 .10 29 4 . 0 9 23 2 .47 .01 .16
2 .09 .01 .w I D 1 155 3 2 1 5.30 3 7 3.14 16
ICP - .SO0 GRAM SAMPLE I S DIGESTED UITH 3UL 3-1-2 HCL-HNCU-HK) AT % DEG. C FOR W E HOUR AND I S DILUTED TO 10 ML UITH UATER. THIS LEACH IS PARTIAL FOR MN FE SR CA P LA CR MG BA T I B U AND LIMITED FOR NA K AND AL. AU DETECTIa L I M I T BY ICP I S 3 PPH. - SAMPLE TYPE: Rock A P
A;y 3/%. DATE RECEIVED: JUL 30 lop0 DATE REPORT NAILEDr
. . . . ... . - I :, . , ... , ..
- 3 . ' _ _ I , . .
. .
C-LEONG, J-UANG; CERTIFIED B.C. ASSAYERS
ACME ANALYTICAL LABORATORIES LTD. DATE RECEIVED: Aut3 9 1990
PRO=( 604) 253-3158 DATE REPORT )(AILED: 852 E. HASTING8 ST. VANCOWER B.C. V6A 1R6 I
1 - BaDtv Research Ltd. FILE # 90-2957R
FA](:( 604) 253-1716
G EOCH EM ICAL ANALYSIS CERTl Fl CATE
* , .
SAMPLE# AU*+ PPb
. B 52751
. . . ' . - SAMPLE TYPE: Rock BY ACID LEACH/M F R W 10 Gn SAnPLE.
D.TOYE, C.LEOWG, J.UANG; CERTIFIED B.C. ASSAYERS
. ... . , . .- . ., . . .. . . .. . I . I. I , . . . .. ,. . , . .... .) . I . .. . .. . . I . . . . .
. ..
I
A m ANALYTICAL LABORATORIES LTD. 852 E. HASTINGS ST. VANCOUVER B.C. V6A 1R6 PBONE(604)253-3158 FAX(604)253-1716
GEOCHEMICAL ANALYSIS CERTIFICATE
SAMPLE#
L600N 300U L600N 275U L6OON 250U L600N 225W L600N ZOOU
L600N 17% L6OON 150U L600N 125U L6OON 1OOU L6OON 75U
L600N 50U L600N 25U L6OON OOU L600N 25E L600N 5OE
L60ON 75E L600N lOOE L6OON 125E L6OON 150E L600N l7SE
L600N 200E L600N 225E L600N 250E L600N 275E L600N 300E
L500N 25E L500N 50E L500N 75E L500N lOOE L500N 125E
L500N 150E L500N 175E L500N ZOOE L500N 225E L500N 250E
L500N 275E STANDARD C/AU-S
Mo Cu F++ w p p n p p P
pa 1 15
$19 1 17 20 1 26 %4 1 49 24
BaDtv Research Limited PROJECT LA POINTE F i l e . # 90-4572 Page 1 901 Industr ial Road #2, Crenbrook BC V1C 4C9 '
. . . . . . . . . N i Co Mn Fe
PPnPPnPPn x 11 4 153 3.04 12 5 546 2.78 12 4 119 3.00 28 15 525 3.65 21 9 764 3.43
27 13 382 3.16 30 15 633 3.25 14 5 206 2.92 15 5 216 3.34 21 8 622 2.77
12 4 150 4.49 17 5 163 2.03 27 14 340 3.29 19 7 172 3.83 15 4 157 3.00
17 6 307 3.81 15 4 132 4.10 23 10 271 2.78 14 5 111 3.88 17 6 165 3.57
34 10 688 4.73 27 6 212 3.93 17 9 959 3.50 22 10 515 3.50 48 6 672 2.73
20 .!6 245 2.83 18 6 185 2.73 15 5 118 2.26 18 5 166 3.49 16 5 157 3.04
39 17 1048 3.72 20 7 237 3.38 20 8 295 3.50 15 7 368 3.46 14 5 152 5.73
17 7 567 4.90 70 32 1049 3.97
5 I D 1 10 5 N D 1 5 5 N D 1 7 8 N D 1 2 3 5 ND 1 15
7 NO 1 12 7 N D 4 2 3 5 N D 1 9 5 ND 1 13 8 ND 1 22
5 I D 2 11 5 ND 2 12 5 ND 1 17 5 ND 3 18 5 N D 1 3
5 N D 1 6 5 ND 1 20 5 ND 1 22 5 N D 3 5 6 N D 1 5
5 N D 2 4 5 N D 1 4 5 N D 1 3 5 N D 1 3 5 ND 4 4 4
5 N D 1 4 5 N D 1 3 9 N D 1 4 5 N D . 1 2 5 N D 1 3
5 N D 3 8 5 ND 1 12 5 N D 5 2 5 N D 1 3 5 N D 1 3
5 N D 2 6 20 7 39 53
B i V PPnPPn
2 24 2 26 2 24 2 21 3 21
2 18 2 17 2 20 2 24 2 20
2 28 2 10 2 22 2 20 2 21
2 24 2 27 2 15 2 28 3 20
2 16 2 17 2 18 2 18 2 49
2 16 2 16 2 13 2 18 2 22
2 16 2 15 2 12 2 18 2 20
2 21 20 58
._ La C r Mg Ba
W P P n X W
13 11 .41 32 12 11 .41 32 17 8 .24 29 74 17 .54 34 21 17 .59 29
38 17 .67 38 48 18 .67 31 9 11 .39 18
19 12 .36 19 73 16 .32 29
14 16 .29 30 14 22 .79 18 16 20 .66 46 11 19 .55 34 8 12 .46 30
11 15 .40 33 11 10 .27 34 11 18 .66 29 25 11 .19 23 46 14 .33 18
18 19 .53 25 11 20 .60 13 7 10 .35 14
10 11 .57 28 7 40 .35 83
11 12 .50 19 17 10 .37 10 35 10 .22 10 18 12 .37 8 24 12 .35 9
22 12 .67 30 17 13 .55 20 14 11 .56 22 8 9 .41 29
10 14 .37 50
7 15 .48 44 37 56 .90 181
3 1.22 .01 .03 3 1.01 .01 .03 3 1.22 .01 .02 3 1.83 .01 .04 3 1.52 .01 .05
-. 3 1.98 .01 -05 3 3.59 .01 .04 3 .87 .01 .03 3 1.54 .01 .02 3 2.35 .01 .03
4 1.71 .01 .03 2 1.37 .01 .02 3 2.07 .01 -04 3 2.22 .01 .04 4 1.02 .01 .02
3 1.21 .01 .03 3 .85 .01 -02 4 1.36 .01 .03 4 1.08 .01 .02 3 1.79 .01 .02
3 1.05 .01 .02 3 1.12 .01 .01 3 .61 .01 .02 3 .84 .01 .03 3 .56 .01 .03
3 .88 .01 .03 3 .80 .01 .02 3 1.35 .01 .02 4 .93 .01 .02 4 .89 .01 .02
4 1.34 .01 .03 3 1.12 .01 .02 3 1.34 .01 .03 4 .65 -01 .02 2 .97 -01 .03
3 .80 .01 .03 36 1.89 .06 -14
+.iq ICP -%500 GRAM SAMPLE I S DIGESTED WITH 3ML 3-1-2 HCL-HN03-HZ0 AT 95 DEG. C FOR ONE HOUR AND I S DILUTED TO 10 ML WITH WATER. THIS LEACH I S PARTIAL FOR MN FE SR CA P LA CR MG BA T I B U AND LIMITED FOR - SAMPLE TYPE: SOIL AU** ANALYSIS BY FA\ICP FROM 10 GM SAMPLE.
DATE RECEIVED: SEP 19 1990 DATE REPORT MAILED: sqt as/?o SIGNED B.C. ASSAYERS
Page 2 Bapty Research L i m i t e d PROJECT LA POINTE FILE # 90-4572 - Th
ppn - SAUPLE#
L500N 300E L400N 300U L400N 275U L400N 25OU L400N 225U
L400N 20W L400N 175U L400N 15W L400N 125U L400N 1OOU
L400N 75U L400N 50U L400N 25U L300N 30W L300N 275U
L300N 25OU L300N 225U L300N ZOW L300N 175U L300N 15OU
UOON 125U L300N lOOU L300N 75U L300N 50U L300N 25U
L300N OOU L300N 25E L300N 50E L300N 75E L300N lOOE
L300N 125E L300N 150E L300N 175E L300N 200E L300N 225E
L300N 25OE STANDARD C/AU-S
- HO cu f i t n
1 15 :17, 55 2 32 1411 110 2 18 82
1 20 149 1 20 163 1 17 392 1 2 3 175 1 22 1%
1 18 99 18 58 131
N i Co Un Fe ppnppnppn x 27 10 1661 2.65 21 12 606 3.20 23 10 454 3.21 18 9 455 2.96 33 9 357 4.18
38 11 403 4.69 19 7 414 3.73 19 8 376 4.02 23 10 532 3.96 19 7 303 3.77
18 6 282 3.68 30 10 501 4.30 21 9 974 4.17 16 7 262 3.57 30 9 465 3.95
28 8 365 3.84 26 8 275 4.22 43 12 538 4.39 23 8 371 3.39 30 10 489 3.57
24 8 350 3.59 25 10 450 3.69 20 15 848 3.84 24 9 450 4.29 18 6 289 3.80
29 9 701 4.65 24 8 3'18 3.93 19 6 204 3.13 16 6 447 4.15 13 5 146 4.00
17 10 531 4.90 22 12 577 4.42 27 13 1965 5.23 29 14 1453 5.04 22 13 1258 4.22
13 8 396 4.39 68 31 1053 3.97
1 1 1 1 2
3 1 1 1 1
1 4 1 2 3
3 1 5 1 1
1 2 1 3 1
2 3 4 2 4
4 5 2 3 3
2 37
Sb B i V PpnPPnPpn
2 2 13 2 2 16 2 4 16 2 2 18 2 2 16
2 2 16 2 2 22 2 5 24 2 2 24 2 2 26
2 2 24 2 2 17 2 2 2 3 2 3 21 2 2 15
2 2 17 2 7 19 2 3 18 2 2 16 2 2 16
2 2 18 2 4 22 2 2 24 2 2 23 2 2 30
2 2 19 2 2 16 2 2 19 2 2 26 2 2 34
2 3 36 2 3 34 2 2 24 2 2 21 2 2 2 3
2 2 26 15 21 55
20 13 .49 150 21 17 .60 36 23 17 .62 33 24 15 -45 27 14 25 .90 36
17 30 1.14 41 11 17 .50 30 10 18 .54 31 18 19 .61 40 11 19 .45 39
10 15 .37 52 14 23 .67 47 12 16 .48 45 27 16 .53 34 17 25 1.00 34
15 23 .94 42 13 24 .73 33 16 32 1.10 44 13 22 .73 20 14 22 .77 32
13 21 .71 33 15 22 .66 35 16 17 .49 33 12 22 .63 35 12 13 .31 48
12 22 .75 52 13 18 .57 27 11 14 .40 26 11 15 .28 37 12 12 .20 30
9 17 .% 43 11 20 1.26 51 9 18 1.19 72
15 18 .77 119 12 15 .70 83
2 1.24 .01 .04 2 1.56 .01 .06 4 1.65 .01 .06 2 1.66 .01 .05 2 1.80 .01 .06
2 2.46 .01 .06 3 1.31 .01 .04 2 1.49 .01 .05
.- 3 1.83 .01 .05 2 1.50 .01 .04
2 1.05 .01 .04 2 2.14 .01 .06 4 1.11 .01 .04 2 1.63 .01 .06 4 1.93 .01 .06
2 1.75 .01 .05 2 1.60 .01 .06 3 2.29 .01 .10 2 1.65 .01 .05 2 1.61 .01 .07
4 1.62 .01 -05 3 1.60 .01 .08 3 1.95 .01 .04 2 1.39 .01 .05 2 .97 .01 .04
4 1.56 .01 .06 2 1.40 .01 -03 2 .97 .01 .03 2 1.77 .01 .03 2 1.16 .01 .03
3 1.94 .01 .05 2 2.29 .01 .05 2 1.86 .01 .06 2 2.05 .01 .05 3 1.72 .01 .05
2 .98 .01 .04 34 1.89 .06 .14
1 3 3 3 6
1 2 6 1 3
4 3 4 3 6
2 5 4 1 4
6 3 3 5 4
4 5 1 4 4
5 5 6 4 5
5 47 -
lSAEIPLE#
L3OOM 275E L300M 300E L200M 25E LZOOM SOE L200M 75E
L200M 1OOE L2OOM 125E L200M 150E L200M 4 K E L200M 200E
L200M 225E L200M 250E L200M 275E L200M 300E L1OOE3 K E
LIOOW 1OOE L1OOM 125E LIOOM 150E L1OOM 1KE LIOOW 2OOE
L1OOEs 225E LlOOM 250E LIOOW 275E LIOOM 300E LOO 3OOW
LOO 275W LOO 25OW LOO 225W LOO 200tJ LOO 175W
LOO 15w LOO 125W LOO 100W LOO 7 5 W LOO SOW
LOO 25W STANDARD C/WU-S
wo cu
9 2 3 4 27 9 22 9 26 9 25
9 30 9 21 9 26 9 18 9 18
9 21 9 32 9 21 9 16 9 28
9 14 9 22 9 25 9 22 4 26
9 22 9 24 9 33 9 47 9 25
9 22 9 7 5 9 28 3 166 a 46
3 49 4 64 9 20 9 28 9 27
9 21 98 60
M i Bpln
13 16 21 25 22
21 15 31 14 48
20 30 22 12 15
12 17 18 20 28
21 19 21 9
21
P 48 19 84 43
45 61 16 11 22
48 70
-
-
4 3 4 3 9
9 9 2 4
1 2 2 1 3
1 2 2 4 4
2 3 1 1 1
2 4 1 4 2
4 2 2 4 9
2
SAMPLE#
LOO 00 LOO 25E LOO 50E LOO 75E LOO 100E
LOO 125E LOO 150E LOO 175E LOO 200E LOO 225E
LOO 250E LOO 275E LOO 300E LlOOS 30OU LlOOS 275u
LlOOS 25OU LlOOS 22511 LlOOS ZOOU LlOOS 175u LlOOS 15OU
LlOOS 125U LlOOS 1oOU LlOOS 75u LlOOS 5ou LlOOS 25U
LlOOS OOU LlOOS 25E LlOOS 50E LlOOS 75E LlOOS 1OOE
LlOOS 125E LlOOS 150E LlOOS l75E LlOOS 200E LlOOS 225E
LlOOS 250E STANDARD C/AU-S
Mo Cu PPnPPn
1 20 1 15 1 13 1 20 1 19
1 11 1 12 1 2 3 1 16 1 25
1 19 1 20 1 22 1 24 1 26
1 47 1 6 3 48 3 3 4 1 21
1 3 4 1 57 1 30 1 6 6 1 61
1 11 1 98 1 18 1 10 1 8
1 20 1 13 1 16 1 19 1 17
1 27 18 57
Bapty Research L i m i t e d PROJECT LA POINTE FILE # 90-4572
N i Co mppn
15 5 18 6 16 9 21 11 14 6
13 6 18 11 2 3 9 15 7 23 13
14 6 12 7 18 7 16 5 20 6
18 11 16 5 49 13 44 21 20 6
35 18 36 33 35 22
102 25 78 22
10 3 96 41 14 5 11 5 8 3
17 7 16 10 13 4 13 5 10 5
30 10 69 31
- nn m 741 248 826
1532 513
282 2350
326 318
1852
a66 967 275 121 161
350 222 297
1084 236
588 1031 703 310 838
89 527 208 246 323
741 3274
41 5 63 1
1421
217 1048
- -
U PPn
5 5 5 5 5
5 5 5 5 5
5 5 5 5 5
5 5 5 5 5
5 5 5 5 5
5 5 5 5 5
5 7 5 5 5
5 20
- Au Th WPPn
ND 2 ND 5 ND 4 ND 2 ND 2
ND 4 ND 1 NO 3 ND 2 ND 2
I D 1 ND 3 ND 6 I D 1 ND 2
ND 1 I D 3 ND 5 ND 1 ND 2
ND 1 ND 2 NO 2 ND 9 ND 4
ND 1 ND 1 ND 3 I D 2 ND 2
ND 3 ND 2 ND 2 ND 1 ND 1
ND 11 7 38
I.. . . . . . . Sb B i
PPnPPn
2 2 2 2 2 2 2 2 2 2
2 2 3 2 2 2 2 2 2 2
2 2 2 2 2 2 2 2 2 2
2 2 2 2 3 2 2 2 2 2
2 2 2 2 2 2 2 2 2 2
2 2 2 2 3 2 2 3 2 2
2 2 2 2 2 3 2 3 2 2
2 2 15 21
- V
PPn
22 21 29 20 31
27 21 14 21 21
20 25 24 26 28
20 42 18 19 21
19 21 20 14 13
14 14 24 23 23
16 23 25 28 24
14 55
-
-
. . . . . . . . .
L
. .
- La
PPn
10 12 11 21 6
11 10 15 14 14
14 10 14 38 25
28 10 10 15 21
28 65 26 10 11
9 7 9
10 10
10 8 8 8
11
15 37
- C r Mg
p p n x
10 .26 15 .SO 13 .39 12 .49 13 .E
12 .39 12 .57 13 .57 12 .35 13 ;46
11 .M 14 .32 14 .50 12 .22 17 .40
18 .40 26 .59 17 .54 15 .44 20 .53
20 .62 19 .53 18 .57 19 .46 16 .38
5 .09 4 .06
11 .25 9 .25 8 .23
11 .61 11 .40 9 .16
11 .21 7 .09
14 -67 55 -90
. . . . . . . . B A 1
p p n x
3 2.15 4 1.34 3 1.27 3 1.64 3 2.44
2 1.06 3 1.20 2 1.10
-_ ,2 .90 3 1.45
3 1.01 3 2.43 3 1.29 2 2.07 3 1.92
4 2.10 3 1.61 3 1.30 3 .94 2 1.47
3 1.72 3 2.72 2 1.74 4 1.36 4 1.13
2 .40 3 .76 3 .93 2 .88 2 .66
2 1.26 2 1.07 3 .50 4 .93 3 .48
3 2.07 36 1.90
I
- Ne
x .01 .01 .01 .01 .01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.06
Page 4
I SB#PLE%
LIOOS Z K E LIOOS 300E L2OOS 30W LZOOS 2KW LZOOS 25W
LZOOS 225W L200S 20W L200S 9KW L200S 15W LZOOS 125W
LZOOS OOOW L20OS KW L200S 5otJ L200S 2 5 W L200S OW
L2OOS 25E L2OOS 50E LZOOS ?5E LZOOS IOOE L2OOS 125E
L2OOS 150E L2OOS 1KE L200S 200E L2OOS 225E LZOOS 250E
L2OOS 275E LZOOS 300E L300S 300W L3OOS 2?5W L3OOS 250W
L3OOS 225W L3OOS 200W L3OOS 1KW L3OOS 150W L3OOS 125W
L300S 1oow STANDARD C/AU-S
e40 cu P p p m
1 20 4 13 4 16 4 96 9 42
1 32 1 32 1 2 9 1 24 1 18
4 95 9 32 1 38 1 49 1 19
1 16 1 26 4 95 4 14 9 14
4 20 4 49 4 24 1 29 1 21
1 12 9 24 1 26 1 98 4 18
2 29 9 33 1 15 1 15 5 20
9 24 98 62
- Mi
wm,
14 9
99 8
92
32 19 21 99 19
99 45 41 62 9
8 12 9 8 9
49 25 13 28 4 9
9 94 11 10 16
10 20 11 25 19
19 69
-
-
- co
ppm
9 5 9 5 4
92 28 14 9
43
98 94 11 48 4
4 4 5 5 5
8 19 94 13 4
4 8 5 3 5
3 92 4 9
46
91 32
-
-
U Au ppmm
5 WD 5 WD 5 WD 5 WD 5 I D
6 WD 5 WD 5 I D 5 WD 5 I D
5 WD 5 I D 5 WD 5 WD 9 WD
5 WD 5 WD 5 WD 5 WD 5 WD
5 WD 5 ND 5 WD 6 WD 5 WD
5 WD 5 WD 5 WD 5 WD 5 WD
5 WD 5 WD 5 WD 5 WD 5 WD
5 I D 20 I
- B i
Pm
2 ' 2 2 2 2
2 2 2 3 2
2 2 2 2 2
2 2 2 2 2
2 16 6 2 2
2 3 2 2 2
2 3 2 2 2
2 99
- -
v Pm
20 24 22 98 31
28 24 as 26 20
92 21 20 19 21
28 23 29 30 33
23 22 22 99 26
14 31 32 29 22
33 24 29 24 18
22 60
- Ca SS
.09
.06 e 08 .01
05 0 19 A4 D 02 e 05
D 14 0 13 -04 .04 0 02
-04 0 02 03
.01
.02
0 07 28
.17 -09 .04
09 .05 .02 e 22 -01
.02
.03 e 03 .02 .32
* 03 .53
&! %
-49 -39 -63 28
-49
096 -51 -51 D 59 -52
-73 - 55 e 43 -32 0 94
-94 05 -29 0 20 -32
.83 -68 3 9 .n 041
e 26 -445 .33 -39 0 6 3
24 -50 -39 .R -99
.48
.91
- 4 4.29 e o 1 -03 3 0 7 5 -01 .03 4 4.11 -01 -02 3 .a -01 -02 4 1.05 -01 -02
4 9.86 -01 .OS 5 9.14 -09 .03 4 9.39 -01 .02
4 9.18 -01 -02
3 9.98 -01 -02 4 .?9 -01 -01 3 -99 -04 -01 3 -82 -01 .01 3 2.85 -01 .01
4 -89 -01 .01 3 .55 .01 .01 4 -71 -01 .03 4 .a -01 .02 4 .83 .04 .02
4 9.26 -01 .03 4 4.94 .04 .w 4 .81 .01 .04 4 9.45 .01 -86 4 .40 -01 .02
3 .59 -01 .03 4 1.27 .01 -04 4 1.24 A1 .02 3 .K -01 .02 3 1.30 e o 1 -01
4 4.60 .01 -02 4 4.48 .01 .03 4 .82 .01 .01 4 9.47 .01 .02 4 4.43 .01 .02
3 4.00 .01 .02 38 1.89 .06 .I4
- 4 1.39 -01 -02
1300s 75U L300S SOU UOOS u u L300S OW L300S 25E
L300S SOE L300S 7SE L300S 100E L300S 125E L300S 150E
UOOS 175E L300S 200E L300S 225E L300S 250E L300S 275E
L300S 300E L400S 30W L400S 275U L400S 25W L400S 22%
L400S 20OU L400S 17% L400S 15OU L400S 12% L400S lOW
L400S 75U L400S 5W L400S 25U L400S OW L400S 25E
L400S 50E L400S 75E L400S 1OOE L400S 125E L400S 150E
L400S 175E STANDARD C/AU-S
1 12 17 1 60 18
1 3 3 . 9 6 1 15 20 1 56 308
Bapty Research L i m i t e d PROJECT LA POINTE FILE # 90-4572 Page 6
2 1 1 2 3
1 1 2 1 2
1 1 1 1 2
1 1 1 1 6
2 1 1 1 2
5 1 3 1 3
3 1 3 1 1
2
C Y
C r ng P P n x
16 .58 16 .47 11 -36 13 .47 10 .I7
7 .19 8 .14
10 .39 12 .54 15 .W
15 .95 10 .41 7 .35
13 -52 9 .45
7 .39 26 .78 22 .87 9 .27
23 .81
16 .38 11 .32 10 .27 11 .25 17 .26
12 .36 9 .36 7 .23 5 .15 1 .01
4 .06 8 .05
13 -50 13 1.33 20 1.84
15 .T7 56 -90
6 A 1 p p a x
6 1.18 7 1.11 6 1.02 6 1.82 6 1.08
6 .71 5 1.05 7 1.00 7 1.43 7 1.32
6 1.78 6 1.01 6 .82 6 1.27 5 1.29
5 .88 6 1.56 6 1.69 5 1.33 6 1.37
6 1.03 6 1.88 6 .89 2 1.53 6 3.19
6 1.94 6 .92 6 1.17 5 1.09 7 .10
6 .40 7 2.55 6 2.20 5 1.12 7 1.78
6 1.47 39 1.89
- Na x
. 01
.01
.01
.01
.01
.01
. O l
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01 -01
.01
.Ol
.01
.01
.01
.01
.06
SAMPLE#
L400S 200E L400S 225E L400S 250E L400S 275E L400S 300E
L500S 25E L500S 50E L500S 75E L500S lOOE L500S 125E
L500S l5OE L500S 175E L500S 2OOE L500S 225E L500S 250E
L500S 275E L5OOS 300E L600S 300U L600S 275W L600S 250U
L600S 225U L600S 2OOU L600S 175U L6OOS 150W L6OOS 125U
L600S lOOU L6OOS 75u L600S 50U L6OOS 25W L600S OOU
L6OOS 25E L600S 50E L600S 75E L600S lOOE L600S 125E
LbOOS l5OE STANDARD C/AU-S
Bapty Research L i m i t e U PROJECT LA POINTE FILE # 90-4572
24 18 3120 4.66 11 8 957 3.55 4 4 83 1.53
10 7 145 3.74 5 ND
6 4 80 2.00 17 8 134 4.59 22 10 226 3.05 37 19 1722 5.82 23 18 2276 5.35
24 19 2821 5.62 24 18 1639 5.61 16 9 309 3.87 29 18 1654 6.56 18 12 1958 3.89
19 11 1609 3.74 18 15 1172 5.04 11 5 169 3.95 25 24 772 3.75 85 26 294 10.73
42 14 244 6.10 63 37 3236 4.71 30 80 4795 2.31 31 11 494 3.22 38 11 301 3.15
36 8 159 3.46 39 14 741 5.69 32 11 229 5.65 15 6 390 3.28 15 6 215 3.59
18 9 510 5.45 24 11 988 3.97 21 9 301 6.29 34 21 816 6.87 30 12 2573 5.21
23 13 3521 5.70 70 31 1054 3.98 ,, 17 7 37
%a
1 1 1 2 6
1 4
10 1 1
1 1 5 3 4
2 2 1 1 6
2 1 1 1 3
2 2 1 2 2
2 5 4 2 1
1
. . . . . . . . Sb B i V Ca
ppnppnppn x 2 2 19 -18 2 3 25 -39 2 2 34 .19 2 2 39 -05 2 2 21 .02
2 2 15 -03 3 2 12 .01 2 4 17 .04 2 2 28 .69 2 3 27 .31
2 2 33 .18 2 2 47 -19 2 2 21 .04 2 6 8 6 . 0 4 2 2 41 .01
2 2 50 .03 2 3 47 .17 2 2 39 .03 2 2 33 .09 2 4 18 .07
2 2 35 .03 2 2 21 .24 4 6 16 -13 2 2 27 .03 2 2 20 .04
2 4 18 .08 2 2 22 .04 2 2 28 .04 2 2 26 .06 3 3 53 .01
3 4 25 -05 4 2 22 .13 2 2 30 .02 2 2 78 .62 2 8 17 1.16
3 10 20 .35 15 16 55 .52
- La
ppn
11 8 9
11 15
13 13 18 9 8
8 8
19 12 22
20 16 19 60 9
15 55 62 10 17
142 44 12 11 12
12 14 13 7 8
9 37
-
11 1.09 89
12 -27 176
21 .49 43
29 1.02 18
10 .20 29 21 2.48 54 12 1.32 96
B A 1 p p n x
- Ne
x
Page 7
2 1.21 4 1.51 2 .98 2 .53 3 1.47
2 1.00 2 .40 3 2.12
- 3 1.84 '4 1.39
3 1.77 3 2.06 2 .90 2 1.39 2 1.11
3 .87 2 1.03 6 1.70 4 1.97 5 .99
2 1.12 2 1.58 3 2.22 2 1.37 2 2.29
4 2.02 2 4.92 3 1.14 4 3.48 4 1.00
2 1.50 4 2.09 3 1.00 2 2.76 5 1.36
5 1.23 36 1.89
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
-01 . 01 -01 .01 .01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01
.01 . 01
.01
.01
.01
.06 -
Bapty Research Limited PROJECT LA POINTE FILE # 90-4572 P a g e 8 SAMPLE#
L600S 175E L60OS 2OOE L60OS 225E L60OS 250E L60OS 275E
L60OS 300E L700S 30W LMOS 275u L70OS 25OU L700S 22511
LMOS 20ou LMOS 175u L700S 15W 1700s 125U L700S lOW
L700S 75U L70OS 5 w L7OOS 25U LMOS ow 1700s 25E
LMOS 50E L M O S 75E L M O S 1OOE L700S 125E L700S 150E
L700S 175E L700S 200E L700S 225E L700S 250E 1700s 275E
L700S 300E L8OOS 300U L800S 275U L800S 25W L800S 225U
L800S 20W STANDARD C/AU-S
no cu W W
1 24 1 20 1 56 1 15 1 21
1 12 1 112 2 33 2 25 3 35
2 4 4 1 15 1 96 1 3 4 1 19
1 44 1 43 1 46 1 20 1 12
1 17 1 14 1 3 4 1 29 1 26
1 24 2 16 1 14 1 25 4 7 3
2 22 3 49 2 19 3 33 3 49
1 8 18 60
10 5 459 3.66 13 7 520 4.15 9 3 129 3.54 9 5 908 3.28
7 3 138 2.06 31 49 1393 3.32 40 13 540 5.12 18 5 134 5.13 30 18 736 4.29
21 13 1630 3.13 22 12 1416 3.03 20 6 139 1.24 25 19 905 2.57 11 4 255 3.35
63 26 2373 5.94 13 6 929 4.92 28 11 1720 4.30
17 8 829 4.32 5 2 95 3.29
21 11 600 5.09 24 12 2748 4.24 15 18 3760 4.73
11 810963.77 6 3 386 3.32 6 3 855 2.31 7 3 303 2.42
17 17 2615 4.59
57 15 248 5.74 17 4 93 3.74 32 8 300 4.37 36 19 2972 3.66
23 11 2666 2.35 71 32 1049 3.98
*U
Au Th Ppnw
I D 1 I D 1 ND 1 ND 2 ND 4
ND 2 ND 1 I D 1 ND 2 ND 3
I D 1 ND 1 I D 1 ND 1 ND 1
ND 1 ND 3 ND 1 I D 3 ND 1
ND 2 ND 1 ND 1 ND 1 I D 1
I D 1 ND 1 ND 1 ND 2 ND 2
ND 3 ND 2 ND 1 ND 1 ND 1
ND 1 7 38
7 8 .70 91 8 1.57 .01 .05 6 .71 .01 .04 2 2 31 .05 8 9 .29 96
2 2 47 .03 8 15 .59 42 6 1.23 .01 .05 2 2 29 .02 9 8 .45 21 6 1.06 .01 .05 2 2 24 .02 9 9 -46 43 6 1.38 .01 .06
2 2 21 .02 8 6 .32 19 4 .60 .01 .04 2 2 27 .05 128 20 .55 31 6 1.97 .01 .03 4 -2 26 .ll 9 9 .28 41 7 .75 .01 .02 2 3 34 .01 7 8 .ll 34 ---6 .E4 .01 .01 2 2 31 .05 65 14 .52 42 7 1.48 .01 .02
2 2 25 .02 21 14 .53 35 5 1.71 .01 .02 2 2 23 .05 9 13 -47 27 5 1.05 .01 .02 2 2 12 .20 17 14 .52 20 3 .87 .01 .02 2 2 20 .09 77 19 .51 23 5 3.43 .01 .02 2 2 33 .03 14 11 -36 23 6 1.15 .01 .02
2 3 15 .20 12 10 .40 52 6 .90 .01 .02 3 2 29 .03 12 16 -27 36 7 1.52 .01 .03 2 2 25 .02 10 15 .43 52 7 1.08 .01 .02 2 2 24 .01 8 11 -46 27 6 1.30 .01 .02 2 2 25 .02 6 10 .ll 21 5 2.57 .01 .01
7 .88 .01 .03 3 2 20 .15 8 6 .18 30 2 2 47 .02 5 6 .12 25 6 .86 .01 .02 3 3 32 .12 6 13 1.00 59 7 1.73 .01 .07 3 3 19 .40 6 9 . 8 3 90 8 1.22 .01 .06 2 2 22 .10 6 9 .56 52 8 1.08 .01 .05
2 2 32 .17 6 8 .31 40 7 1.26 .01 .03 2 2 35 .04 6 6 .18 34 6 .?9 .01 .03 2 2 37 .04 6 6 .19 76 5 .67 .01 .03 2 2 22 .02 10 5 .I7 23 5 .49 .01 .04 3 2 18 .03 8 8 .51 63 8 1.08 .01 .ll
2 2 20 .06 7 6 .46 126 6 .90 .01 .13 2 2 25 .02 8 8 -18 30 6 .?7 .01 .02 2 2 36 .01 4 8 .16 21 6 .?7 .01 .01 2 2 26 .04 5 7 .16 31 7 .83 .01 .02 2 2 21 .12 187 12 .41 46 6 1.69 -01 .03
Bapty Research L i m i t e d PROJECT LA POINTE FILE # 90-4572 Page 9
SAMPLE#
L80OS 1751 LBOOS 150N L8OOS 1251 LBOOS 1001 L80OS 75N
L80OS SON L80OS 25N 1800s OON L800S 25E LBOOS 50E
1800S 75E 1800s 100E 1800s 125E L80OS 150E L80OS 175E
LBOOS 200E L800S 225E LBOOS 250E L80OS 27SE L80OS 300E
STANDARD C/AU- S
ACME ANALyTICAL LABORATORIES LTD. 852 E. HASTINQS ST. VANCOUVER B.C. V6A 1R6 PHONE( 604)253-3158 FAX(604) 253-1716
GEOCHEMICAL ANALYSIB CERTIFICATE B a p t y Research Limited PROJECT LAPOINTE File # 90-4790 Page 1
901 Industrial Road #2, Crsnbrook BC V1C 4C9 Submitted by: LYNEA U R L W
I C P - .SO0 GRAM SAMPLE I S DIGESTED WITH 3ML 3-1-2 HCL-HN03-HX) AT 95 DEG. C FOR ONE HOUR AND I S DILUTED TO 10 HL WITH WATER. THIS LEACH I S PARTIAL FOR MN FE SR CA P LA CR MG BA T I B W AND LIMITED FOR NA K AND AL. AU DETECTION L I M I T BY ICP I S 3 PPH. - SAMPLE TYPE: P 1 SOIL PZ ROCK AUf ANALYSIS BY ACID LEACWAA FROn 10 GH SAMPLE.
, L
DATg RECEIVED: SEP 25 1990 DATE REPORT MAILED: .D.TOYE, C.LEOWG, J-WANG; CERTIFIED B.C. ASSAYERS
ACME ANALYTICAL LABORATORIES LTD. 852 E. HASTINGS ST. VANCOWER B.C. V6A 1R6 PHONE(604)253-3158 FAX(604)253-1716
GEOCHEMICAL ANALYSIS CERTIFICATE
SAMPLE#
L500N 30OU L500N 275U LSOON 250U L500N 225U L500N 20OU
L500N 175U L500N l5OU L500N l25U L500N 1OOU L500N 75U
L500N SOU L500N 25U L500N 00 L400N 00 L400N 25E
L400N 50E L400N 75E L400N lOOE L400N 125E L400N 150E
L400N 175E L400N ZOOE L400N 225E L400N 250E L400N 275E
L400N 300E LlOON 30OU LlOON 275U LlOON 25OU LlOON 225U
LlOON ZOOU LlOON 175U LlOON 150U L1OON 125U LlOON 10OU
LlOON 75U STANDARD C/AU-S
B a D t v Research L i m i t e d PROJECT LAPOINTE F i l e # 90-4795 Page 1 901 Industrial Road #2, Crenbrook BC V1C 4C9 Submitted by: LYNEA CARLSON
no cu PPnppn
1 34 1 43 1 42 1 30 1 45
1 31 2 31 2 29 1 32 2 27
1 25 2 20 1 28 2 50 1 50
1 25 1 21 1 24 1 15 1 26
1 21 1 30 1 31 1 24 1 33
1 25 2 20 1 37 1 3 4 1 98
3 7 2 3 7 3 4 59 2 33 1 32
1 17 19 59
Pb 2n ppnppa
17 48 25 76 21 62 40 63 18 68
11 86 24 56 2 3 7 7 19 100 26 78
13 79 19 61 20 49 20 55 20 53
17 64 24 84 25 102 21 60 26 103
3 6 9 9 89 349 52 166 34 172 50 149
87 156 11 50 12 68 24 73 11 82
17 77 24 83 19 81 22 105 12 104
14 64 37 131
_ . , ~~~
Mn Fe p p a x
250 3.40 441 4.46 172 3.31 329 3.60 392 3.47
378 4.24 198 3.53 586 3.84 945 3.27 949 2.94
570 3.68 568 3.23 278 3.57 223 4.17 296 3.44
291 4.57 325 3.87 922 4.38 532 3.16 357 3.79
443 4.21 4157 3.80 1727 4.12 2353 3.65 969 4.05
2011 2.66 163 s3.74 819 4.23
1188 3.57 379 3.49
1022 5.32 1499 4.69 533 4.47
1529 4.61 1631 5.44
301 3.29 1054 3.96
5 N D 1 5
5 N D 4 3 5 N D 2 7 5 N D 2 9 5 I D 2 21 5 ND 1 18
5 N D 3 9 5 ND 2 12 5 N D 3 5 5 N D 4 4 5 N D 2 3
5 N D 2 5 5 N D 3 3 5 N O 2 4 5 N D 2 4 5 N D 6 3
5 N D 3 4 5 ND 1 22 5 N D 2 4 5 N D 2 7 5 N O 6 4
5 ND 1 17 5 ND 4 . 4 5 N D 5 4 5 N D 1 4 S N D 3 4
5 N D 4 3 5 N D 3 6 5 N D 3 6 5 N D 2 8 5 N D 2 5
5 N D 4 4 19 7 40 53
Sb B i ppnw
2 2 2 2 2 2 2 2 2 2
2 2 2 2 2 2
. 2 2 2 2
2 2 2 2 2 2 2 2 2 2
2 2 2 2 2 2 2 2 2 2
2 2 2 2 2 2 2 2 2 2
2 2 2 2 2 2 3 2 2 2
2 2 2 2 2 2 2 2 2 2
2 2 14 19
- V
ppn
23 25 22 24 21
19 25 22 18 16
19 23 22 31 24
27 20 26 28 18
26 24 22 23 20
18 37 28 23 22
23 20 22 25 26
26 56
- Le C r Hg
w#m x 22 14’ .34 27 20 .72 26 15 .39 19 15 .45 36 18 .56
18 25 1.13 15 15 .40 32 19 .66 47 19 .58 35 17 .57
24 21 .85 18 16 .51 22 15 .48 29 21 -27 22 16 .36
14 17 -50 14 22 .94 15 18 .45 10 11 .29 15 15 .70
9 14 .49 16 15 .65 15 16 .73 11 13 .40 19 17 .98
13 13 .28 10 11 .28 17 20 .76 21 28 .94 45 26 1.00
17 19 .82 38 17 .66 62 16 .76 22 23 .67 16 29 .82
9 15 .45 36 57 .92
- Be
ppa
38 43 38 40 41
42 39 37 37 35
39 33 19 21 32
30 29 41 38 41
58 117 113 192 66
143 37 30 30 28
29 36 31 36 40
29 181
- ~~
8 A 1 Ne p p n x x
2 1.89 .01 2 2.25 .01 2 2.06 .01 3 1.65 .01 3 2.14 .01
8 2.09 .01 3 1.21 .01 3 1.87 .01 2 2.05 .01 2 1.73 .01
2 1.86 .01 3 1.30 .01 2 1.17 .01 7 2.80 .01 2 1.74 .01
7 1.32 .01 6 1.66 .01 4 1.54 .01 3 .93 .01 3 1.61 .01
4 1.13 .01 6 1.59 .01 4 1.46 .01 2 1-23 .01 2 1.78 .01
4 1.14 .01 2 1.78 .01 2 1.86 .01 4 1.86 .01 4 1.93 .01
2 1.86 .01 2 1.63 .01 8 1.51 .01 4 1.82 .01 4 1.76 .01
2 .90 .01 31 1.90 .06
-
ICP - .SO0 GRAM SAMPLE I S DIGESTED UITH 3HL 3-1-2 HCL-HN03-HZO AT 95 DEG. C FOR ONE HOUR AND I S DILUTED TO 10 HL UITH WATER. THIS LEACH I S PARTIAL FOR MN FE SR CA P LA CR MG BA T I B U AND LIMITED FOR NA K AN AL AU DETECTION L IHIT BY ICP I S 3 PPH. - SAMPLE TYPE: SOIL P P
DATE RECEIVED: SEP 25 1990 DATE REPORT MAILED: SIGNED B Y . . . . . . . . . .D.TOYE, C.LEONG, J.UANG; CERTIFIED B.C. ASSAYERS
\ .
‘“7 * *
,.. . .
Bapty Research L i m i t e d PROJECT LAPOINTE FILE # 90-4795 Page 2
I
LlOON SOU LlOON 25U LlOON 00 LlOON 25E LlOON 50E
1500s 30W L500S 275u L5OOS 25W L500S 225U L500S 20W
1500s 175u 1500s 15W L5OOS l25U L500S low LSOOS 75u
L500S 5W L5OOS 25U 1500s 00 STANDARD C/AU-S
. . . . .
! . . . . , . ,
. . . I : . : . . .
. . . - 1 .
., . .
APPENDIX 1V
Statement of Work
. . . . ' 3 . , . , . . I , , . , . . . ... . . .. . , . .
. , . . .
* . . , , .
:#' -. . . . . , . (Name)(s) .: . 2 I:'. I, '; I - . , , * 8 '
. . 305. - :67.5: W: €IASTCNGi $qiij!'-. j
. . ! (Name) i ,606i TRAIL STREET
- ' (Address) 1 KZMBERLEY,. B. C..
. . .................... . . I . . ............................... # . .ill .,a! .t . . 3 . . . . . . . . . , . ' (Address). ' '. ...............................................................................
, . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
. .. .
. . . . . . .. . . . . . . . . . . . . . . . . .... . .
~ _- - ...,... * .. <, I :. . 4 2 7.-.7 6 3 1. .OR. k26.-.62 7.7.. : :. .6.694M.5 :..:
. . . ' ( Telepholie) . . : , (Telephone) .
Valid, subsisting. F.MC, yo. . . . ( 89 ) . . .28326.8... . . . ; . . . . .:... ..i : Valid subsisting FMC- Nd89r). ,280
,: FMC Code,. .$.OUKOG . . .(go) 211652
. . . . . . . . BAp.TKB :.. . . . . . . . . . .
, or caused to be done, workpn the 1 ..!??!..6r..R@E..
.(NOTE: ,If only paying cash in lieu, tur . .......
. . . . . . . . .'*t ~
4 .. ............ ----. - . . . . . . . . . . . . lhrough 8 (as appropriate) of Ihe Regulalions.'. ....-_ i
' . \ I \ r' i:). <, : 1
. .
. . . . + .
. i i:; (; . . . . . . . . .
,: .. . . . i . > . . . . ...................................... - . '. . . . . . . . -_
......................................
j Who was Ihe Name ,. !
. . . . . . . . . . . . . . _ _ .. ~ -. .... )I '.: 3 : . I i .I.... ............. i... ..-.: . . . . ....... ! ............... 1... ...lC--..- -.. , . . _
f.. .................................................... ..-.-. ...
........................ I . I :
108 . T.. , 1 N&CE.X) GROUP Na
.... .:; ' ...
A u e - d woe to be credited to portable assessmer$f
10 00 OF THE F AS FOLLOWS:
Columns G through P inclusive MUST BE COMPLETED before work credits can be granted to claims Col- umns G through J and Q through T inclusiye,MUST EE COMPLETED before a cash payment or rental pay- ment can be credited. Columns not applicavle need not be completed.
q-+ INITS: I 'ixPIRY DATE
....................... A . . .. ,
. q.:, ,.; ,. . . . .y ........................ ...... . . ....
-. .___ .. _. i
K '.WORK TD BE APPLIED
PLICATION OF WOR'
... . . , > . . ,
$180.00 P A L OF M
:REDIT , '
i:;,Ni. I 0. . R ' r. Lmmr
~ . - . EXPIRY ..NEW. ,DATE &Iffi&SED I ..I . . . .
. ' I_
. . . . . . . .
... . '. .p
3 .. ... ..-. ................................. . . . . .. ................................. -. . . . . . , . .................................
................................... .- r"" . I , :,;;. _.. ... i . F. ....... . ...................... :. ...........
. . . . . . 1. . . r . - - ;;;.. .r>-- . - .. .%..~ . . -.. ................................. . .... raL: . "+, ...... ..
c _ ci '
. . . . . . . .
..*x.., . . . . . . . . . . . . .......................... ': " 1 ' ' _ .. :-......
.*.- ' ' .,-- -. . . ................................. 1 . .;.' 3.. . . * I .
. .-
I_s
P ; EXCESS -CREDg qEMAINING
. . . . ........... ' Q " . ,-
.......... -.
i -9 .......... iu , -
4:: )..* .......
- . . ........... ...........
.- . .... . . ...........
..........
.......... -..-_. .
-- .
.. ..
Cash Payment CASH IN LIEU OF V
............
RK OR 'LEA S
L ~ E c- RENTAL.
.... :. I ..
. . . . . , -.. . . . . .
................ ,,{ : . d J r .+ -. ..............
...............
..............
..............
..............
..............
..............
............ .- . . . . .............
. . . . . . . . . . . . . . . . .
............. , . . , . _ _ ' * .: . '
............. . -. % .
__.. :: ._... . . . . . . . ............. . _ I - *. . . ,- -._
i RENTAL . T
_. NEW -EXPIRY DATE . . n
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I. the undersigned Free Miner. hereby acknowledge and understand that it is an offence to.kndngly make a faice Statement or provide false information under the Mineral Tenure Act. I further acknowledge and understand fk.3 if, the statements mad$ or inform@on given, in this Statement Of Wotk f Cash Payment are found to be lzk' ' and the.explor$on and development has not been performed. as a l l e g 4 n this Statement of Work - cash pz ment. then the work reported on this statemem will be cancelled a n e subject mineral claim(s) may as a'res:~
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forfeit'to and'ves; back tothe Province. "' :.'. I.
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