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ARIS SUMMARY SHEET
Di
rict Geologist, Nelson
Off Confidential: 90.05.19
ASSESSMENT REPORT 18830
MINING DIVISION: Nelson
PROPERTY :
LOCATION :
POogY
LAT
49 12 10
UTM
11 5449852
NTS
082F03W
CAMP :
004
CLAIM(S) :
OPERATOR(S):
AUTHOR(S):
REPORT YEAR:
COMMODITIES
SEARCHED FOR:
KEYWORDS :
Poogy,DC 1-2,Bear 1-2
Landis, J.R.
Landis, J.R.
1989, 50 Pages
WORK
DONE :
Ymir
-
LONG
117 23 30
471468
Nelson Area
Silver,Lead,Zinc
~urassic,Elise Formation,Nelson Plutonic Rocks,Andesites
Argillites,Monzonites
Geophysical
EMGR
4.9 km;VLF
I ACTION:
REPORT ON THE POOGY GROUP MINERAL CLAIMS
ERIE MOUNTAIN AND BENSON CREEK AREA
COVERING: Record Numbers:
LOCATED:
Latitude
49'
12'10"
Longitude 117' 23'30"
TOPOGRAPHICAL MAP:
82B/3
MINERAL CLAIM MAP:
M82F/3W
ELEVATION :
2700' TO 5300'
OWNED BY:
John R. Landis
Derek Colville
PREPARED BY:
John R. Landis
DATE SUBMI TTED :
June 9, 1989
GEOLOGICAL BWANCH
ASSESSMENT REPORT
PAGE
A.
Introduction
1.
B.
c.
3
Geographic Position and Access t o Claims
a)
Location Map
-
Area
b)
Location Map
-
Claims
c)
Topographic M a p
d)
Geological Map
el
Legend
2.
Property
3.
People Involved
4.
Brief History
-
3
-
Mineral
Claims
Claims
f
1.
Geophysical Survey
2.
Lines established
3.
Prospecting
Detailed ~echnic-Data
1.
AppendixAtoH
3
InkSZQretation
The Poogy Group of twenty-two mineral claims are
situated on the west side of the Erie Creek mining area.
They can be reached from Salmo by old logging roads.
From Salmo, one would travel west along Southern
Transprovincial Highway 3 to Erie Creek. After crossing
the bridge at Erie Creek, take the first road right and
travel parallel to Erie Creek for two Kilometres. Take
the road that turns left and stay on this road to its
end. The geographic positioc of the claims is Latitude
49'12'10"
and Longitude 117 23'30".
2.
The property involves 22 claims held by two
individuals. The claims are as follows:
a)
Poogy Claims
-
18 units - registered by John R.
Landis
b)
DC#l; DC#2 - 2 units
Bear#l; Bear#2 - 2 units
-
registered by Derek
Colville
Much of the property is covered with overburden so
the VLF-EM Sabre Model 27 was used to prospect for any
potential mineralized zones.
A fault, in a north-west direction cuts the Elise
Formation, the Nelson Plutonic's, and the Archibald
Formation south of Erie Mountain.
A magnetic high lies south-west of Mount Erie. This
is in between the low north of Mount Erie and another
low south-west of Mount Erie and shows an interesting
doughnut formation. Since much of the area is under
heavy over-burden VLF-EM Surveys with soil sampling
would help to give a better understanding of the reason
for the magnetic contours as on the aeromagnetic map.
The claims lie in all three geological formations
although the eastern portion is mostly in the Elise
formation with granitic intrusions.
The VLF-EM Sabre Model 27 surveys indicated areas
of high field strengths. However, there were no distinct
cross-overs. The high readings in Field Strength could
be due to the monzonite formation as pointed out in
Walker's Memoir 172, 1934. The magnetite content in the
monzonite formation could be giving the high readings. A
good soil sampling program would augment the VLF-EM
Sabre Model 27 survey.
Also, old diggings in the area need examination.
The Bear Claims and the eastern side of the Poogy
Claims can be reached by old logging roads.
3.
The people involved in the program on the claims
were as follows:
a)
Derek Colville, a professional roofer and
businessman, has been involved in prospecting for
the past two years. He has taken the Geology course
at Selkirk College and this spring he took the
prospector's course in Nelson. He is also a member
of the Chamber of Mines.
b)
John R. Landis, Student Assessment Officer, has
been involved in prospecting, mining, diamond
drilling, and geophysical surveys. He has taken
geology courses at Selkirk College and prospecting
courses at the Chamber of Mines in Nelson. He was
responsible for the VLF-EM Sabre Model 27 survey.
He is also a member of the Chamber of Mines.
Most of the activity in the Erie Creek area was on
the eastern slopes with past producing gold mines such
as the Second Relief and the Arlington at the turn of
the century and into the 1940's (there has been much
activity in this area to date with some projects slated
for this summer).
There has been activity north of these claims with
fairly good showings of silver, lead, zinc and some
gold.
The Armstrong Group consisting of Crown-granted
claims, Armstrong, Erie and the Black Knight were worked
in 1902 and then lay idle until 1928 when a 2-ton sample
was shipped worth $22 in silver.
The workings lie within a stock of Nelson Granite
and are mineralized with pyrite and galena. Stibnite was
evident.
On the Erie Claim there was evidence on marmatite,
galena, chalcopyrite in calcite gangue.
The Erie Claim is on the east side of the DC#2
Claim in this report,
The Pinnacle Claim is in the Poogy Claim area. So
historically there has been some activity in the area
but none of recent date.
The geophysical surveys were done to locate any
possible anomalies or changes in the geological
structures under the overburden.
Lines and surveys were established on the following
claims:
DC#1
&
#2 Claims
A VLF-EM Sabre Model 27 survey was established from
the Initial Post (IP) north (360') to the Final Post
(FP) for 457.2 metres and to 500 metres. (Slope
correction - snow at the upper level made it rough
going. ) .
Poogy Claims
A VLF-EM Sabre Model 27 survey was established from
Post 3s east (90" in 1000 metre stretches.
The complete line went for 3000 metres to Post 3s
6E.
Poogy Claims and Bear#2 Claim
A line from the East boundary of the Bear Claim ran
for 510 metres in a 200' direction. Then a line from 480
metres went for 400 metres west 270' to reach the Poogy
line which was running north. Post No. 2s 6E of the
Poogy Claim was located.
Then a line from Post No.
for 500 metres.
went north (360')
Bear Claims and Poogy Claims.
A line from the East boundary of the Bear#2 Claim
was established 270' west for 960 metres where a steep
cliff terminated the survey to another time (The high
readings obtained on this line were similar to the high
readings on the Poogy Claim line from 2310 metres to
2850 metres. This parallel line has similar readings.).
RETATION
The first VLF-EM Sabre Model 27 survey was done on
the line for DC#1 and DC#2 from the Initial Post (IP)
and ran in a northern direction to the Final Post (FP)
for 500 metres.
-
An old mine was passed at the 200 metre mark.
From 0 metres to the end of the line, there were no
significant changes in either the Dip reading or the
Field Strength reading. This could indicate that the
geological structure runs in a north-south direction.
The Seattle, Washington Station was used for this
survey (Appendix A ) .
2.
On the Poogy Claims, Seattle Washington was used
for the VLF-EM Sabre Model 27 survey.
Starting with 0 at Post 3s the Dip went down to -20
but dropped to 0 at 90 metres. However, the Field
Strength remained constant and weak.
Another cross-over occurred at 480 metres, 570
metres and then at 660 metres. The survey ended at a
constant Dip of -10 and the Field Strength at 40
(Appendix B ) .
3.
The main southern boundary was continued with the
VLF-EM Sabre Model 27 survey. Seattle, Washington was
used as the station.
The Dip readings went from a -10 to a high of -30
and also an increase in the Field Strength. The area at
1440 metres needs examination.
The talus was black and argillicious in structure.
The low Dip reading of -10 before the creek at 1980
metres and the high Field Strength would indicate
structural change that should be examined (Appendix C).
4.
For the final 1000 metres from Post 3S4E to Post
3S6E, the VLF-EM Sabre Model 27 was used to complete the
survey.
Possible cross-overs occurred at 2040 metres, 2100
metres, 2160 metres, 2370 metres. It was here that the
Field Strength took a significant jump to 95 and then to
a 100.
The Dip decreased, but the Field Strength remained
high almost to the end of the survey.
This could be the monzonite zone as related in
Walker's Memoir 172, 1934.
There was much over-burden in this area. It also
h a s many d i g g i n g s t h a t h a v e grown o v e r w h i c h would
i n d i c a t e much a c t i v i t y p o s s i b l y a t t h e t u r n of t h e
c e n t u r y ( A p p e n d i x Dl.
5.
I n order
27 s u r v e y w a s
Bear#2 Claim.
510 metres a t
t o c o v e r a d i f f e r e n t a r e a , a VLF-EM S a b r e
s t a r t e d a t t h e s o u t h - e a s t b o u n d a r y of
This l i n e followed a n old logging road f o r
200' s o u t h - w e s t ( A p p e n d i x E).
T h e r e were no s p e c t a c u l a r c h a n g e s i n t h e o v e r a l l
readings.
Then a l i n e f r o m t h e 480 metre m a r k w a s e s t a b l i s h e d
i n a west d i r e c t i o n o f 270P f o r 400 metres w h e r e i t
c r o s s e d t h e Poogy C l a i m s .
A g a i n , t h e r e were n o u n u s u a l r e a d i n g s ( A p p e n d i x F ) .
Then f r o m P o s t 2 s 6E a s u r v e y was made i n a
n o r t h e r n d i r e c t i o n (360' 1 t o P o s t 1s 6E o f 500 metres.
T h e r e w a s a c r o s s - o v e r p a s t t h e creek a t 60 metres.
The D i p r e m a i n e d l o w a n d s o d i d t h e F i e l d S t r e n g t h .
T h e r e was much e v i d e n c e o f much a c t i v i t y a t o n e t i m e .
The VLF-EM S a b r e 27 c e r t a i n l y was n o t p i c k i n g u p
a n y t h i n g e x c i t i n g ( A p p e n d i x GI.
6.
A p a r a l l e l l i n e t o t h e s o u t h e r n b o u n d a r y was
s u r v e y e d t o see i f h i g h r e a d i n g s c o u l d b e o b t a i n e d i n
t h i s a r e a . The l i n e was s t a r t e d a t t h e e a s t b o u n d a r y of
t h e B e a r # 2 C l a i m a n d e s t a b l i s h e d w e s t ( 2 7 0 ) f o r 960
metres u n t i l a s t e e p c l i f f was e n c o u n t e r e d .
The P o o g y l i n e was c r o s s e d a t 480 m e t r e s .
The D i p a t 6 0 0 metres w a s -12 a n d t h e F i e l d
S t r e n g t h jumped f r o m 40 t o 9 5 . I t w e n t t o a 1 0 0 + a n d
s t a y e d t h a t way t o t h e t o p o f a c l i f f .
The o u t c r o p had m a g n e t i t e i n i t s o t h i s is w h a t
c o u l d be g i v i n g t h o s e h i g h r e a d i n g s .
A l s o , t h e h i g h r e a d i n g s c o i n c i d e d w i t h t h o s e on t h e
s o u t h e r n b o u n d a r y l i n e w h i c h is 1 0 0 0 metres away.
T h i s area d e f i n i t e l y r e q u i r e s e x t e n s i v e g e o p h y s i c a l
work t o i s o l a t e t h e area t h a t i s g i v i n g t h e h i g h
r e a d i n g s ( A p p e n d i x HI.
The a s s a y s were t a k e n a t t h e mine dump on t h e DC#1
a t 200 m e t r e s ( A p p e n d i x I).
T ST-
1.
Vehicle:
Four wheel drive
fuel and maintenance
2.
Geophysical Operator
6 X $200
$
1,200.00
3.
Field Assistant
6 X $100
$
600.00
4.
Equipment and Field Supplies
Flagging, sample bags, Assays
VLF-EM Sabre Model 27
6 X $50
$
300.00
5.
Food
($10 X 2 ) X 6
$
120.00
6.
Report: Writing, typing, printing
$
180.00
TOTAL
$ 2.800.00
9
E.
1.
D e r e k Colville
2.
John R. Landis
I, DEREK COLVILLE, certify that I have assisted in
Geophysical surveys of mineral properties.
This involved survey work, staking, VLF-EM 16 and VLF-EM
Sabre Model 27 method, and the Self-potential method.
I have taken a geology course from Leslie Anderton at
Selkirk College.
Recently, I have completed a Prospector's Course at
Nelson, B.C.. It was sponsored by the Chamber of Mines and
the Ministry of Energy, Mines and Petroleum Resources.
I am a member of the Chamber of Mines, Nelson, B.C..
At present, I am self employed as a roofer and spend my
spare time in exploring old mining properties.
Dated at Castlegar, B.C. this 6th day of June, 1989.
Derek Colville
Colville Roofing
Prospector
I, JOHN R . LANDIS, of the City of Castlegar, certify
that:
1.
2.
I successfully completed the Prospector's Course in
Nelson, B.C., sponsored by the Chamber of Mines and
presented by George Addie, District Geologist, and other
specialists in the mining field. I have attended other
Prospector's Courses since that time in order to keep
current in this field.
I am a member of the Chamber of Mines, Nelson, B.C.
3.
I took geology courses from Leslie Anderton at
Selkirk College.
4.
I have worked as a diamond driller for T. Connors
in the early 1950's.
5.
I have a Bachelor of Education degree from the
University of British Columbia, Vancouver, B.C., 1964
and obtained a Masters of Education degree from Eastern
Washington University in 1970. I also hold a Masters of
Arts degree in Psychology and Counselling from
International College, Los Angeles, U.S.A..
6.
Although I have been in the teaching profession for
the past 33 years as a teacher, principal and a
psychometrician, I have also spent part of my life in
the mining field in Salmo, B.C., Port Radium, N.W.T.,
and Paulson, B.C., so I have some knowledge and
experience in the mining industry.
Dated at Castlegar, B.C., this 6th day of June, 1989.
B.Ed.,M.Ed.,
Prospector
M.A.,
1.
Walker, J.F., Geology and Mineral Deposits of Salmo Map
Area, British Columbia; Geological Survey, Canada,
Memoir 172, 1934.
2.
Map 1145A, Geology, Salmo, B.C.,
3.
Methews, W.H., Lode-Gold Deposits, South-eastern British
Columbia. Bulletin No.20 - Part 11.
1964
I
M A P 84796
SALMO
BRITISH COLUMBIA
1
Scale: One Inch to One Mile = Ml'rs
63.360
0
64
I
A
,
.- - - .--
argifire. and tuff
L O W E R A N D MIDDLE JURASSIC
HALL FORMATION: argillite, siltsrone. shale. phyllire: 14a. ce
hornfels; 14b, includes abundant volcanic rocks
I
:.:
?CT.~JS
siltsrone
and
I
L~.;fER. MIDDLE.
ROSSLAP
I 5[ %
I
I
6
-
Andesite
dugire pc
L-.srgillacec
k:
f
L O W E R JURASSIC
ELISE FORMATION: andesire and basalt flows and flow breccia, agglomerate. augire
porphyry: 13 a , tuff, siltsrone. and argillaceous quartzite; 13b, amphlbolite
TRIASSIC
(7)A N D
JURASSIC
L O W E R JURASSIC AND(?) OLDER
ARCHIBA LO FORMATION: siltsrone. argill~reargillaceous quamire: mirmr t ~ +;.id
lava locally abundanr
I
ORDOVICIAN
.
-
I
L O W E R A N D (?) M I D D L E ORDOVICIAN
ACTIVE FORMATION: black argillite and slate; 9 a , grey limestone and argillaceo~s
limestone :9 b, silicified argillire and limestone: 9 C, dolomire dolomite breccia, and
limestone
.
I
1
I
CAMBRIAN
MIDDLE CAMBRIAN
NEL WAY FORMATION: cream weathering grey dolomite; limesrone and argiflite; 8a,
limestone and calcareous argillite: 8 b , dark and light grey dolornite; 8c. grey limestone
L O W E R CAMBRIAN
LA18 FORMATI0N:phyliire. argillire. schist, micaceous quartzite, and limestone:
7 a , Reeves Member: grey limestone: minor dolomite: 7 b , Emerald Member:
black phyllire and argillite; 7 c ,upper Laib Formation :phyllite, schist, micaceous
quamite: minor limesrone
LOWER CAMBRI.
Quamire
and argil
lOc, ?hi
RENO FORMATION: argillite. argillaceous quamite; 6a, Truman Member: phyllire and
argillire with limesrone lenses
. . ..
QUARTZITE RANGE FORMA TION: white, green. and pinkish auam're: 5a. Motherlode
Member: white q u a m i t ~ minor
;
argi//ife,grit and green schist; 5 b. Nugget Member:
whire quamire :argillaceous quamire and argillite ar base; 5c. Navada Member: thin
bedded argillaceous qmra'te; white quamite at top; 5d. argillaceous quarturtutee
probably equivalent to lcrver Nugget Member (5b)
THREE SISTERS FORL"T1ON: green and grey grit and ~ u a m . t e ;mmor conglomerzte
and green schist; 4 a, conglomerare: 4 b, chlorite schlst ;4 c , brown micaceous schisr
-
I
WINDERMERE
MONK FORMATION: green argillite andphyllire; 3 a , conglomerate: 3 b , limesrone
M A P llA5A
GEOLOGY
SALMO
BRITISH
COLUMBIA
Scale 1:63,360
1 Inch to 1 rnlle
1
0
Mllrs 1
Sedimentary rocks; p Kilometres 1
dare-and phyllitc: f3;
t
-
0
1
2
- -.
3
3 Mllrs
*---.
4
5 Kilometres
A~prowrnaremnpcrrc d~clmarron.21'36' East dccreasmp 2 9' an-ually
L E G E N D
!I
18.CORYELL PL UTO'ONIC ROCKS :atkalhe rocks: 188, auglte-biotlte monzonite :
lab1 basic spnite
2
19. SHEPPARO INTRUSIONS: Ieucocraric gmnita and sysnite
C R E T A C E O U S (?I
L O W E R CRETACEOUS (1)
NELSON PLUTONIC ROCKS: granitic rocks: 17r, porph *tic granite: V b , granite:
17c ,granodiononte:17d1quartz diode
JURASSIC
MIDDLE A N D I ' ~ UPPER JURASSIC
U P P E R ROSSLAND GROUP
Andesite. basalt. and latire flows and flow breccia, agglomerate; inrercalated siltstone.
argillite. m d tuff
LOWER. MIDI
ROS!
L O W E R A N D M I O D L L JURASStC
HALL FORMATION: argillite, siltstone. shale, phyllite: 14a1carbonaceous siltstone an
hwnfels: 14b, includes abundant volcanic rocks
augi
L O W E R JURASSIC
ELISE FORMATION: and&@ and basah flows and flow breccia. agglomc~ste.augite
porphyry: 13a1 tuff. sil(srone, and argiltarnous quamite: 13b, amphibolite
TRIASSIC 171 A N D J U R A S S I C
L O W E R JURASSIC A N D 0)
OLDER
ARCHIBALD FORMATION: sllrstona. argillita argllleceous quartzite: minw tuff and
lava locslly ebundanr
ORDOVICIAN
L O W E R A N D I?)M I D D L E ORDOVICIAN
ACTIVE FORMATION: block argil/ito md k / ~ t #90,
; grey limestonr and argillaceous
limestone; 9 b, .silicified argillite end limestone: Qc, dolomite dolomite brecaa, and
limesrone
.
CAMBRIAN
M I D D L E CAMBRIAN
1.1
NEL WAY FORMATION :ueem weathering grey dolomite; //mestone and argillin: 8 a ,
limestone end c8lcamous argi/l/re: Bb,dark and light g m y dolomite: 8c. g m y limestone
L O W E R CAMBRIAN
LAlB FORM A TION: ph yllite, orgill~te.schist. mic8cwus q u ~ t z i t sand
.
Itmestone:
78,Reeves Membu: grey limestone; minw dolomita: 7 b 1 Emerald Member:
block phyllin and argtllite: 7c ,upper Laib Formation: phyllite, whist, micarnous
quartzrte :mtnor limestone
-
1
.
1
RENO FORMATION: aqillite, a r ~ ~ ~ b c e o
quartzite;
us
6a, Tr
ar~illitewith limestone lenses
QUARTZITE RANGE FORMATION: whim, m n , and
Memaw: white quamite: minor .m,//ite, ~t andwhite quanu'ie: ergillaceous qwrtu'te and wgillito or
1
WINDERMERE(?)
A
GEOLOGY
S A L M0
Scale 1:63,360
[ T I2
L O W E R CAL
5 A Vire and
-lode
Station
LCP OM
20M
4OM
60M
80M
lOOM
120M
140M
160M
180M
200M
220M
240M
260M
280M
300M
320M
340M
360M
380M
400M
420M
440M
460M
480M
500M
DiP
Field Strenath
Road
Trench
45
45
45
40
40
40
35
30
45
30
35
35
30
35
35
30
30
35
35
35
35
40
40
35
40
45
-8
27 7-
BENTON CREEK IE MOUNTAIN
POOGY CLAIMS
TRAVEL 90' EAST. APRIL 2 2 . 1989
SEATTLE, WASHINGTON STATION
Station
OM
3 OM
60M
9OM
120M
150M
180M
210M
240M
270M
300M
330M
360M
390M
420M
450M
480M
500M
SlOM
540M
Post 3s
Creek 250M
3s 1E
BCLS SURVEY POST - IRON POST
40
30
30
30
30
30
30
35
30
30
30
30
30
25
30
35
35
30
30
35
27 S U R V U
Mo-
EmGmwuM
TRAVEL 90'
U S T . APRIJa 29. 1989
ON STATION
Creek
40
40
40
45
50
50
55
50
50
50
50
60
60
65
65
70
85
60
60
40
Talus
40
50
45
55
50
40
Outcrop
Creek
40
40
40
45
45
80
100
80
35
-
Er, 27 S
m
IR HQUNTAIN
TRAVEL 90' EAST. MAY 6, 19m
GTON STATION
muAkawa
UQ
Station
35
30
35
40
40
40
45
45
Gully
Gully
55
50
60
75
95
95
100
100
100
100
100
95
90
90
85
80
80
90
90
75
80
80
80
75
75
75
65
60
FINAL POST
-
3 s 6E
D POOGY CL-
N
UR
CONTINUE SURVEY WEST 2 7 0
(FROM 480M)
F i e l d Strenath
M o m
R AND POOGY
CLAIMS
TRAVEL 270" WEST. MAY 13, 1989
SEATTLE, WASHINGTON STATION
Distance
UE
REACHED POOGY LINE AND POST
Field Strenuth
- NO. 2 s 6E OF POOGY
CLAIM
S U E MODEZ 77 SURVEY
F: MOUNTAIN
L 3600 N O W H . MAY 13. 1989
ATTLE- WASHINGTON STATION
Distance
OM
30M
60M
9 OM
120M
150M
180M
210M
240M
270M
300M
330M
360M
390M
420M
450M
480M
500M
Post 2s 6 E Poogy
AT POST 1s 6E POOGY
Creek
40
35
35
35
35
45
40
35
35
35
35
30
35
35
35
50
45
40
M O m 27 SURVEY
MOUNTAIN
AND POOGY (&M&&
TRAVEL 270' WEST, 5050' LANDING
SEATTLE, WASHINGTON STATION. MAY 14, 1989
Distance
OM
30M
60M
9 OM
120M
150M
180M
210M
240M
270M
300M
330M
360M
390M
420M
450M
480M
510M
540M
570M
600M
630M
660M
690M
720M
750M
780M
81OM
840M
870M
900M
930M
960M
Field Strenuth
5200'
Road
Top of
Steep C l i f f
5300 '
60
60
65
70
70
70
70
60
55
60
65
60
60
75
60
60
60
40
40
40
95
loo+
loo+
loo+
loo+
loo+
loo+
loo+
loo+
loo+
loo+
100+
80
Hondar-Ckgg & Company Lld.
130 Pernberton Avr.
North Vancouver, B.C.
V7P 2R5
-'m)985-0681 Telex 04-352667
Geochemical
Lab Report
REPORT: U89-02421.0 ( COHPLETE
I
REFERENCE INF0:
SUBflITTED BY: J.R. LANDIS
DATE PRINTED: 8-JUN-89
CLIENT: MR. JOHN LANDIS
PROJECT: NONE GIVEN
-
ORDER
NUHBER OF
LONER
ANhLYSES DETECTION LIHIT EXTRACTION
ELEMENT
38
39
Cu
Ni
Copper
Nickel
1
1
IPPfl
2 PPfl
40
Cr
Chromium
1
2 PPfl
SAHPLE TYPES
NUflBER
SIZE FRACTIONS
HETHOD
HN03-HCL HOT EXTH
HN03-HCL HOT EXTR
Atomic A b s o r p t i o n
Atomic A b s o r p t i o n
X-Ray F l uorescence
NUflBER
SAflPLE PREPARATIONS NUflBER
REHARKS: ELEUATED DETECTION L I f l I T S DUE TO HIGH
RARE EARTH ELEHENT CONTENT.
REPORT COPIES TO: 808
-
1 0 t h STREET
INVOICE TO: 808
- 1 0 t h STREEl
-
-
Geochemid
Lab Report
I
HEPWT: V89-02421.0
r
SAnPLE
L
.
1
_I
ELEHENT
H2 D.C.
280
<5
II
PROJECT: NONE GIVEN
Il s
Ba
Br
Cd
Ce
CO
Cr
CS
Eu
28
600
(1
(10
55
<I0
240
5
<2
Geochemical
Lab Report
hochr-Cku& Cuuipiy La.
130 Pcmknon Ave.
Nonh \/usouvrr, B.C.
V7P ZRS
(604)985-0681 Trkx 04-352667
I
REPORT: V89-02421.0
I
SAHPLE
NUtIBER
I
ELEHENT
UNITS
1
I
1
Fe
PCT
1.9
22.0
R2 D.C.
02 SPUNKY
PROJECT: NONE GIVEN
I
Hf
PP~
Ir
PPB
La
PPH
6
9
<lo0
<I00
27
987
Lu
PPH
HO
P P ~
<0.5
1.2
66
<2
Na
PC T
Ni
PPH
Kb
PPH
Sb
PPH
2.60
0.44
<50
180
160
(24
1.2
0.2
I
NUHBER
1
R2 D.C.
1
ELERENT
UNITS
I
Tb
Ts
PPH
Sn
PPH
Ta
PPI
PPH
PPH
PPH
<I0
2.4
<200
19
Se
Sn
PROJECT: NONE GIVEN
I
-4
<1
<20
Th
PPH
20.0
U
PPH
18.0
BuW-Ckgg & Cornpay Ltd.
I30 Prrnknon Avr.
Nonh Vmouvrc, B.C.
V7P 2K5
(601) 985- 0681 T c h 01-352667
L
f
H2 D.C.
ELEHENT
UNITS
5.3
10.0
PAGE
U
iC
PPn
Yb
PPH
Zn
PPH
4
<5
430
Geochemical
Lab Report
I
REPORT: V89-02421.0
SAWLE
NUHBER
Sc
PPH
Geochemical
Lab Report
HEPOHT: V89-02421.0
SAHPLE
PAGE 10
I
& u & ~ - C kY~Cu~upanyLid.
I30 PrrnbertoliAvr.
Nonh Vaicouvrr, B.C.
V7P 2K5
(601) 985-0681Telcx 04-352667
C
PAGE 1 A
2r
PPH
<500
Pt
PPB
PROJECT: NONE GIVEN
Pd
PPB
Au
PPB
Cu
PPH
Ni
Cr
PPH
PP~
PAGE 10