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ABERFORD RESOURCES LTD .
GEOLOGICAL AND GEOCHEMICAL REPORT
ON THE
DEW GROUP
CONSISTING OF THE DEW 1 and 3 CLAIMS
New Westminster Mining Division
NTS 92H/6E
West Longitude 121' 10' North Latitude 49' 27'
G E O L O G I C A L B R A N C H r A S S E S S M E N T R E P O R T
Report Date: November, 1983
L+ Report No: 21-83
By: J. E. Robinson
TABLE OF CONTENTS
A. INTRODUCTION
Page
1. Geography and Physiography 2. Property DefinitAon 3. Program Summary
B. GEOLOGY
1. Ladner Group 2. Dewdney Creek Group 3. Needle Peak Pluton 4. Other Intrusive Rocks
C. STRUCTURE
D. MINERALIZATION
E . GEOCHEMISTRY 1. Sampling Method
a) Soils b) Heavy Mineral Panned Concentrates c) Stream Sediment
2. Laboratory Methods a) Preparation b) Determination
3. Results 4. Discussion
F- CONCLUSIONS AND RECOMMENDATIONS
REFERENCES
LIST OF FIGURES
FIGURE 1 General Location of the DEW Group
FIGURE 2 Detailed Location of the DEW Group
FIGURE 3 Cross Section of the Northern Cascade System
FIGURE 4 The Coquihalla Gold Belt
L FIGURE 5 Soil Gold and Arsenic Geochemistry
FIGURE 6 Stream Sediment and Heavy Mineral Geochemistry 1
LIST OF PLATES (In Back Pocket)
PLATE 1 Soil Geochemical Grid with Values
PLATE 2 Geology, DEW Claims
APPENDICES
APPENDIX A Statement of Expenditures
APPENDIX B Geochemical Laboratory Reports
APPENDIX C Soil Sample Descriptions
APPENDIX D Rock Sample Descriptions
APPENDIX E Stream Sediment and Heavy Mineral Samples
APPENDIX F Statement of Qualifications
A. INTRODUCTION
1. Geography and Physiography
The forty unit DEW Group is situated within the central part of the
Cascade Mountains, twenty kilometres northeast of Hope, B.C. on Dewdney
Creek (Figure 1). Access to the property is gained via the Dewdney
Creek forestry road which joins the Coquihalla road about 24 kilometres
from Hope. Old logging roads, many of which are passable by 4 wheel
drive vehicle, provide excellent access to the western half of the group
(Figure 2). Upgrading of the impassable roads would require a minimal
amount of work.
The depth of overburden varies considerably on the property. East
of Snider Creek, till cover is minimal with good rock exposure. Snider
Creek, a paleotopographic depression, contains a thick deposit of till,
with exposed thicknesses in excess of 15 metres. West of Snider Creek,
a moderate amount of till cover is suggested by the rolling topography,
and the rarity of outcrop.
The grid was placed on the north facing slope of Snider Mountain,
facing the Dewdney Creek Valley. Steeply incised Snider Creek modifies
this to produce a slope facing northeast on the west side of Snider
Creek, and a northwest facing slope on the east side. Relief is
moderate to steep with elevations ranging from 600 metres to 1400 metres
above sea level.
\
The eastern half of the claims is covered by an old burn, now
heavily overgrown, containing small isolated stands of cedar, spruce and
hemlock. Clear cut logging has been carried out on the western half of
the claims.
2. Property Definition
The DEW claims were originally staked in 1981 by a predecessor
company of Aberford Resources Ltd. The claims were centred over
drainages which yielded anomalous gold and tungsten values in heavy
mineral and stream sediment samples (White, 1982). Field work carried
out by Aberford Resources Ltd. in 1982 identified an area of elevated
arsenic soil geochemistry on the DEW 3 claim. Geological mapping
indicated that this area corresponds to the contact between fine
volcanoclastic sedimentary rocks of the Lower to Upper Jurassic age
Ladner Group, and a predominantly granitic suite of rocks forming a
narrow extension of the Eocene to Miocene age Needle Peak Pluton. A
more detailed program, the subject of this report, was carried out in
August, 1983
Several claim groups exist both to the northwest and southeast of the
property. To the southeast, on the divide between Dewdney Creek and the
Tulameen River, Treasure Mountain is covered by several crown granted
claims, remnants of an old lead-silver camp worked in the early part of
the century. The recent opening of the Carolin Gold Mine (1981) to the
northwest has been associated with the staking of a large acreage of
land. Aquarius Resources Ltd. of Edmonton controls much of the ground
along the Coquihalla Serpentine belt - Ladner Group contact (Hozameen fault), which hosts the gold mineraliztion at Carolin. The western
boundary of the DEW property adjoins this claim group.
The DEW 1 and 3 claims, located in the New Westminster Mining
Division, NTS 92H/6~ consist of:
- Two 20 unit claims = 1,000 hectares or 2,471.2 acres
Record # 1345 and 1347 respectively
- Located by M. Dawson, agent for Aberford Resources (formerly Pan Ocean Oil Ltd.)
- Recorded on November 12, 1981 - Due November 12, 1983
3. Program Summary
In August, 1983, a two-week field program involving geological
mapping and geochemical sampling was undertaken to further define the
arsenic anomaly identified in the western most soil geochemistry line of
the 1982 program.
A chained and flagged grid approximately 2 kilometres square in
area was put in on the western half of the DEW 3 claim (refer to Plate
1). The grid extends for 1 kilometre east of the western boundary of
DEW 3, and covers the entire area between the claims north and south
boundaries. A total of 168 soil samples were collected at 100 metre
stations on 16 kilometres of grid lines spaced 100 metres apart. In
addition, 34 rock chip samples, 9 heavy mineral panned concentrates, and
13 stream sediment samples were collected for analysis.
Geological mapping on a scale of 1:10,000 was carried out on the 2
kilometre square grid area to better define the location and nature of
the contact between the Ladner Group sediments and the Needle Peak
Pluton.
B. GEOLOGY
1. Ladner Group
The area is underlain by the Lower to Middle Jurassic age Ladner
Group rocks which are part of the Tyaughton-Methow trough (Figure 3) in
the northern Cascade system. This group occupies a northwest trending
belt extending from the international boundary to Boston Bar in the
north. The group is a thick marine succession consisting of slate,
pelite, sandstone consisting of interbedded andesitic to dacitic
volcanic detritus, minor conglomerate, tuffaceous greywacke and local
volcanic flows.
FIGURE 3:
Cross Section of the
Northern Cascade System.
On the property (refer to Plate 2 in back pocket), Ladner Group
rocks are represented by dark grey to black argillite, slate and
greywacke, with a few interbeds and small lenses of pebbly wacke and
conglomerate. Bedding is generally vertical with local steep easterly
or westerly dips. A prominent slaty cleavage parallel or sub-parallel
to bedding is locally evident.
Adjacent to the Needle Peak Pluton, the Ladner Group has been
partly converted to a dark grey to black, generally pyritic, siliceous
hornfels which locally contains porphyroblasts of andalusite up to 2mm
in size.
The Ladner Group is believed to represent a distal turbidite
sequence. Although not seen on the property, well preserved sedimentary
structures (cross-bedding, groove and load casts) indicate turbidity
current deposition with an eastern provenance (Ray, 1982).
2. Dewdney Creek Group
Regionally overlying the Ladner Group is the Upper Jurassic age
Dewdney Creek Group. This group comprises a sequence of massive, poorly
bedded sandstone which is comprised of green volcanic detritus, poorly
sorted polymictic conglomerate, and laminated greywacke. Though not
seen on the property, it is well exposed immediately east of the Needle
Peak Pluton.
3. Needle Peak Pluton
The Eocene to Miocene age Needle Peak Pluton, a predominantly
granitic suite of rocks, intrudes the Ladner Group, and underlies the
east half of the claims. Four phases of this pluton have been seen on
the property: a marginal hornblende diorite phase, a biotite - + hornblende granodiorite phase, minor hornblende-biotite quartz diorite,
and minor porphyritic (k-feldspar) quartz monzonite. These phases
probably represent the differentiation of a single magma, multi-stage
intrusive event (Belik, 1982).
4. Other Intrusive Rocks
The Ladner .Group is cut by two main sill or dyke forming intrusive
rocks (Ray, 1983). One is a generally fine grained mafic to ultramafic
intrusive which forms sills, dykes and irregular masses. The other is a
light brown coloured quartz feldspar porphyry system which also forms
sills and dykes. This generally granitic system has been shown to
attain a syenitic composition in some locations. Ray (1982) cites two
references to Cairnes (1924, G.S.C. Mem. 139; 1929, G.S.C. Summ. Report,
Part A) who considered these bodies to be genetically related to
reef-hosted gold in the area. Regionally, these dykes have been found
to contain pyrite, arsenopyrite and gold, though only pyrite was found
in the dykes on the property. Quartz veining, often containes minor
pyrite, arsenopyrite and gold is associated with this intrusive.
Observations made on the DEW claims iadicate that the source of these
feldspar porphyry dykes may have been the Needle Peak Pluton. Most of
the dykes encountered ranges from lOcm to 20cm in width, ocassionally
being as wide as 50cm. However, a 20 metre wide, coarse grained
feldspar-quartz dyke was encountered near station 1E-13s on the grid.
Though unmineralized, this dyke is compositionally very similar to the
finer grained mineralized feldspar porphyry dykes.
C. STRUCTURE
Major northwest trending transverse and strike-slip faults exhibiting '
large displacements occur within the Tyaughton-Methow trough, transecting
the area of the DEW claims (Figure 4). The two most significant are the
east Hozameen fault and the Chewanten fault. The east Hozameen fault, which
occurs about 1 kilometre west of the claim group, separates the Coquihalla
Serpentine Belt to the west from the Ladner Group. Along this contact, the
Ladner Group hosts the mineralization in the Coquihalla Gold Belt (Figure
4). The Chewanten fault, occurring about 5 kilometres to the east of the
KILOMETRES - +
A . . - - . . . + -
0 CO(IUIHALLA GROUP
0 NEEDLE PEAK PLUTON
0 PASAYTEN GROUP a JACKASS MOUNTAIN GROUP
0 DEWDNEY CREEK GROUP
LEGEND
LADNER GROUP
0 COOUIHALLA SERPENTINE BELT
0 FOLIATED GRANODIORITE
0 HOZAMEEN GROUP 0 APPROX. LOCATION OF DEW CLAIMS
PAST AND PRESENT GOLD PRODUCERS
1 = EMANCIPATION 4 = PIPESTEM
2 = AURUM 5 -WARD
X REPORTED GOLD OCCURRENCES
6 =BROKEN H I L L 7 = SNOWSTORM 9 = RUSH OF THE BULL 10 =GOLDEN CACHE
12 = MURPHY 13 =GEM 15 = HOME X I 6 =NORM AND GEORGIA I 8 = RODDICK 19 = M A R V E L 21 = MAJESTIC 23 =GOLO CORD
22 =GOLO COIN
3 = IDAHO ZONE (CAROLIN MINE)
8 = MONTANA 11 = McMASTER ZONE 14 = STAR
2 17 = EMIGRANT 20 = SPUZ A, 8. G
A N 0 MONUMENT
FIGURE 4: Coquiha l la Gold B e l t ( a f t e r Ray, 1983)
claim group, separates Ladner Group rocks from the Upper Cretaceous age
Pasayten sedimentary rocks which lie to the east of the fault.
A third fault, trending northwest, transects the DEW claims. This fault
has been mapped as the boundary between the Ladner Group and the Needle Peak
Pluton in the vicinity of the claim group (Monger, 1970) but observations on
the property indicate that this is not strictly true. A halo of hornfelsed
sedimentary rocks of the Ladner Group, locally metamorphosed to andalusite
grade, occurs adjacent to the pluton, and actual intrusive contacts can be
identified in outcrop. Therefore, this fault either postdates or was
synchronous with the intrusive event.
Folds on the property are generally tight and isoclinal, as indicated
by the near vertical east and west dipping strata. Axial planes trend
north-south. Drag folding, possibly related to faulting, is well exposed in
Snider Creek.
D MINERALIZATION
The most interesting mineralization noted on the property occurs in
quartz veining associated with feldspar porphyry dykes hosted by the Ladner
Group. All deposits and occurrences cited by Ray (1983) within the
Coquihalla Gold Belt show gold mineralization of the Ladner Group
accompanied by the introduction of silica, either as quartz veins or as
diffuse silicification, and several (including one past producer) exhibit,
the felsite porphyry association. Examples, shown on Figure 4 of this i
report are:
Ward deposit (4,199 oz Au), producer No. 5
Rush of the Bull, occurrence No. 9
Emigrant, occurrence No. 17
Spuz, A, B, G and Monument, occurrence No. 20
On the DEW claims, a rock chip sample of this type of quartz vein
contained highly anomalous amounts of gold and arsenic. In addition, this
association is likely responsible for the highly anomalous soil sample at
station 5W-18s because a "swarm" of feldspar porphyry dykes occurs at this
location.
Previous work on the property (see Belik, 1982) revealed minor scheelite
within quartz veining associated with a pyritic felsic dyke in Dewdney
Creek. A composite sample of the dyke geochemically assayed only 2ppm
tungsten. The significance of tungsten mineralization is not known, but it
is interesting to note that gold mineralization in both the Idaho Zone
(Carolin Mine, producer #3 on Figure 4) and the Spuz occurrence is
associated with weak tungsten geochemical anomalies.
A relatively strong 'pyrite halo' is evident peripheral to the Needle
Peak Pluton. Here, pyrite and pyrrhotite, in amounts up to lo%, and rare
chalcopyrite occur as fine - grained disseminations and fracture fillings within Ladner Group and Dewdney Creek Group sediments. Similar mineral-
ization can be seen in the hornfels adjacent to the pluton, and locally
within diorite along the margins of the pluton.
Mineralization is rare within the Needle Peak Pluton. The pluton
locally contains widely spaced, narrow quartz veins with minor pyrite. \
Fracturing is poorly developed but locally exceeds 10 fractures per metre
near the margins of the pluton. Narrow northeast - trending quartz - sericite - pyrite alteration zones were noted at a few locations in 1982.
E . GEOCHEMISTRY
All soil, rock chip and stream sediment samples were geochemically
analysed for gold, arsenic and tungsten. Heavy mineral panned concentrates
were analysed for gold, arsenic, tungsten, silver, copper, lead, and zinc.
All analyses were performed by Bondar-Clegg and Company Ltd., located at 130
Pemberton Avenue, North Vancouver, B.C.
1. Sampling Method
a) Soils
A total of 168 soil samples were collected during the 1983 program.
Samples were collected by digging a hole, using Estwing rock pick
shovels, to a depth of 15-30cm. The "B" horizon was sampled except
where soil development necessitated sampling the "B-C" horizon. Samples
were placed in standard kraft envelopes. Orange and blue flagging tape
was secured at each grid station, and the station number was indicated
on the flag with permanent ink felt marker.
b) Heavy Mineral Panned Concentrates
A total of 9 heavy mineral panned concentrate (HVKL) samples were taken
from the active part of the stream bed at locations where a decrease in
stream velocity allowed for sediment accumulation (ie. pools, bars). A
vertical section of sediments was shoveled into a /I6 mesh screen until
sufficient -6 mesh fraction was obtained to completely fill a standard
38.lcm (15 inch) steel gold pan. The -6 mesh fraction was panned to a
volume of 30ml to 50ml of heavy material, and transferred to 70ml ,
plastic snap-top bottles.
c) Stream Sediments
A total of 13 stream sediment samples were collected from Snider Creek
and its tributaries. Samples were taken from the active part of the
stream bed, and placed in standard waterproof kraft envelopes.
2. Laboratory Methods
a) Preparation '
All soil and stream sediment samples were dried, then seived to obtain a
-80 mesh fraction. Rock samples were crushed to pea size fragments
(about 0.5cm), then a 0.23kg (0.5 lb) split was pulverized to -100 mesh.
All heavy mineral panned concentrate samples were completely
pulverized.
b) Determination
Analytical determinations were conducted as follows:
Element Extraction Method Results
Cu,Pb,Zn,Ag ~ o t HNO~ Atomic Absorption PPM
As Nitric Perchloric Colourimetric PPM
W Carbonate Fusion Colourimetric PPM
Au Aqua Regia Fire Assay A.A. PPB
3. Results
\
a) Soils
Visual examination of the analytical results for gold, arsenic and
tungsten was used to determine appropriate value designations for
contour intervals. Gold in soils, Figure 5, is contoured at 15ppb and
20ppb, which correspond to the following designations:
Background <15ppb
Possibly Anomalous 15 - <20ppb Definitely Anomalous >20ppb
Arsenic in soils, Figure 5, is contoured at 50ppm and lOOppm, which are
designated as follows:
Background <50ppm
Possibly Anomalous 50 - <100ppm Anomalous >lOOppm
Contour intervals were selected on a trial-and-error basis to avoid
the production of "Bullseye" anomalies; a relatively high value for the
first contour was selected, with successively lower contour intervals
attempted until one was found that produced reasonable results (ie. an
area of high values contained within a halo of lower values). This
technique worked well with both gold and arsenic. However, the choice
of a 15ppb contour interval for gold is controversial because the
detection limit for this element is 5ppb + - 5ppb.
Tungsten results for soils were not plotted or contoured because no
values significantly above a background of 2-3ppm were obtained.
Analytical results are contained in the geochemical lab reports
(Appendix 11).
b) Stream Sediment and Heavy Mineral Samples
Threshold values for gold and arsenic are indicated below. Valuep
greater than those shown are considered anomalous.
Gold Arsenic
Stream Sediments ~ O P P ~ ~ O P P ~
Heavy Minerals ~ O P P ~ ~ O P P ~
The locations of all samples and their values are shown on Figure 6.
L E G E N D
0 STREAM SEDIMENT Au ( P P ~ ) A ~ ( P P ~ )
HEAVY MINERAL CONCENTRATE A u / A s / W A 9 /Cu/ Pb/ Zn
C L A I M LINE W I T H I.D. POSTS A N D CORNER POST
L
4. DISCUSSION
Arsenic in soils shows a good response across the central portion of the
grid. This east-west trending anomaly, 700 metres wide at its widest point,
contains two subparallel belts of strongly anomalous values on the east side
of the Creek. Both of these strongly anomalous belts are on the order of
lOOm wide. The northerly belt is at least 400 metres long and is open ended
to the east. The southerly belt is at least 200 metres long, however the
weak halo enveloping this belt continues westward across the creek. The
till cover in the creek and on the slope to the west presumably masks a
stronger response. A disconcerting note to the western extension of this
weak anomaly is that it follows the old logging road remarkably well. If
the fill for this road was taken from a pit on the east side of Snider
Creek, a false anomaly could be created adjacent to the road bed.
Gold anomalies correspond well to the delineated arsenic anomaly belt.
Station 1E - 700s has the highest value of 120ppb Au with 600ppm As. Several moderately strong spot anomalies in gold also occur on the east side
of the creek (Station 1E-10s @ 55ppb Au, and 3W-12s @ 35ppb Au), and have
weakly anomalous halos extending downslope towards Snider Creek.
On the west side of the creek, the narrow central grid arsenic anomaly
corresponds to a zone of low to moderate gold values that is at least 300
metres wide and open ended to the west. Anomalies in this area are l
supported by stream sediment samples JERSS-3 and 4 (40ppb Au and 35ppb Au
respectively), both of which are anomalous in gold and arsenic.
A similar situation exists in the extreme northwest corner of the grid.
Two stations have strongly anomalous Au + As responses (station 8W-2s @
215ppb Au + 190ppm As; station 6+50W-3s @ 160ppb Au + 180ppm As), encompassed by a larger area of low to moderate gold values. Gold responds
over an area that is about 200m wide, and being open ended to the west, is
at least 200 metres long.
On the southern portion of the grid, gold anomalies in soils are
substantiated by anomalous stream sediment and heavy mineral samples. In
soils, gold and arsenic are both strongly anomalous only at station 5W-18s
(Au 150ppb, As 600ppm). Stream sediment and heavy mineral samples taken
from the upper reaches of Snider Creek restrict this anomaly to the Creek's
west branch, and cut it off just downstream of line 7W (heavy mineral sample
KR-6).
A single rock sample was anomalous in both gold and arsenic (JER-019 @
265ppb Au + >1000ppm As). This sample was taken approximately 100 metres
upstream of the main Snider Creek crossing, and consisted of quartz veining
associated with some pyritic feldspar porphyry dyking. A sample of the dyke
taken at the same location contained no gold (JER-018 @ <5ppb Au, 32ppm As).
Two other samples of this type of dyke also failed to respond for gold:
JER-013, taken from a 20 metres wide dyke adjacent to the Needle Pead Pluton
and JER-015, taken at the western edge of the property.
Samples of the quartz veining associated with these dykes showed
varying responses to gold. Sample JER-004 (80ppb Au, 37ppm As), taken from
the location of the feldspar porphyry dyke "swarm" on line 5W, was weakly
mineralized with gold, while JER-009 (5ppb Au, 47ppm As) responded only with
a background level of gold.
i
F. CONCLUSIONS AND RECOMMENDATIONS
Gold mineralization on the property appears to be restricted to the
quartz veining associated with the feldspar porphyry dykes. This conclusion
is supported by the results of the soil geochemistry which indicate that
mineralized features cross-cut the northerly trending structural fabric of
the area, and by the few rock samples that were taken.
Additional work involving intensive rock sampling, and detailed soil
geochemistry is recommended. Rock sampling should concentrate on the quartz
veins associated with the felsite dykes. Two additional lines of soil
samples should be put in on the DEW-3 claim to cutoff the open ended
anomalies that exist. One line would be along the west boundary of DEW-3,
and another added to the east side of the existing grid.
REFERENCES
L Belik, G.D., (1982): Geological and Geochemical Report on the DEW 1-4 Claims,
New Westminster Mining Division, British Columbia, (prepared for Aberford Resources Ltd .) .
Monger, J.W.H., (1970):. Hope Map-Area, West Half (92H), British Columbia; Geological Survey of Canada, Paper 69-47.
Ray, G.E., (1982): "Carolin Mine - Coquihalla Gold Belt Project", British Columbia Ministry of Energy, Mines and Petroleum Resources, Geological Fieldwork, 1981. Paper 1982-1, pp. 87-101.
Ray, G.E., (1983): "Carolin Mine - Coquihalla Gold Belt Project", British Columbia Ministry of Energy, Mines and Petroleum Resources, Geological Fieldwork, 1982. Paper 1983-1, pp. 63-84.
White, G.D. (1982): "DEW Claims", Merritt Volcanogenic Project 1981: Geology, Geochemistry and Geophysics, pp. 54-60.
APPENDIX A
Exhibit A Statement of Expenditures
EXHIBIT A
Statement of Expenditures Dew Group
New Westminister M.D., NTS 92~16 Southwestern British Columbia
WAGES
B. W. Smee, Exploration Supervisor Travel August 22 - 1 day @ $300.00 Field Work August 23-25 - 3 days @ $300.00
J. E. Robinson, Geologist Travel August 15, August 29 - 2 days @ $125.00 Field Work August 17,19, 21-28
10 days @ $125.00 Report Preparation - 5 days @ $125.00
K. L. Reading, Prospector Travel August 19, August 20 - 2 days @ $110.00 Field Work August 21-28 - 8 days @ $110.00
TOTAL WAGES
L ACCOMMODATION
MEALS
FUEL
TRUCK RENTAL - $30.00/day X 12 days - $30.00/day X 4 days
FIELD EQUIPMENT
REPORT COST - Typing, reproduction, drafting
Statement of Expenditures Dew Group
Geochemical Analysis
168 Soil Geochemistry @ $14.50/sample $2,436 .OO Sample
Au As W . Prep. Retention $6.00 + $3.25 + $4.25 + $0.75 + $0.25 = $14.50/sample
34 Rock Geochemistry @ $16.60/sample $ 564.40 Sample
Au As W Prep. Retention $6.00 + $3.25 + $4.25 + $2.75 + $0.35 = $16.60/sample
9 Heavy Mineral Concentrates @ $20.00/sample $ 180.00
Au As W A8 Cu Pb $6.00 + $3.25 + $4.25 + $1.90 + $0.95 + $0.95 + Zn Prep.
$0.95 + $1.75 = $20.00/sample
13 Stream Sediment Geochemistry @ $14.50/sample $ 188.50 Sample
Au As W Prep. Retention
'L $6.00 + $3.25 + $4.25 + $0.75 + $0.25 = $14.50/sample
$3,368.90
122 Single Datum Transmission @ $O.lO/datum
102 Multiple Datum Transmission @ $0.25/datum
2 Data Set Charge @ $2.50
Summary of Expenditures Dew Group
WAGES
ACCOMMODATION
MEALS
FUEL
TRUCK RENTALS
FIELD EQUIPMENT
REPORT COST
GEOCHEMICAL ANALYSIS
TOTAL EXPENDITURE
PAC Account Transferral Request *16.63% of value of assessment work
DEW GROUP
DEW 1 20 units @ $lOO.OO/unit for 1 year = $2,000 .OO 20 units @ $200.00/unit for 1 year = 4,000 .OO
DEW 3 20 units @ $100.00/unit for 1 year = 2,000 .OO 20 units @ $200.00/unit for 1 year = 4,000 .OO
APPENDIX B
Geochemical Laboratory Results
B a d u ~ 6 C o c n p n y u d .
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j 5 DEW 125-02U 3 1Q4 5 i 5 DEW 13s-02W 3 1 b .< 5
L : 5 DEW 14s-09Y 2 28 ( 5 ! 5 IIEU 15s-02U 3 2B 15
, i S DEW 16s-02U 3 36 10 .--------.-. - ... . -.-..---. *---- .
3
--&COIIIPU)rM
I 3 0 PmMon Avc. Nmh Vmmuver. B.C. CaMda V7P ZRS Phone: (604) 985-0681 Tdex: LW352667
BONDAR-CLEGG - G e o c
Lal
r---l---l---- ..... ....- ---". .......... ..-.
, REIY3KT: 123-2350 PR'h'OJECT: DEY .- < .......................... ......--......... .- . . ... ........................
.. .................................................... .... ....................
SAHPLE ELEHENT Cu Pb Zn Ad Y As Au MEER UNITS PPH. FW PPH ~ ~ f l PPH PM FPB ...... .. .... . -. ...............-.... ..............................................................................
-.-- "-." ..-......... . . . -. ..... ....-.... -- .
2 13 c: 5 S IIEW 185-02bl 3 27 10 S DEW 195-02;6 3 22 10 S MU 125-05# 2 25 10
3 20 10 - ..... . " ................... .. ...................... .- ........ ........-.... - .
S Mbl 145-05W 2 22 10 S BEW 15s-05W 2 43 69 S ItEM 165-05M 2 30 15 S DEW 17s-05W 2 13 5
EY 18s-05Y 5 609 .--.- ... - 150 ............. -. ............ . -- -- ...... " --- -.-. .. - . " -
S N Y 195-0561 3 A J 10 'Y7
j SL3YBL 9 I S 5 S L3!J 100s i 2 17 f: 5
j S L3Y 2009 ' 2 12 15
1 L3Y PREFIX , S 1700S(200'W) 2 14 10
4 L -.---,-.- - ----I ..-. ... --.----------
BOnd.rc1*01&Corn~~Ud. 130 Pmbenon Ave. Nonh Vancouver. B.C. C;ulada V7P 2R5 Phone: (600) 9850681 Tekx: 04-352667
-- REPORT: 123-2380- PROJECT: DEU - - - - PAGE 3 - - - - --- - - - - -----
SAHPLE ELEHENT Cu Pb Zn As U As Au _NUHEER__ _ UNITS-- PPH- - - f ~ n _ PPH FFH PFH PPH PPE - - - - - - -- -
,-.- 1 - -- -lll-lll.-ll- -- - - - - - - - - - - - - - - - - - --- - - --
130 Pantienon Ave. Noah Vancouver, 0.C Canada V7P ;RS Phone: (6041 985&81 Tckx: W-352M7
Geoc Lai
.... - ....... .- . . . . . .
- ....... + . . . . . . . - . . . . ....................... -. .... . . . . . . . . - - . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . - . - ..........................
SAHF'LE ELEMENT Cc; F'h Zn A5 A:. id As I. N'JRBEK_.". _SE!IT.?..u. F'F'H' E!!! F'FM PPB .... ".. .... .. .--. .. -.
+-.--.. ......... . ................ ...
: S 1E-,352 i S 1E-OIS 8 3 .<5 : Ci 1E-03s 9 4 15
' I , S 1E-04s 34 2 <S 2 5 .......... ... .................. ........
. . . . . . . . . . . . .......................... ...
: S 1E-06S 57 3 .< 5 S 1E-975 bO0 3 120
I ; S 1E-0% 9 40 c .< 5 I S 1E-OSS 72 3 5 1 i S IE-10s 55 4 50 , -.--.-.- . .......-. . ...... -. ....................... , ...-........ ..... ....-... ^I__.I_ ...... __ . . . . . . . . . . . . . . . . _ . . ........................... - . - - - -- ..
S If-11s 3 C.2 L 5 1 S 1E-12s 43 7 (Z C I.'
, ,
' S 1E-13s 40 3 (5 S 1E-14s 22 2 ( 5
20 5 (5 ................... . . . . . . . . . . . . . . . . . . . . . . . . . . . . - - . .......................... ( .--..-.-,- ..................... . .- . . . . . . . . . . . . . . -- . - .. - .... .........
1 S IE-16s 10 4 (5 S 1E-liS 10 7 .:-
'+- ! L .J
1 S AU-0+00S 17 2 (5 ! s AN-100s 3 24 L %: 5
. . . . . . . . . . . . . . . . .
48 5 5 20 3 5 37 4 i: 5
3 65 L 35 7 30 A 10
24 4 i 5
.. ............ -. . .. ...-.-..... ........................ -.........
180 2 160 42 2 30 17 5 10 2.0 3 5
7 47 A 25 ........................... . - ...... .
30 3 ,: 5 23 2 10
bZ 3 A t F L,
25 2 15 -,---.. ... .......... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ..-.......... I
-& C a a p u y Ud. 1W Pmbenon Ave Nonh Vancouver. B C Canada V7P 2R5
Geo Phone (W) 9R54631
Lz Tekx W35m7
..... . . . ...... - ; REPORT: 123-2443 PROJECT: DEW
. . . . . . . . . . . ...... . .............................. ............ .. . . . . . . . . . . . . . . . . ........ .. ..... .. -- ...__I.---..-- . . _. _
SAHPLE ELEMENT Cu Pb 2r1 fis As 13 Au FIUMBER .....__._... UNITS PPH PPM FPE FPM PPM FPH FPP ........ ....................... - . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
. . . . . . . . . . . . . . . . . _ ...-- _ .. .. . . - . . . .
' S 71d-13005 31 2 I? S 7W-1400s 38 4 25
1 S 715-15005 28 3 10
1 S 713-1500s 23 3 ( 5 1 - S 7H-37005 ---_ -- - - - - - - ---- - -- - -- --_ .----- 48 - - -. 4 -- - 10 . - - - -.- - - - - . _ i "--- - - ----" - - - - --- - - - - - - -- - - - - -
S N-1600s 10 4 (5 21 2 (5
B t
28 4 5 i I ' 5 PW-08s 48 5 25
S BW-09s z 1 -.--- __--- _._ _ _ 40 4 20 - . rl- --^--. - _ --- . . - - - - - - - -- ---- - - - . - - -
- -- - - - - - - .
i : S SW-10s 45 5 25 2 ; S 8W-11s 370 4 15 : S 6M-12s 24 3 E
5 ; S BW-13s 50 4 35
i L-3 PW-I?_S --_- - _ - ---_- - - - - - 2 1 3 10 - - -- - - - - - - -
I ? 4 20
20 4 (5 23 2 15
- - - - - - - - .
S 8H-10% 31 4 A -1 i
.)I
S 9M-200s ! 90 4 215 S 8W-300s 4 1 7 35 S BW-400s 4 0 2 10 S BW-500s
- - 24 - - - - 3 10 - - - - - - - - --- -- ---- -- - -
- - - - - -- - - - - - - - - . - -- - - - - - - - -- - - - -
S 2kl-500s 7 24 i 15 i S B1l-?ODs 63 4 25 I T JER SS1 24 3 0
T JER SS? 32 3 30 T JEE SS3 I I --_ - - - - - - - - - - - - -- - - - -- - 50 3 - - -- 40 - - - -- -- -- - - - - - - - - - -
I , - - - - - - - - - - - - - - - - -
T JER 554 7 36 A 35 I T KRB3 SS-2 13 4 15
T KR63 SS-3 25 3 ( 5 T RR93 5s-4 33 4 20 T Kg83 qS-5 21 5 c
I ---I. -2 ------ - - .. - -" . - - - - - 7 - -- .- - . --- --- - -- I
lkmdu43cK#&ColnpnyLld.
130 Pmbenon Ave Nonh \ m u v e r . B C Canrla V7P .K5 Phone (W)9850681 Tclex w352667
BONDAR-CLEGG
--------.-..-.-. ........... .- . .- .- . ..................... -- ..........
: REPORT: 123-2443 PROJECT: DEW .......................... ..... .... .......... .. . . . . . . . . . . . . . . . . . .-.. -- . . ................... -
SAHPLE ELEMENT Cu P i.--. ~uiz!~!! !-!%'IS .... ..FP$ !rn. ... .PO! P?? . F P ~ P P ~ .... PFP ....................... - -. ....... 7--------. -- . .. . . . . . . . . . . . . . . . . . . . ................. -. . . - .......... .- - - . - . - .- ..... ; T KR63 SS-6 A i 77 4 5 I T ~ ~ 8 3 ss-7 2e 4 10 : T KR83 SS-9 26 3 5 I 'I KR83 SS-9 30 4 20 I ! 37 7c
hL .'L. i .._r.t~e; _:st!? ......................................................................................... - ......... - . . . . . . . . . . . . . . . . . . . . . . . ? .. - .. - -. .... - . -. ... . - ....-.................. ................................................. . . . . . . . . . . . . . . . . . . . . . . . . . .
' R EMS-0003. 5 5 10 - : F: BUS-0002 . -
J ,, .: 5 I R MJS-0003 10 9 C
A
! R EMS-0004 7 9 A 25
i , I . Fi: BUS-0005 6 4 : - ---.. .... .I..-IX__.-.-.... ... .. ... - . _ . . . . . . . . - . . - -. ....... - -- -- -- . - .. .:5 , ,." -..... .................................. . . . . . . . . ......... - ... -. .... - ... - . -
j R PUS-000b 7 9 ..'C A A . J
I R WS-0007 4 1 4 I
i R EMS-0003 7 5 .: 5 - 4 i R BUS-0009 3 4 <5
R JER-001 13 9 f L -........- . . . . . . . . . . . ...... . . . . . . ... - .... .- ......................
A . . . . .
t: 5 ....... ...... . . , . - .... . - . . . . . . . . . . . . . . - .- -
: R JER-002 3 I 5 7 i I : R JER-004 L 37 4 80 1 P Jm-005 2 3 C
I 6.t
/ ,
F: IER-90b /? ,A 3 ( 5
' R JER-009 47 5 5 . ... ........ - .... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . , . . . . . . . . _ . . . . . . . . . . . . . i ' R JER-912 6 4 15
h' JEE-013 6 2 <Z R JER-014 3 2 ;:5
30 4 5 6 2 3:s
" ....... .. -. ............................ .- . . . . . . . . . . . . . . . ..... .... - . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .... .......................
62 4 35 R JEA-018 32 4 (5
> 1000 4 265 1 R JER-020 73 L A 3 10
i : R ER-1 . 3 2 (5 i L- .......... . . . . . . .
... ............ .......... ...... .- . . . . ..-.. . . . .- - . -. . - . - -.- .- -
34 4 10 %'q ,i 2 10
R KR-4 7 3 (5 ii' KR-5 $2 4 10
7 \:2 1. ( 5 ............ -. ..-... - -. ..... - - ... ......... --- ..... - - . -- ...-..-.- - . .- . -- .--. -. ... . . . . . . . . . . . . . . . . . . . - .......................... - - . -- . - . - - ... -. . -. - .. - .. .................................................... ..... . . . . . . . . . . . - . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
i R KR-7 17 3 20 R 1E-2S P 4 <5 % 1E-18s 3 2 ( 5 F; 16s-OOW 145 2 10
7 A 4 -.--------- ---.- . .....
I .
& Colnpnv Ud.
130 Pmbmon Ave North Vancouver. B C Cvlada V7P ?R< Phone. (604) 9RSWJI Tekx Oe35?&5'
:BONDARwCLEGG Geo La
PAGE 4 . . . . . . ............. - -. ....... - .. - .......... .. . . - ....... .
SAHPLE ELEHEHT Cu Pb Zn A5 As tJ Au 1 NUMBER UNITS - - - - - - - - " - PPd PPH PPH PFM PPH PkH PFE
- - - - - - - - - - - - - - - - - - - - --- -- ------- - - - - - - - * ---
APPENDIX C
Soil Sample Descriptions
DEW CLAIMS - 1983 SOIL SAMPLES
S t a t i o n
0s- 1 W
1s-1W
2 S- 1 W
3s-1W
4s-1W
5s-1W
6 S- 1 W
7s-1W
8s-1W
9s-1W
10s-1W
11s-1W
Horizon Descript ion
Orange, loose , granular t ex tu re
Depth
15cm
15-20cm
20cm
20-30cm
20-30cm
30cm
25cm
20-25cm
30cm
30cm
25cm
15-25cm
Orange, loose, granular
Orange, loose, granular t ex tu re
Orange, loose, granular t ex tu re
Orange, loose , granular t ex tu re
Brown, organic r i c h
Orange, loose, granular
Orange, loose, granular
Orange, loose , granular
Orange, loose, granular
Orange, loose , granular
Orange, granular contining much monzo- d i o r i t e rubble
Orange, granular with much monzodiorite
Orange, loose , granular
Orange, loose, granular
Orange, loose , granular
Orange, loose , granular
Orange with monsodirotie and a g r i l l i t e rubble, grey
Orange, granular
Dark brown, high organic
Black-brown, organic r i c h , g rave l ly with monzod io r i t e / a rg i l l i t e rubble
Orange-brown, granular with rubble of f e l s i c dyke and a r g i l l i t e
DEW CLAIMS - 1983 SOIL SAMPLES
S t a t i o n Horizon Descr ip t ion Depth
23) 17s-OW B Orange with rubble of monsodiori te and 15-25cm . f e l s i c dyke
24) 0s-2W B Orange, loose , g ranular 25cm
25) 1s-2W B Orange, loose , g ranu la r 20cm
26) 2s-2W B orange, loose , g ranular 20-25cm
27) 3s-2W B ? Light orange-brown, poss ib l e s o i l disrup- 20cm t i o n by bul ldozer
28) 4s-2W B-C Thin orange horizon over grey-brown, poss ib l e f i r e ash
29) 5s-2W B Orange, l oose , g ranu la r 15-20cm
30) 6s-2W B Orange. P a r t i a l development of 'A' horizon 15-20cm a r a r e occurrence
31) 7s-2W B Orange below we l l developed 'A' 15cm
32) 8s-2W B Orange \-
20cm
33) 9s-2W B Orange 20cm
34) 10s-2W B Orange 30cm
35) 11s-2W B Orange, g ranu la r , a r e a d is rupted by old 15cm bul ldozer work, organic l a y e r below we l l l e v e l 'B'
Orange, granular 20cm
Orange, s o i l c o l l e c t e d between c l a s t s i n 25cm monzodiorite t a l u s s lope
I n f o r e s t with good s o i l development, 25cm orange, granular
Orange, g ranu la r , poss ib l e c a t d i s r u p t i o n 15-20cm
Orange, granular 15-20cm
Orange, taken 20m e a s t of s t a t i o n due t o 18cm extens ive washout. A t l e a s t 40 f t . till
Orange, high c l a y content 15cm
DEW CLAIMS - 1983 1 SOIL SAMPLES
: t3"
I S t a t i o n Horizon I
Descript ion Depth
Brown, high c l ay , pebbly, c l ay bed a t 20cm
Orange s o i l a t sur face of p y r i t i c Ladner cross-cut by many f e l s i c dykes
Orange, granular , 40' s lope
Orange, granular , 40' s lope
47) 16s-5W till Taken i n broad, bul ldozer leveled area . very sandy
Orange, granular
Orange, granular
Orange, granular
Orange, granular
Brownlorange i n overgrown a rea , high organics
Orangelbrown moderate organics a s r o o t l e t s
Light brown/orange with moderate organics a s r o o t l e t s
Orange - low organics a s r o o t l e t s
Orange-brown, moderate c l ay content
Orange, shallow s o i l above Ladner, halfway up stream bank
Orange-brown, g rave l ly - poss ib le s o i l d i s rup t ion
Orange, pebbly
Light brown-orange, gravel ly , abundant till
Bright orange above till
Orange with moderate c l ay content
DEW CLAIMS - 1983 SOIL SAMPLES
S t a t i o n Horizon
Rock
Descr ip t ion
Dark golden brown, high organics wi th many Ladner fragments
Altered, dyked a r g i l l i t e
Orange above Ladner
Orange
Orange
Orange
Orange over monzodiorite
Orange, many angular Ladner c l a s t s
Orange with organics as r o o t l e t s
Orange wi th some lower greylbrown
Orange with high organics
Orange wi th A r g i l l i t e fragments
Orange
Orange
78) 5s-1E B
79) 4s-1E Light brown, high organics as r o o t l e t s
80) 3s-1E B Orange
81) 2s-1E Rock Hornfelsed a r g i l l i t e with qua r t z ve ins
82) 1s-1E B Orange
83) 0s-1E B Orange
Depth
25cm
APPENDIX D
Rock Sample Descriptions
DEW CLAIMS - 1983 ROCK SAMPLES
Submitted for Geochemical Analysis (Au, Ag , W)
Sample
JER Series
001
Location
15+50S - 6W
Description
Rose quartz vein with silicified argillitel quartz breccia
Pyritic hornfelsed argillite
Silicified argillitelquartz breccia with quartz vein
Hornfelsed argillite
Interbedded argillite and wacke
Silicified argillitelquartz breccia
Pebbly arenite - pebbles zoned in 3-4cm layers about 15cm apart
Orange weathered, coarse grained felsic dyke
Coarse lithic wacke
Road at West boundary, Dew 1
Rusty, hydrothermally altered pyritic felsic dyke with quartz veining
Hornfelsed, pyritic argillite in contact with monzodiorite intrusive
Highly pyritic, hornfelsed argillite adjacent to monzodiorite contact
lOOm upstream from Snider Ck crossing
Pyritic, locally altered felsic dyke with: quartz veining
lOOm upstream from Snider Ck crossing
Silicified, sheared argillitelquartz breccia
Bottom of Waterfall Quartz vein in shear separating blocks of Ladner
KR Series
KR- 1 Pyritic argillite
Pyritic argillite
Pyritic argillite
DEW CLAIMS - 1983 ROCK SAMPLES
L*Y Geochemical Analysis (Au, Ag, W)
Sample Locat i o n Descr ip t ion
KR S e r i e s
KR- 4 2W - 18s approx. A r g i l l i t e i n c reek
KR-5 Line 7W cross ing Quartz veined, a l t e r e d , p y r i t i c d i o r i t e west branch Snider Ck
KR-6 Approx. 7W - 14s P y r i t i c d i o r i t e
KR-7 Approx. 6W - 1s i n Conglomerate of up t o lcm quar tz and a r g i l l i t e small e a s t flowing and a r e n i t e c l a s t s . P y r i t i c t r i b . of Snider Ck
BWS S e r i e s
BWS-0001 10s - 1+20E Sulphide r i c h boulder ( f l o a t ? ) of ho rn fe l s - sediments ( looks l i k e a volcanic)
Breccia with abundant accompanying qua r t z ve in ing specimens from f l o a t , but c l o s e t o bed- rock source
From con tac t of sediments and f e l s i c dyke, bo th of which a r e sulphide-r ich. Sample from out- crop near base of t r e e on edge of f o r e s t - l o c a t i o n f lagged
Highly a l t e r e d and veined sediment - a r e a f lagged
Outcrop of h ighly a l t e r e d and veined sediment a r ea f lagged
Highly a l t e r e d sediment conta in ing abundant p y r i t e - could be f l o a t - a r e a flagged
Highly a l t e r e d sediment wi th abundant qua r t z ve in ing and Fe s t a i n . Vugs f i l l e d with a black powdery substance
Weakly a l t e r e d sediment - minor veining - a r e a f lagged
Sample of f l o a t above outcrop c lose t o anomal- ous s o i l samples. Highly p y r i t i z e d a l t e r e d sediment. Near edge of t r e e s . Area f lagged
APPENDIX E
Stream Sediment Sam~les
DEW CLAIMS - 1983 STREAM SEDIMENT SAMPLES
JER SS-1
JER SS-2
JER SS-3
JER SS-4
KR- 1
KR-2
KR- 3
KR- 4
KR- 5
KR- 7
KR-8
2W - 17+81S East branch of Snider Creek
5W - 14+80S West branch Snider Creek
8W - %28S East flowing t r i b . of Snider Creek
8W - 12+97S Eas t flowing t r i b . of Snider Creek
Eas t branch of Snider Creek
I n e a s t branch
4W - 15+75S Samll t r i b . of e a s t branch
Snider Creek, midway between branches and creek cross ing
Snider Creek a t road c r o s s i n g
Snider c reek , midway between road cross ing and base l i n e
Snider Creek, about lOOm south of base l i n e
Snider Creek, lOOm from Dewdney Creek confluence
HEAVY MINERAL SAMPLES
Snider Creek a t road cross ing - v i s i b l e Au
25m upstream from KR-1
Duplicate a t mouth of Snider Creek
East branch approx. 4W - 15+75S
West branch approx. 150m upstream from branch confluence
West branch approx. 200m upstream from KR-5
Halfway up dry wash t o e a s t of w a t e r f a l l
Lower pool below w a t e r f a l l , Snider Creek
Upper pool below w a t e r f a l l , Snider Creek
APPENDIX F
Statement of Qualifications
STATEMENT OF QUALIFICATIONS
I, John E. Robinson of Calgary, Alberta, hereby certify that:
1) I am a graduate of Syracuse University (1981) with a B.Sc. degree in Geology.
2 ) I have been actively and continuously engaged in the practice of mineral exploration for at least 2 years.
3) I am presently employed by Ishtar Exploration Ltd. of 72 Wellington St. W., Markham, Ontario as a consultant geologist.
4 ) I performed the work described in this report for Aberford Resources Ltd. of 300 - 5 Avenue S.W., Calgary, Alberta.
5) I performed the work describe herein under the supervision of Barry W. Smee, Exploration Supervisor, Aberford Resources Ltd.
L A eeJ&-- Johyij E. Robinson, consultant Geologist
STATEMENT OF OUALIFICATIONS
I, Barry W. Smee of Calgary, Alberta, supervised the author of this report. This report is based on the results of an exploration program conducted on the ~ e w 1 and 3 claims and do hereby certify that:
1) I am a graduate of the University of Alberta, and the University of New Brunswick with a B.Sc. and Ph.D. in Geology, respectively.
2) I have practised continuously as a geologist since May, 1969.
3) I am employed by Aberford Resources Ltd. of 300 - 5 Avenue S.W., Calgary, Alberta
4) I am a member of the Association of Exploration Geochemists.
5) I am registered as a Professional Geologist in the Province of Alberta.
