NI 43-101 Technical Report
SUMMARY REPORT
ON THE
CARRUTHERS PASS PROPERTY
OMINECA MINING DIVISION BRITISH COLUMBIA.
WITH RECOMMENDATIONS FOR CONTINUING EXPLORATION
NTS: 094D039
Latitude 56 degrees 23' N, Longitude 126 degrees 18' W
(centre)
for
Hawthorne Resources Inc.
and
Wildrose Resources Ltd.
by
J.W. (Bill) Morton, P.Geo., Coauthor
Mincord Exploration Consultants Ltd.
Geoffrey Goodall P.Geo., Coauthor
Global Geological Services Inc.
June 30, 2006
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
TABLE OF CONTENTS
SUMMARY......................................................................................................................... i
1
INTRODUCTION AND TERMS OF REFERENCE.................................................... 1
2
RELIANCE ON OTHER EXPERTS........................................................................... 1
3
PROPERTY DESCRIPTION AND LOCATION: ........................................................ 2
4
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND
PHYSIOGRAPHY ............................................................................................................. 5
5
HISTORY .................................................................................................................. 6
6
GEOLOGICAL SETTING ........................................................................................ 10
6.1
Regional Geology............................................................................................ 10
6.2
Property Geology ............................................................................................ 12
7
DEPOSIT TYPES.................................................................................................... 14
8
MINERALIZATION .................................................................................................. 14
9
EXPLORATION....................................................................................................... 15
10
DRILLING............................................................................................................ 15
11
SAMPLING METHOD AND APPROACH............................................................ 23
12
SAMPLE PREPARATION, ANALYSIS AND SECURITY.................................... 23
13
ADJACENT PROPERTIES ................................................................................. 25
14
MINERAL PROCESSING AND METALLURGICAL TESTING ........................... 25
15
MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES ...................... 25
16
OTHER RELEVANT DATA AND INFORMATION............................................... 25
17
INTERPRETATIONS AND CONCLUSIONS....................................................... 26
18
RECOMMENDATIONS AND BUDGET............................................................... 27
18.1 Cost Estimate .................................................................................................. 28
19
REFERENCES.................................................................................................... 29
20
STATEMENT OF QUALIFICATIONS.................................................................. 31
21
SIGNATURE PAGE ............................................................................................ 35
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
Summary Report on the Carruthers Pass Property, June 30, 2006
LIST OF FIGURES
Figure 1 – Location Map ..................................................................................................3
Figure 2 – Claim Map.......................................................................................................4
Figure 3 – Regional Geology Map .................................................................................11
Figure 4 – Property Geology..........................................................................................13
Figure 5 – Soil Geochemistry - Copper..........................................................................16
Figure 6 – Soil Geochemistry - Zinc...............................................................................17
Figure 7 – Rock and Talus Geochemistry......................................................................18
Figure 8 – Ground Geophysical Grids............................................................................19
Figure 9 – Drill Hole Location Plan.................................................................................20
Figure 10 – Airborne Geophysics, EM Conductors ........................................................21
Figure 11 – Airborne Geophysics, Total Field Magnetics...............................................22
LIST OF TABLES
Table 3.1 – Claim List ......................................................................................................2
Table 8.1 – Select Mineralized Boulder Samples...........................................................14
Table 10.1 – Significant Drill-hole Intersections .............................................................23
Table 18.1 – Recommended Exploration Budget...........................................................28
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
2
Summary Report on the Carruthers Pass Property, June 30, 2006
SUMMARY
The Carruthers Pass property is located in the Omineca Mining Division of British
Columbia approximately 200 kilometres north of the town Smithers and 70 kilometres
south of the Kemess gold-copper mine. The property covers a small, isolated group of
peaks and the lower elevation terrain connecting them north of Carruthers Pass,
bounded by the Osilinka Ranges to the northeast and the Sikanni Range to the
southwest. Access to the Carruthers Pass property is by helicopter as there currently is
no road.
The Carruthers Pass property is situated on the eastern edge of the Stikinia Terrane of
the Intermontane Belt of the Canadian Cordillera. The property is underlain by Upper
Triassic Takla Group volcanic and sedimentary rocks of the Dewar Formation, with
minor amounts of the Savage Mountain Formation and the Permian Asitka Group
present. The property has the potential to host a Besshi-type volcanogenic massive
sulfide deposit (shale hosted type). Mineralization on the Carruthers Pass property
consists of both massive and laminated iron, copper and zinc sulphides hosted in
sediments. Pyrite and pyrrhotite commonly occur as disseminations, fracture fillings and
along bedding planes in sedimentary rocks and occasionally in volcanic rocks.
The property consists of 8 contiguous, modified-grid mineral claims for a total of 130
units, or nominally 3,250 hectares. All of claims comprising the Carruthers Pass
property are registered in the name of Phelps Dodge Corporation of Canada, Limited
(“Phelps Dodge”). The property is subject to a June, 2003 option agreement (amended
June 19/06) with Wildrose Resources Ltd. who has the right to earn a 100% interest in
the Carruthers Pass Property by completing specified cash payments and work
commitments (subject to certain “back-in right” provisions). Wildrose Resources Ltd. has
subsequently granted an option on the property to Hawthorne Resources Inc.. In an
agreement dated May 31, 2006 Hawthorne can earn a 60% interest in the Carruthers
Pass property by making cash or share payments totaling $140,000, and incurring
exploration expenditures totaling $1,000,000 within specified times over a five-year
period.
The most recent exploration on Carruthers Pass was completed in 2005. Wildrose and
Maxtech Ventures Inc., a previous optionee of the property, completed 408.5 metres of
diamond drilling in three holes. Drilling intersected significant footages of argillite with
bedded pyrite and local intercepts of ±0.15% zinc. Maxtech terminated its option with
Wildrose in January 2006.
The authors conclude that the work programs completed between 2003 and 2005,
particularly the airborne geophysical survey completed in 2004, have increased the
potential for the discovery of copper and zinc mineralization which would also be
expected to contain precious metal credits. The authors therefore conclude that the
property warrants continued exploration. A budget of $135,000 is recommended to
assess previously untested anomalies and conduct geological mapping and sampling.
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
i
Summary Report on the Carruthers Pass Property, June 30, 2006
1
INTRODUCTION AND TERMS OF REFERENCE
The authors have been retained by Hawthorne Resources Inc. (“Hawthorne”) and
Wildrose Resources Ltd. (“Wildrose”) to prepare a National Intrument 43-101 compliant
report which can be publicly filed electronically on SEDAR and satisfy required “Qualified
Person” reporting. Sources for information in this report draw on company reports held
by Wildrose, Phelps Dodge Corporation of Canada, Limited (“Phelps Dodge”) and
reports on file with the Geological Survey of Canada (“GSC”). An earlier 43-101 report
on the Carruthers Pass property, filed on December 24, 2003, by Maxtech Ventures Inc.
and authored by Jay Page P.Geo., has also provided a key source of information. The
authors of the current report are both registered Professional Geoscientists and are
familiar with the Carruthers Pass property, J.W. Morton, P. Geo. having coordinated the
2003 to 2005 exploration on the Carruthers Pass property without a visit to the property
and Geoffrey Goodall, P. Geo. who managed the year 2000 diamond drill program on
the property and has spent considerable time in the field on it.
2
RELIANCE ON OTHER EXPERTS
The opinions expressed in this report are based on the available information and
geologic interpretations as provided by Wildrose, BC MEMPR assessment files, BC
Geological Survey (“BCGS”) reports and Geological Survey of Canada (“GSC”) reports
and bulletins. The authors have exercised due care in reviewing the supplied
information and believe that the basic assumptions are factual and correct and the
interpretations are reasonable.
Claim title is granted through the BC Mineral Titles Online service and supporting
government legislation. The authors have relied on the accuracy of these records to
determine claim ownership.
All sources of information for this report are referenced in Section 19 (References). No
independent verification of other geological, geochemical or geophysical data was
undertaken.
J.W. Morton P.Geo, a coauthor of this report, is a “Qualified Person” as defined by NI
43-101 but is not an “Independent Qualified Person” for the reason of being an officer
and director of Wildrose Resources Ltd., owner of the property. In addition, he has not
visited the property. Geoffrey Goodall P.Geo. , the secondary coauthor is an
“Independent Qualified Person” by definition of the Standards for Disclosure for Mineral
Projects (NI 43-101) and has visited the property.
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
1
Summary Report on the Carruthers Pass Property, June 30, 2006
3
PROPERTY DESCRIPTION AND LOCATION:
The Carruthers Pass property is located in the Omineca Mining Division of north-central
British Columbia, approximately 200 kilometres north of Smithers and 70 kilometres
south of the Kemess gold-copper mine (Figure 1). The property consists of 8
contiguous, modified-grid mineral claims totaling 130 units, or 3,250 hectares located on
National Topographic System map-sheet 094D08W between the latitudes of 56 degrees
20 minutes and 56 degrees 25 minutes North, and longitudes of 126 degrees 15 minutes
and 126 degrees 22 minutes West (Figure 2).
Claim Name
CAR 1
CAR 2
CAR 3
CAR 4
RUT 1
RUT 2
RUT 3
RUT 4
Tenure No.
357875
364302
365532
371849
357876
365536
371847
371848
Units
16
20
12
8
16
18
20
20
Expiry
Dec. 1, 2007
Dec. 1, 2007
Dec. 1, 2007
Dec. 1, 2007
Dec. 1, 2007
Dec. 1, 2007
Dec. 1, 2007
Dec. 1, 2007
The claims are located in the Omineca Mining Division, British Columbia and are
registered in the name of Phelps Dodge Corporation of Canada, Ltd. There are no
environmental problems or aboriginal issues known to the authors specific to the
Carruthers Pass claims other than those that are general to British Columbia and
Canada. Exploration permits required by the BC Ministry of Energy, Mines and
Petroleum Resources (“MEMPR”) for activities conducted in 2005 were granted under
Notice of Work approval number 1300682, issued on April 18, 2005. As no previous
issues have been identified during prior exploration programs, the authors do not
anticipate difficulties in obtaining exploraion permits in the future.
Assessment work requirements in British Columbia require that, in the first three years of
a claim’s existence, exploration work in the amount of $4.00 per hectare per year be
completed. The amount of exploration work required to keep the claims in good stead
increases to $8.00 per hectare per year after the third anniversary. An equal amount of
cash may be paid in substitution to exploration expenditures (cash in lieu). A filing fee of
$0.40 per hectare per year is also required. The Carruthers Pass claims are now past
their 3rd anniversary and the annual amount of exploration required to keep the titles
valid is $26,000. Excess expenditures incurred in any year can be filed up to an amount
that moves the expiry date ten years into the future.
The agreement between Wildrose and Hawthorne dated May 31, 2006 provides
Hawthorne the right to earn a 60% interest in the property by completing exploration
expenditures totaling $1,000,000 before the fifth anniversary and making cash payments
totaling $140,000 before the same anniversary. Wildrose holds the Carruthers Pass
property through an agreement with Phelps Dodge dated June, 2003 that gives Wildrose
the right to earn a 100% interest subject to a back in privilege in favour of Phelps Dodge.
The back in privilege allows Phelps Dodge the right to earn a 60% interest by incurring
exploration expenditures that are the greater of 200% of Wildrose’s expenditures or
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
2
126º 18’ W
Cirque
Akie
Kemess
N
Carruthers
Pass
230kV
POWER LINE
BRITISH
COLUMBIA
BEAR
LAKE
Carruthers
Pass
Sustut
56º 22’ N
Williston
Lake
Vancouver
C.
B.
IL
RA
29
GERMANSEN
LANDING
TAKLA
LANDING
MACKENZIE
Bullmoose
Bennet Dam
Bell
Granisle
SMITHERS
97
Mt. Milligan
16
FORT
ST. JAMES
Equity
Endako
16
0
50
PRINCE
GEORGE
100
kilometres
LEGEND
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
Omineca M.D. British Columbia, CANADA
Existing mine
Developed prospect
General Location Map
Railway
Highway
Power line
Date
Scale
June 2006
NTS
93
as shown
By
Barrett/Morton
Fig
1
Asit
ka
R
iv
er
N
Car 4
371849
TRUE NORTH
(UTM north at 002º)
2N x 4W
Car 3
365532
3N x 4W
4S x 5E
4S x 4W
Car 2
Car 1
364302
357875
4S x 5W
4S x 4E
Rut 2
365536
Rut 1
Rut 4
357876
371848
6,250,000N
4S x 5E
Qu
6N x 3E
ena
da
Rut 3
371847
C
re
ek
0
500
1000
2000
s
Pa
ss
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
Omineca M.D. British Columbia, CANADA
Ca
rr
ut
he
r
metres
Claim Map
665000E
Date
Scale
June 2006
UTM
NAD 83, Zone 9
1:25,000
By
Barrett/Morton
Fig
2
Summary Report on the Carruthers Pass Property, June 30, 2006
$1,500,000 (with the Back-in election to be made within 90 days from the earliest of the
sixth anniversary or the completion of 2,500 metres of drilling). Phelps Dodge may earn
an additional 10% interest by completing a feasibility study within 3 years of earning its
back-in interest. Should Phelps Dodge elect not to exercise its back-in privilege it will be
entitled to a 21/2 % net smelter royalty that may be reduced to 1% by payment of
$1,500,000.
4
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND
PHYSIOGRAPHY
The Carruthers Pass property is located approximately 200 kilometres north of Smithers
and 70 kilometres south of the Kemess gold-copper mine. The property covers a small,
isolated group of peaks and the lower elevation terrain connecting them north of
Carruthers Pass, bounded by the Osilinka Ranges to the northeast and the Sikanni
Range to the southwest.
Drainage is provided by Quenada Creek that envelops the property on its eastern,
southern and western sides. Quenada Creek, along with the northern drainages from
the property, flow into the Asitka River, which in turn is a tributary, via the Sustut River,
of the Skeena River.
The meta-volcanic and meta-sedimentary rocks of the Carruthers Pass property create a
topography of precipitous scarp faces and extensive talus slopes. Elevations range from
a high of 2084 metres (6835 feet) on the summit of an unnamed peak on the RUT 1
claim to a low of 1370 (4494 feet) metres in the Whistler Basin to the northeast. Treeline is at approximately 1500 to 1600 meters elevation. Extensive deposits of glacial till
and fluvial glacial-outwash mantle the valley sides and bottom, disrupting the drainage
patterns. Access to the Carruthers Pass property is by helicopter, there currently is no
road access. The closest road is the Omineca mining road 29 kilometres to the northnortheast. Permanent helicopter bases exist at Smithers, approximately 200 kilometres
to the south; at Fort St. James, approximately 230 kilometres to the south-southeast; at
Mackenzie, 220 kilometres to the southeast; and at Prince George, approximately 336
kilometres to the south-southeast. The closest maintained airstrip is at the Kemess Mine
70 kilometres to the north. Seasonal helicopters have at various times in the past been
based at Johanson Lake on the Omineca mining road and at the Kemess airstrip.
Supplies and fuel are commonly sourced in Fort St. James and trucked north to
Johanson Lake via Germansen Landing.
The Carruthers Pass property enjoys a temperate continental climate with warm
summers and cold winters. Snowfall accumulation in this part of the province is often in
the range of one to two metres depth, with more to be expected in alpine areas. Surface
exploration work on the Carruthers Pass property is best carried out between early July
and late September.
The rugged nature of this landscape with its numerous broad, subsidiary valleys
separating higher mountainous regions offers many options for the construction of
surface facilities and tailings impoundment sites, and there are numerous sources of
water readily available. The property is located within 29 kilometers of the industrial
power grid that connects the Kemess Mine to the North American power grid.
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
5
Summary Report on the Carruthers Pass Property, June 30, 2006
5
HISTORY
There is no exploration work recorded in the general area around the Carruthers Pass
property prior to it being staked by Phelps Dodge in 1997. A British Columbia regional
geochemical survey released in July of that year identified six creeks draining the
property area that returned anomalous copper (147 to 215 ppm) and cobalt (31 to 38
ppm) from stream sediments (BCGS, 1997). Phelps Dodge, attracted to the area by the
regional geochemical survey results, staked the CAR 1 and RUT 1 claims in July 1997.
A brief exploration program carried out during September 1997 consisted of preliminary
prospecting, rock sampling and contour soil sampling over the claim area. A total of 37
rock samples and 8 stream sediment samples were collected during prospecting. Soil
sampling, in the absence of a grid, consisted of 7-kilometres of contour soil samples on
the CAR 1 claim (100 metres intervals), and 5.6 kilometres of soil sampling on two
contour lines on the RUT 1 claim. This yielded an aggregate total of 127 soil samples.
The analysis of rock samples yielded a wide range of values with most samples
returning background values, typically in the range of several hundred ppm copper, with
much less zinc and lead. Two samples of massive sulfide, discovered during
prospecting, stand out with their high values. In the northwest corner of the CAR 1 claim
a bedrock grab sample returned values of 8,307 ppm copper, 2,215 ppb silver, 109 ppm
zinc, 687 ppm cobalt and 455 ppm arsenic from a 20 metre by 20 metre exposure of
shale-hosted massive sulfide (Fox, 1998). On the RUT 1 claim a large piece of massive
pyrrhotite-chalcopyrite associated with calcite veins in andesite talus returned 1.12%
copper, 2.1 gpt gold, 56.3 gpt silver, 7.06% zinc and 172 ppm lead (Fox, 1998).
Silt samples from all six creeks draining the property returned anomalous copper, zinc,
silver, cobalt and arsenic, with values ranging up to 445 ppm copper, 862 ppm zinc,
1,104 ppb silver, 56 ppm cobalt and 189 ppm arsenic (Fox, 1998).
Anomalous concentrations of copper, zinc, silver, cobalt, arsenic, antimony, bismuth and
selenium were also identified in soils from the CAR 1 and RUT 1 claim areas (Fox,
1998). The soil sample contour lines identified a large, broad area with elevated to
anomalous concentrations of copper, zinc, silver cobalt and arsenic extending from the
southern part of CAR 1 to the northern half of the RUT 1 claim. High values for most
other elements were scattered sporadically across the claims. Average soil geochemical
values included 243 ppm copper, 358 ppm zinc, 19 ppm lead, 735 ppb silver, 41 ppm
arsenic, 18 ppm molybdenum, 41ppm cobalt, and 307 ppm barium; maximum values
included 1,691 ppm copper, 5,456 ppm zinc, 172 ppm lead, 1,947 ppb silver, 472 ppm
arsenic, 144 ppm molybdenum, 689 ppm cobalt and 4,576 ppm barium (Fox, 1998).
Background concentrations of gold were generally low, with an isolated maximum of 33
ppb (Fox, 1988). In 1998, Phelps Dodge carried out a much larger exploration program
that included extensive soil sampling, mapping and prospecting. An initial phase of
prospecting and contour soil sampling was done in July, with a follow-up phase of grid
soil sampling, prospecting and geological mapping completed in September 1998. The
program began with the CAR 2, CAR 3 and RUT 2 claims being staked in July to cover
possible trends of mineralization. Two grids were established in 1998, the largest one
consisting of 12 lines oriented at 040 degrees for a total of 24.3 line-kilometres on the
CAR 2 claim, and 7.5 line-kilometres in 4 lines on the RUT 2 claim. In addition, 10
contour soil sample lines were established throughout the remaining claim area. A total
of 782 soil samples were collected. Geological mapping at 1:7,500 scale and
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
6
Summary Report on the Carruthers Pass Property, June 30, 2006
prospecting of the claim area was also carried out during this period and a total of 92
rock samples were collected.
The analytical results of the soil sampling re-enforced and extended the copper and zinc
soil anomalies identified in 1997, forming a broad, northwesterly-trending zone
approximately 5 kilometres long. Average values for copper (215 ppm) and zinc (318
ppm) are slightly lower than the previous year’s survey, reflecting the broader area
sampled; most other elements had similar background values, albeit with sporadic highs,
to the previous survey. Phelps Dodge evaluation of the 1997-98 soil sample data
defined anomalous values as being greater than: 500 ppm copper, 1,000 ppm zinc,
2,000 ppb silver, 150 ppm arsenic and 25 ppb gold. Prospecting and geological mapping
in the vicinity of the 1997 copper soil anomaly successfully identified a stratabound,
copper-mineralized, shale horizon that was eventually traced along strike for
approximately 700 metres. The mineralization consists of up to 15% disseminated pyrite
with stringer and/or bedded chalcopyrite that grades up to 30% (Fox, 1998). This shale
unit strikes northeasterly, has a moderate dip to the south and is mostly exposed across
a cliff face. Fox described the results of sampling this poorly accessible unit: “Four rock
samples were collected from the mineralized shale horizon. Three of these samples
returned 53,196 ppm (5.3%), 6,033 ppm and 3,276 ppm copper with up to 1,555 ppm
zinc and 70,284 ppb (70 gpt) silver. One sample of a calcite vein within the zone
returned 5,740 ppm copper and 2,871 ppm zinc. Samples of the hanging wall and
footwall rocks generally returned 200 to 300 ppb copper, however, cherty siltstone in the
footwall returned up to 6,741 ppm copper and a lens of altered hanging wall basalt within
the mineralized zone returned up to 1,847 ppm copper. Two rock samples collected from
another small showing of massive sulfide mineralization hosted within the same
lithological package some 100 metres to the north, returned over 20,000 ppm (>2.0%)
copper with up to 56,122 ppm (5.6%) zinc. These samples also contain elevated gold
(up to 169 ppb), silver (up to 100 gpt), arsenic, antimony, bismuth, mercury, selenium
and tellurium.” (Fox, 1998). Although, the mineralized shale horizon clearly attracted the
most attention, a sample of dark green tuff containing 10 to 15% sulfide (chalcopyritepyrite) from the south boundary of CAR 1 returned 1,178 ppm copper (Fox, 1998). The
1998 program concluded that further work was warranted and should include detailed
prospecting and sampling of the copper-zinc soil anomalies and the chip-sampling of the
mineralized shale horizon to investigate the continuity of mineralization. Phelps Dodge
returned to the Carruthers Pass property in 1999 with a program that included the
staking of the CAR 4, RUT 3 and RUT 4 claims; additional soil sampling (30 samples);
rock sampling (51 samples); and some limited geophysical surveys (magnetometer and
Genie EM). Most of the geophysical surveying was done in the vicinity of the massive
sulfide boulder and on the steep slopes above (in the southern part of the CAR 2 and the
northern part of the RUT 1 claims). Approximately 2.25 line-kilometres (11 lines) of
Genie EM and magnetometer survey was carried out by Peter Walcott & Associates
Limited, with an additional 1.3 line-kilometres (5 lines) of magnetometer survey by the
Phelps Dodge crew. Survey lines in this area appear to all be oriented at 135degrees –
215 degrees. There was also a magnetometer survey carried on the south slope of the
property by Phelps Dodge in the central and southern part of the RUT 1 claim. Five lines
in this area were run east west for a total length of 5.6 line-kilometres. In scanning the
geochemical data it is apparent that a wide range of copper and zinc values were
returned from the rock and soil samples. The best copper and zinc values in rocks came
from samples described variously as pyritic black shale, pyritic hornfelsed shale,
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
7
Summary Report on the Carruthers Pass Property, June 30, 2006
tuffaceous siltstone and siliceous siltstone. The average values of the soil samples were
higher than previous surveys.
The year 2000 work program by Phelps Dodge commenced with a small geophysical
program followed by the diamond-drilling of six holes for a total of 989 metres. The
geophysics, consisting of Genie EM and magnetometer surveys was contracted to Peter
Walcott & Associates Limited. The objective of which was to locate the source of the
massive-sulfide boulder found in talus on the CAR 2 claim. The survey included
measurements of the vertical gradient over a 0.5 metre interval and the total intensity of
the earth's magnetic field at 12.5 metre intervals over the grids previously established by
the contractor and Phelps Dodge. Measurements of amplitude ratio were made at three
frequency pairs, 337/112, 1012/112, 3037/112 Hz using an S.E. 88 electromagnetic unit
employing a coil separation of 50 metres. Additional measurements were made with a
100-metre coil separation on the largest grid. Wallcott indicates in his report that a total
of 9.4 line-kilometres of magnetic survey and 12.0 line-kilometres of EM surveys were
carried out. At least part of this was in the bowl and steep slopes above the massivesulfide boulder and over the south grid area surveyed in 1999 (Kulla, G., personal
communication, December 17, 2003). The pseudo-sections of the geophysical survey,
which are not attached to the Walcott report, identify a magnetic anomaly at the site of
the boulder, and a Genie EM anomaly that traverses the slope that the boulder lies on.
The diamond-drill program in 2000 consisted of six holes drilled from three different
locations with a total footage of 989 metres. The core remains stored at the camp-site in
the valley bottom. All six holes cored shale-siltstone sequences that are variously
intruded by local mafic sills. None of the holes extended to the location of the massive
sulfide boulder which may in fact be outcrop and consequently the hypothesis that the
massive sulfide is outcropping remains untested. Anomalous copper and zinc values
were returned from drill-hole #3 with the best intersection being encountered between
128.00 to 129.00 metres depth where with a 1 metre intercept of 10,057 ppm (1%)
copper, 2,576 ppm (0.25%) zinc and 15,292 ppb (15.3 gpt) silver (Cameron, 2001). This
was within a 5-metre section (from 127.00 to 132.00 metres depth) that averaged 5,656
ppm (0.57%) copper, 1,859 ppm (0.19%) zinc and 7,817 ppb (7.8 gpt) silver (Cameron,
2001). Eight other 1-meter intervals in drill-hole # 3 returned copper values greater than
1,000 ppm, all within a 29-metre interval from 121.00 metres to 150.00 metres which
averaged 1,944 ppm (0.19%) copper (Cameron, 2001). No intervals in the other five
drill-holes returned assay values over 500 ppm copper. There were however, several
anomalous zinc (of greater than 1,000 ppm zinc) intersections in drill-holes # 2 and # 6.
Weakly anomalous silver values accompany many of the zinc anomalies in drill-holes #
3 and # 6. Gold values were uniformly low. Cameron (2001) states that the
mineralization intersected in drill-hole # 3 correlates with the exposed massive sulphide
layer outcropping on the cliff face below the drill pad. He also notes that the first hole, #
1 failed to intersect this horizon because it passed through a thickened mafic sill in the
nose of a prominent fold. The last hole, # 6 was believed to be too high in the
stratigraphic section to intersect the mineralized horizon.
In September 2003 Mincord Exploration Consultants Ltd., on behalf of Wildrose
Resources Ltd., completed a small prospecting and sampling program on the property.
The program was handicapped by an unexpectedly early snowfall but never the less did
confirm the results of previous work. A number of strongly anomalous “single point” rock
and or soil/talus fines samples greater than 1000 ppm copper and or zinc were obtained
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
8
Summary Report on the Carruthers Pass Property, June 30, 2006
from the 22 rock samples and 16 soil samples collected in this program that remain to be
followed up.
In 2004 Fugro Airborne Surveys Corp. completed 295 line kilometers of helicopter
airborne survey on the Carruthers Pass property, with funding provided by Maxtech
Ventures Inc. The survey employed a DIGHEM multi-coil, multi-frequency
electromagnetic system mounted in an AS350B3 turbine helicopter flying at an average
speed of 50 kiometres and hour and maintaining an average EM sensor height of 30
metres. A total of 627 conductors were identified by the survey. Of these, 452 are
interpreted by Fugro to be caused by discrete bedrock sources while 2 are interpreted to
be caused by a conductive rock unit or thick cover and 173 are interpreted to be caused
by conductive cover [overburden]. The Fugro report indicates that that the discrete
conductors “B or D” type are usually attributed to conductive sulphides or graphite. The
Fugro report indicates that the conductors are located with an accuracy of 10 metres. An
initial attempt to field check some of the conductors that displayed correlation with
known geological features was carried out in mid September 2004. An unexpected
snowfall negated the effectiveness of this work.
In 2005 408.5 metres of diamond drilling in three holes was completed with a fourth hole
being abandoned due to platform instability. The 2005 drilling encountered significant
footages of argillite containing bedded pyrite with a few intercepts grading >0.10% zinc.
Since Wildrose acquired the Carruther’s Pass option from Phelps Dodge in 2003 the
following exploration expenditures have been incured:
2003 $90,323
2004 $101,490
2005 $185,357
Total $377,170
Given the degree of exploration success from the limited work programs conducted to
date on the Carruthers property, the numerous airborne geophysical conductors and
single point geochemical anomalies that remain untested, the authors believe that
continued exploration on the Carruthers Pass property is warranted.
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
9
Summary Report on the Carruthers Pass Property, June 30, 2006
6
6.1
GEOLOGICAL SETTING
Regional Geology
The Carruthers Pass property is situated on the eastern edge of the Stikinia Terrane of
the Intermontane Belt of the Canadian Cordillera. The Ingenika Fault lies to the
immediate east of the property, marking the terrane boundary with Quesnellia further to
the east. There, Upper Triassic Takla Group volcanics are intruded by the Early
Jurassic Hogem Batholith, a very large elongate granodioritic to monzonitic intrusion
which is located approximately 7 kilometres east of the property. To the immediate
southeast of the Carruthers Pass property there is a very structurally complex area
where Stikinia and the Cache Creek Terrane meet in a complex zone of numerous,
easterly dipping thrust sheets and northeasterly striking, high-angle reverse and normal
faults. The Pinchi Fault, one of the major structural features of the Intermontane Belt,
terminates in this area, along with the sub-parallel Vital Fault several kilometres to the
southwest. These faults are cut and displaced by approximately 115 kilometres of rightlateral movement by the more northerly-trending Takla–Ingenika-Finlay fault system.
Reconstruction efforts by Gabrielse (1991) show the Kutcho and Nahlin faults to the
north as being continuations of the Pinchi and Vital faults respectively. The Finlay and
Ingenika faults form extensive shear zones up to several kilometres wide of numerous
parallel, vertical faults, which together with the thrust faulting west of and terminated by
the Ingenika Fault, contribute to a north-northwesterly structural grain to the regional
geology in this area. The regional geology as presented by Gabrielse is shown in figure
3.
The Carruthers Pass property covers a basal marine section of the Upper Triassic
western Takla Group, which in this area is at least 600 metres thick, occupies several
southeasterly-trending basins and is truncated by the faults that separate Stikinia from
Cache Creek and Quesnellia (Souther, 1991). In the McConnell Creek map-area the
western Takla Group consists of three formations: the basal Dewar Formation, the
Savage Mountain Formation and the overlying Moosevale Formation; which together
form a rock package which can be traced for approximately 100 kilometres west of the
Ingenika Fault. The basal Dewar Formation is formed of fine-clastics deposited in a
back-arc or continental margin environment, and is more specifically, composed of
submarine calcalkaline volcanoclastic rocks, sandstone, siltstone and graphitic shale. It
reaches a maximum thickness of approximately 1500 metres in the Sikanni ranges,
thinning to about 400 metres in the Sustut peak area. The Savage Mountain Formation
is composed mainly of augite and bladed-feldspar porphyry volcanic flows and
pyroclastics. Locally, thick successions of pillow basalts are common. The volcanic
component is both dominant and subaerial to the north where the formation reaches its
maximum thickness of approximately 4,000 metres in the Sustut Peak area. The
Savage Mountain Formation overlies the Dewar Formation in this area, but is coextensive with the Dewar Formation in the south where it is largely composed of tuff,
siltstone and shale. The overlying Moosevale Formation is composed of subaerial
volcanoclastic rocks to a maximum thickness of 1600 metres in the Savage Mountain
area, but it is not present in the Carruthers Pass property area. The north edge of the
property covers a fault-bounded section of Permian Asitka Group metasediments that
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
10
Carruthers
Pass
geological contact
geological fault
N
creek
(see following page for geological legend)
0
1
2
3
4
kilometres
5
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
Omineca M.D. British Columbia, CANADA
Regional Geology Map
Date
Scale
June 2006
UTM
NAD 83, Zone 9
as shown
By
Barrett/Morton
Fig
3
Summary Report on the Carruthers Pass Property, June 30, 2006
record a period of deformation and low-grade regional metamorphism in the Late
Permian to Early Triassic (Greenwood, etal, 1991).
6.2
Property Geology
The main part of the Carruthers Pass property claims is underlain by Upper Triassic
Takla Group volcanic and sedimentary rocks of the Dewar Formation (the basinal shale
component), with a minor amount of the Savage Mountain Formation exposed on the
western side of the CAR1, 3 and 4 claims. The following property description is taken
from Cameron (2001, p. 8) and is presented in figure 4. Dewar Formation shale,
siltstone and intermediate to mafic volcanic tuff form most of the geology evident on the
property. Shale units are black and generally pyritic with minor siltstone, andesitic tuff
and limestone interbeds. Grey to light green siltstone is well bedded, contains common
soft sediment deformation structures and is intercalated with minor shale, basalt and
andesitic tuff. Chert is light to dark grey and well layered, with minor siltstone and shale
interbeds. Volcanic rocks consist of olive green andesitic tuff with some reworked
epiclastic units, basalt and andesite flows and minor light orange, well layered felsic tuff.
A wide dioritic intrusion follows a north trending ridge across the central CAR 1 and 3
claims, ranging in width from approximately 80 to 280 metres.
Near the centre of the CAR 1 claim, the diorite is epidote altered and contains local
quartz-calcite vein stockworks, while to the south, the diorite is sheared and
serpentinitic. Bordering the intrusion on the west is a 100-metre wide band of brick-red,
intensely hornfelsed shale. The westernmost CAR 1 and 3 claims are underlain by the
Savage Mountain Formation, which consist of olive green andesitic flows, tuff and
breccia with interbedded siltstone and minor black shale. Mafic sills have intruded the
basinal sediments and were commonly encountered during the diamond-drill program.
A late Triassic mafic dyke, mapped for some 5 kilometres along strike, parallels the
Ingenika Fault on the east side of the property.
The Dewar Formation rocks exposed on the Carruthers Pass property are structurally
complex, with north-northwesterly directed folding apparent, especially on the eastern
side of the property. A northeasterly trending fault follows the prominent drainage on the
CAR 2 claim. Northwest of the fault, lithologies strike in a northerly direction, while
southeast of the fault they strike in a roughly east-west direction, perpendicular to the
observed axis of folding. The westernmost rocks exposed in a prominent cirque and
ridge on RUT 2 have been intensely faulted and folded; their proximity to the Ingenika
Fault shear zone may explain their greater structural complexity. The metamorphic
grade of the Dewar Formation rocks is low, not more than green-schist, and they have
not developed a slatey cleavage. Sedimentary rocks on the property are in general,
slightly hornfelsed and locally limonitic.
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
12
663000 E
2106
SMva
SMsi
ap
hs
60
SMva
hs
80
SMps
SMsi
664000 E
Dc
Dc
Dsi
56
61
Dc
Scale
Date
1:25,000
June 2006
By
UTM
Barrett/Morton
NAD 83, Zone 9
Fig
4
Property Geology Map
Omineca M.D. British Columbia, CANADA
72
Dps
Dc
2012
Dsi
Dps
LCP Car 3
Dva
Dva
56
Dps Dps
Dps
LCP Car 2
Dva
Dva
Dps
Dva
Dps62
LCP Car 1
45
56
2031
Dsi
44
61
62
Dps
51
70
LCP Rut 3
54
54
Dvb
1949
62
Dc
32
Dps
Dvb
42
42
Dps
20
25
Dvb
18 84
38
40
62
65
50
84
80
60
Dva
2084
54
42
Dsi
Dps
LCP Rut 2
60
46
40
34
Dsi
Dva
Dps
Dva
Dsi
Dps
74
56
74
60
Dps
Dva
Dvf Dvb
56
45
Massive Sulphide Dsi
Boulder
Dva
05
32
Dvb
Dc
10
28
40
10
Dsi
40
55
Dps
Dsi
45
38
Dsi
Dps
80
52
45
Dvb
Dps
Dva
38
1963
85
66
LCP Rut 1
60
Dps
46
Dvb
Adapted from Fox, P.E. (1999): Geological and Geochemical Report on the
Carruthers Pass Property, Phelps Dodge Corporation of Canada, Limited
Dsi
ap
Dsi
Dva
Dsi
81
ap
1907
hs
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
6250000 N
6251000 N
6252000 N
6253000 N
SMva
665000 E
665000 E
666000 E
666000 E
667000 E
667000 E
668000 E
668000 E
38
Hornfelsed shale: brick red, massive.
Felsic tuff: light orange weathering
and grey to dark grey fresh surfaces,
well defined layering
and common
6252000 N
spherulites.
Basalt/Andesite: olive green, massive.
Andesitic tuff: olive green, massive
with irregular black (chl/mang
coated?) fracture surfaces; minor
epiclastic units.
Chert: light grey to dark grey beds
and laminae, with minor interbedded
siltstone and shale.
Siltstone: grey to light green beds and
laminae, soft sediment deformation
6253000minor
N
structures common;
shale,
basalt, and andesitic tuff.
laminae; minor shale.
Diorite: medium to fine grained.
38
Copper mineralization
Limit of geological mapping
Lakes
Streams
Elevation contour (20m interval)
Index elevation
contour
6250000
N
Fold axial trace (syncline,anticline)
Bedding (strike and dip)
Fault
Geological contact (defined, inferred)
Symbols
ap
6251000 N
Late Triassic intrusives
green, irregular black (chl/mang
coated?) fracture surfaces; minor
breccia units.
SMva Andesitic tuff and conglomerate: olive
SMsi Siltstone: grey to light green beds and
siltstone and andesitic tuff layers.
SAVAGE MOUNTAIN FORMATION
SMps Pyritic black shale: minor intercalated
hs
Dvf
Dvb
Dva
Dc
Dsi
siltstone and andesitic tuff layers; rare
limestone lenses.
DEWAR FORMATION
Dps Pyritic black Shale: minor intercalated
Upper Triassic Stuhini Group
669000 E
6249000 N
669000 E
Summary Report on the Carruthers Pass Property, June 30, 2006
7
DEPOSIT TYPES
A volcanogenic massive sulphide deposit (VMS) in the Dewar Formation is the type of
deposit being explored for on the Carruthers Pass property. The Besshi-type of copperzinc rich VMS deposit is most appropriate given the thick accumulation of clastic
sediments in the Dewar Formation, which is thought to be a marginal or back-arc basin,
and has been intruded by mafic sills of calcalkaline affinity. The massive sulphide
boulder is composed of pyrrhotite, chalcopyrite and sphalerite, and has relatively low
lead values but high gold and silver values, The reader is referred to the discussion
under mineralization for more details about the boulder. The massive sulphide
mineralization discovered on the property to date, both in outcrop and in drill core has
the appropriate mineralogy, along with evidence in the mineral textures of soft sediment
deformation and slump features. Fine laminations of pyrite/pyrrhotite, and sphalerite
have been found in black shales on the property. All of these features are evidence
supporting this geological environment being favourable to host a Besshi-type VMS
deposit. The morphology of this type of deposit is one of thin, tabular lenses and the
general lack of associated alteration and their occurrence at variable or “stacked”
horizons can make them a difficult target to explore for. The identification of favourable
horizons is critical and must make full use of soil and rock geochemistry, prospecting
and geophysics. Once identified, favourable horizons can be evaluated by their
geochemical signature (both economic and trace element values), sulphide textural
features, and the presence of nearby geological features such as quartz-carbonate
stockworks and faults. However, the discovery and evaluation of this type of deposit
most likely will require a large amount of diamond drilling.
8
MINERALIZATION
Mineralization on the Carruthers Pass property consists of massive and laminated
sediment hosted iron, copper and zinc sulfides. Economic minerals identified to date are
chalcopyrite and sphalerite. These are commonly associated with the iron sulfides pyrite
and pyrrhotite. These sulfides commonly occur as disseminations, fracture fillings and as
laminations along bedding plane in sedimentary rocks and occasionally in volcanic
rocks. Concentrations up to 10% sulfide have been observed (Cameron, 2001).
Massive sulfide observed on the property, both in the boulder on the RUT 1 claim and in
drill-core from drill-hole 295-3 display soft sediment deformation along with chaotic,
disrupted sulfide textures including angular fragments of thinly laminated pyrite and
pyrrhotite-rich bedding. These textures are characteristic of slumping and suggest an
environment of rapid sedimentation and possibly rapid burial and preservation. Fine,
wispy and disseminated particles of carbonate are found in the sulfide-rich fragments
and as beds to 2 cm in the massive sulfide boulder. The massive sulphide boulder (a
several tonne rock protruding from talus) typifies the target.
A selection of samples taken from this boulder as reported by Fox, 1998 is as follows:
Sample #
Copper (%)
Zinc (%)
62692
72638
63454
Govt-A
1.12
2.62
3.13
4.44
7.05
2.99
4.50
4.48
Silver
(g/t)
56
>99
>99
250
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
Gold
(ppb)
2,100
169
458
3,170
14
Summary Report on the Carruthers Pass Property, June 30, 2006
One unusually high cobalt sample was also taken in the northwest corner of the property
on the CAR 1 claim where a bedrock grab sample is reported to have returned values of
8,307 ppm copper, 687 ppm cobalt, 2,215 ppb silver, 109 ppm zinc, and 455 ppm
arsenic from a 20 metre by 20 metre exposure of shale-hosted massive sulfide (Fox,
1998).
Elsewhere, on the east flank of the property, on the RUT 2 claim, a rock sample of
stratiform 1-2 mm thick laminations of pyrite with minor sphalerite was collected from
black shale outcrop in 2003 and its analysis (sample # P-03-CR-07) indicated a zinc
content of 2,758 ppm, along with 95.9 ppm selenium (Page, 2003). The outcrop was
measured and determined to be striking 005o and dipping 85oE. This sample should be
further explored along its projected strike.
Reconnaissance style soil geochemical results for copper and zinc are presented in
Figures 5 and 6, respectively. Rock and talus geochemistry results for copper and zinc
are provided in Figure 7.
9
EXPLORATION
No exploration work has been conducted by, or on behalf of Hawthorne on the
Carruthers Pass property although Wildrose, optionor of the property to Hawthorne,
completed, with the assistance of Maxtech Ventures Inc., a field prospecting and
evaluation program costing approximately $32,000 in 2003, an airborne geophysical
survey costing $76,200 in 2004 and a diamond drilling program costing $175,198 in
2005. The significant components of the work completed since 2003 include 295 line
kilometers of helicopter assisted geophysical survey and 408.5 metres of diamond
drilling in three holes completed and one abandoned.
Results of the ground geophysical surveys are provided in Figure 8. Airborne
geophysical electromagnetic (“EM”) conductors are presented in Figure 10 and the
airborne magnetic geophysical signature is shown in Figure 11.
10 DRILLING
Diamond-drilling was carried out in 2000 by Phelps Dodge who drilled six thin-wall NQholes from three set-ups for a total of 989.3 metres and in 2005 by Wildrose and
Maxtech Ventures Inc. who drilled three NQ holes from 3 set-ups for a total of 408.5
metres. A fourth hole attempted by Wildrose and Maxtech was abandoned shortly after
collaring after the drill platform became unstable. Drill hole locations from both drilling
campaigns are presented in Figure 9.
Both the 2000 and 2005 drill programs were contracted to Britton Brothers Diamond
Drilling of Smithers, BC. All core was logged and sampled at a facility established in the
valley floor below drill sites 295-1, 2, 3 and 05-04. The core was logged and intervals
corresponding to observed mineralization were sampled, generally on one-metre
intervals. Core was split and one half was placed in a bag and labeled with a unique
sample number, the remainder was returned to the core box for future reference. The
core remains stored on site.
J.W. (Bill) Morton P.Geo and Geoffrey Goodall P.Geo
15
664000 E
Scale
Date
1:25,000
June 2006
By
UTM
Barrett/Morton
NAD 83, Zone 9
Fig
5
Reconnaissance Soil Geochemistry
Anomalous Copper
Omineca M.D. British Columbia, CANADA
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
6250000 N
6251000 N
2106
665000 E
665000 E
2031
LCP Rut 3
LCP Rut 1
1963
1949
Adapted from Fox, P.E. (1999): Geological and Geochemical Report on the
Carruthers Pass Property, Phelps Dodge Corporation of Canada, Limited
2012
LCP Car 2
667000 E
667000 E
663000 E
6252000 N
1907
LCP Car 3
LCP Car 1
666000 E
666000 E
6253000 N
2084
LCP Rut 2
668000 E
668000 E
N
0
6250000 N
6251000 N
6252000 N
metres
100 200 300 400 500
area of Cu
mineralization
6253000 N
>1300 ppm Cu
>1000 ppm Cu
>700 ppm Cu
>500 ppm Cu
>300 ppm Cu
Geochemistry Legend
669000 E
6249000 N
669000 E
664000 E
Scale
Date
1:25,000
June 2006
By
UTM
Barrett/Morton
NAD 83, Zone 9
Fig
6
Reconnaissance Soil Geochemistry
Anomalous Zinc
Omineca M.D. British Columbia, CANADA
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
6250000 N
6251000 N
2106
665000 E
665000 E
2031
LCP Rut 3
LCP Rut 1
1963
1949
Adapted from Fox, P.E. (1999): Geological and Geochemical Report on the
Carruthers Pass Property, Phelps Dodge Corporation of Canada, Limited
2012
LCP Car 2
667000 E
667000 E
663000 E
6252000 N
1907
LCP Car 3
LCP Car 1
666000 E
666000 E
6253000 N
2084
LCP Rut 2
668000 E
668000 E
N
0
6250000 N
6251000 N
6252000 N
metres
100 200 300 400 500
6253000 N
>3000 ppm Zn
>2000 ppm Zn
>1400 ppm Zn
>1000 ppm Zn
>800 ppm Zn
>650 ppm Zn
Geochemistry Legend
669000 E
6249000 N
669000 E
100
200
1949
734
968
695
689
1109
723
2005
397
495
663
1247
579
1
2
3
4
5
6
7
8
9
10
11
12
1131
596
460
312
488
440
587
549
458
759
1371
653
Cu(ppm) Zn(ppm)
#
TALUS SAMPLING
RESULTS
0
metres
300
400
500
area of Cu mineralization
Talus Sample Location
copper assay (ppm)
Rock Sample Location
zinc assay (ppm)
copper assay (ppm)
Soil Sample Location
zinc assay (ppm)
Scale
1:25,000
3 June 2006
P Rut
Date
By
UTM
Barrett/Morton
NAD 83, Zone 9
Fig
7
Reconnaissance Rock,
Soil & Talus Geochemistry
Omineca M.D. British Columbia, CANADA
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
Rut 1
7
498
904
894
409
LEGEND
1963
1245
649
1154
644
465
2385
429
600
312
815
1947
1062
667000 E
667000 E
259
224
409
894
479
716
112
267
924
306
12
666
1165
665
960
423
593
1618
1039
304
648
347
857
8
19,806
49,869
2084m
101
122
7
173
324
59
142
503
54
1
244
177
336
67
978
65
295
199
249
81
668000 E
668000 E
125
93
177
137
392
3159
172
614
436
718
701
439 976
1014
104 123
528 2758
575
1874
118
155
149
105 500
201
462 193
396
1172 501
858
212
78
6250000 N
6251000 N
N
2106
664000 E
Scale
Date
1:25,000
June 2006
By
UTM
Barrett/Morton
NAD 83, Zone 9
Fig
4
8
Ground
BasedMap
Property
Geology
Geophysical Grids
Omineca M.D. British Columbia, CANADA
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
6250000 N
6251000 N
6252000 N
1907
LCP Car 1
LCP Car 3
LCP Car 2
2031
LCP Rut 3
LCP Rut 1
1963
Mag 1999; Mag + Genie E.M. 2000
1949
Mag + Genie E.M. 1999
Mag + Genie E.M. 2000
Adapted from Cameron R.S., (2001): Diamond Drilling Report on the Carruthers
Adapted
from Fox,
.E. (1999):
Geological
and Geochemical
ReportReport
on theon the
Pass Property;
and PFox,
P.E., (1999):
Geological
and Geochemical
Carruthers
Dodge
Corporation
of Canada, of
Limited
Carruthers Pass
Pass Property,
Property;Phelps
both from
Phelps
Dodge Corporation
Canada, Limited
2012
665000 E
665000 E
663000 E
6253000 N
666000 E
666000 E
667000 E
667000 E
2084
LCP Rut 2
Mag 1999; Mag + Genie E.M. 2000
668000 E
668000 E
0
N
6250000 N
6251000 N
6252000 N
6253000 N
metres
100 200 300 400 500
669000 E
6249000 N
669000 E
2106
664000 E
Scale
Date
1:25,000
June 2006
By
UTM
Barrett/Morton
NAD 83, Zone 9
Fig
4
9
Diamond Geology
Drill Locations
Property
Map
2000/2006
Omineca M.D. British Columbia, CANADA
HAWTHORNE RESOURCES INC.
WILDROSE RESOURCES LTD.
Carruthers Pass Property
6250000 N
6251000 N
6252000 N
1907
LCP Car 1
LCP Car 3
LCP Car 2
2031
LCP Rut 3
LCP Rut 1
1963
1949
Adapted from Fox, P.E. (1999): Geological and Geochemical Report on the
Carruthers Pass Property, Phelps Dodge Corporation of Canada, Limited
2012
665000 E
665000 E
663000 E
6253000 N
666000 E
666000 E
DDH 05-1
DDH 295-1,2,3
DDH 295-6
LCP Rut 2
DDH 05-2
DDH 05-3
DDH 295-4,5 2084
DDH 05-4
667000 E
667000 E
668000 E
668000 E
6250000 N
Copper anomaly
Drill hole 2005
6251000 N
6252000 N
6253000 N
metres
100 200 300 400 500
Drill hole 2000
Symbols
0
669000 E
6249000 N
669000 E
