TAGISH LAKE GOLD PROPERTY WHITEHORSE MINING

Transcription

AMC Mining Consultants (Canada) Ltd
BC0767129
Suite 1330, 200 Granville Street
Vancouver BC V6C 1S4
CANADA
T
F
E
+1 604 669 0044
+1 604 669 1120
amccanada@amcconsultants.ca
TAGISH LAKE GOLD PROPERTY
WHITEHORSE MINING DISTRICT
NI 43 101 REPORT
Longitude 135° 20’ W, Latitude 60° 10’ N
prepared for
NEW PACIFIC METALS CORP.
Report Prepared by
Brian O’Connor P.Geo.
NUMBER 711039
September 02 2011
ADELAIDE
+61 8 8201 1800
BRISBANE
+61 7 3839 0099
MELBOURNE
+61 3 8601 3300
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www.amcconsultants.com
UNITED KINGDOM
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NEW PACIFIC METALS CORP
Tagish Lake Gold Property NI 43 101 Report
1
SUMMARY
AMC Mining Consultants (Canada) Ltd (AMC) was commissioned by New Pacific Metals
Corp (New Pacific) to review a NI 43-101 report written by New Pacific. The report was
reviewed by the B.C. Securities Commission; the review identified disclosure issues and this
report is meant as an independent technical report compliant with Canadian National
Instrument 43-101 (NI 43-101) for the Tagish Lake Gold Property (Tagish or the Property).
AMC is of the understanding that this replacement report is acceptable in the pre July 1,
2011 NI 43-101 format.
The author is the “Qualified Person” pursuant to NI 43-101 and is responsible for preparing
this technical report. To prepare this report the author visited the site 25 July through 28 July
2011. Mr. O’Connor reviewed the available historical exploration data with Mr. Gerhard
Jacob (exploration geologist) and Mr. Alex Zhang (chief exploration geologist) of New
Pacific.
1.1
Introduction and Property Location
Tagish is located 84 km by road south of Whitehorse, Yukon within the Whitehorse Mining
District. It consists of 982 active quartz mining claims and three full Crown Grants totalling
178 km2.
New Pacific completed the acquisition of the 100% interest in Tagish Lake Gold Corp (TLG)
through a court-approved plan of arrangement under the Business Corporations Act of
British Columbia. TLG will operate as a wholly owned subsidiary of New Pacific.
1.2
Geology and Mineralization
Tagish is located within the Intermontane Belt of the Canadian Cordillera, and locally
situated in a Tertiary subvolcanic to volcanic caldera system (Mt. Skukum Volcanic Caldera)
which is underlain by a dome (or several dome) complexes.
There are three known precious metal deposits in the Property: Mt. Skukum gold deposit,
Skukum Creek gold-silver deposit and Goddell gold deposit. In addition, there are numerous
mineral showings and geochemical anomalies within the claim block, such as the Charleston
gold-silver showing, Becker-Cochran antimony mineralization, Porter-Antimony Creek silverantimony showing, and Raca gold-silver showing..
The Mt. Skukum gold deposit is a high level, epithermal, auriferous, quartz-calcite, vein type
gold deposit, and hosted in open fractures in Tertiary andesitic volcanic rocks. Both grade
and width of the auriferous veins change dramatically along strike and down dip with
frequent swelling and pinch out.
The Skukum Creek deposit is a mesothermal quartz sulphide vein type gold-silver deposit. In
some documents it is also taken as the lower portion of an epithermal system. The quartz
sulphide veins are hosted in Mesozoic intermediate to felsic intrusive rocks and emplaced
along the contact of rhyolite/andesite dykes with intrusive rocks. The veins and dykes formed
a unit which emplaced along shear zones and faults developed in intrusive rocks. Besides
gold and silver, the veins contain varying amount of base metals. Geological data suggest
AMC 711039 : September 2011
i
the gold-silver showings at the locations of Raca and Charleston are of a similar or same
type of mineralization.
The Goddell gold deposit is an epithermal deposit hosted in shear zones and associated with
disseminated sulphides in altered monzonitic intrusive rocks and intermediate to felsic dykes.
High grade gold is mostly associated with fine disseminated acicular arsenopyrite. Besides
arsenopyrite and pyrite, gold mineralization is closely related to other sulphides such as
stibnite in forms of veinlets and stockworks. Induced Coupled Plasma (ICP) results indicate
the mineralization zone contains anomalous values of base metals.
1.3
Historical Exploration
Historical work on the Property culminated with the discovery and resource definition of the
three known deposits during the 1980s to 1990s. There are two years of gold production at
the Mt. Skukum Gold Mine from 1986 to 1988 with total gold production of 77,790 ounces.
Historical exploration consisted of surface geological surveys, geochemical surveys, ground
and airborne geophysical surveys, trenching, and surface and underground drilling.
Approximately 121,000m was drilled in more than 910 holes, and 7,630m of underground
drifting and crosscutting were developed, mostly for the three deposits.
1.4
Metallurgy Testing
From 1988 to 2006, various types of mineral processing and metallurgical test work have
been completed on the ore of the Skukum Creek gold-silver deposit. Tests included grinding
and flotation to produce bulk sulphide concentrates, as well as cyanidation of the flotation
concentrates, cleaner flotation, specific gravity and bond work index determination. Settling
tests were also conducted on flotation tailings.
1.5
Mineral Resources
There are no current resource estimates for Tagish. There are historical resources as
described in the History section of this report.
1.6
Conclusions and Recommendations
Based on the review of the exploration reports, past operator status and existing
infrastructure, the author is of the belief that further exploration on Tagish is warranted. The
author agrees with the exploration budget for Phase 1 presented in Table 1.1 which would
collect additional information on Tagish.
ii
Table 1.1
Summary of the Phase 1 Property Exploration Budget for 2011-2012
Exploration Project Description
Budgeted
Amount $
Measurement
Unit of
Measure
Unit Cost $
Surface construction
New Camp
284,900
10,908
SQFT
26.12
Geology building
262,200
5,200
SQFT
50.42
11,500
900
SQFT
12.81
Road regrading & rebuilding
120,000
24
km
5,000
Subtotal
678,600
Dry room expansion
Equipment
Mining, Ventilation, Power generators - Goddell
614,800
Mining, Ventilation, Power generators Skukum
385,300
Office and computer equipment - Geology
Environmental equipment
Equipment for general operation
Subtotal
86,400
5,000
305,900
1,397,400
Surface exploration
Reporting & assessment
387,400
Staking & mapping
224,800
551
claim
408
37,900
1,500
ea
25
24,000
metre
Sampling
Geophysics
456,800
Surface drilling
3,508,400
Subtotal
4,615,300
146.2
Goddell Underground Exploration
Site preparation
Dewatering
Underground drilling
Equipment repair & maintenance
Subtotal
446,500
128,100
16,200,000
3,729,400
23,000
litre
0.01
metre
162.1
91,100
4,395,100
Skukum Underground Exploration
Site preparation
Dewatering
Subtotal
583,000
134,300
19,160,352
litre
0.01
2,350,400
13,000
metre
180.8
8
month
174,938
59,800
3,127,500
Studies
Environmental Study
266,700
Subtotal
266,700
General operation
General operation
Subtotal
Total
1,399,500
46,300
1,445,800
15,926,400
iii
Phase 2
Contingent on the program as tabled for Phase 1 being successful in gathering a suitable
level of information on the geology (sufficient to estimate an Indicated Resource), as well as
engineering, legal, operating, economic, social, and environmental factors involved with
Tagish. The author would agree New Pacific’s budget amount for a Feasibility study budget
as presented in Table 1.2.
Table 1.2 Summary of the Phase 2 Property Exploration
Feasibility Study
Budgeted
Amount $
Measurement
Unit of
Measure
Unit Cost $
575,900
iv
CONTENTS
1
SUMMARY ......................................................................................................................i
1.1
Introduction and Property Location...........................................................................i
1.2
Geology and Mineralization ......................................................................................i
1.3
Historical Exploration ............................................................................................... ii
1.4
Metallurgy Testing ................................................................................................... ii
1.5
Mineral Resources ................................................................................................... ii
1.6
Conclusions and Recommendations ....................................................................... ii
2
INTRODUCTION ........................................................................................................... 4
3
RELIANCE ON OTHER EXPERTS ............................................................................... 5
4
property description and location ................................................................................... 6
4.1
Location .................................................................................................................. 6
4.2
Tenure .................................................................................................................... 6
4.3
Property Description ............................................................................................... 7
4.4
Permits, Royalties, and Liabilities ........................................................................... 7
5 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND
PHYSIOGRAPHY ................................................................................................................. 9
5.1
Topography, Elevation, and Vegetation ................................................................. 9
5.2
Accessibility and Proximity to Population Centre ................................................... 9
5.3
Climate ................................................................................................................... 9
5.4
Infrastructure ........................................................................................................ 10
5.4.1 Surface Rights, Power and Water ..................................................................... 10
5.4.2 Tailings and Waste Storage .............................................................................. 10
5.4.3 Processing Plant (Mill) ...................................................................................... 10
5.4.4 Underground Development ............................................................................... 10
5.4.5 Other Structures................................................................................................ 10
5.4.6 Local Labour Resources ................................................................................... 10
6
HISTORY ..................................................................................................................... 12
6.1
History of Ownership ............................................................................................ 12
6.1.1 Mt Skukum ........................................................................................................ 12
6.1.2 Skukum Creek .................................................................................................. 12
6.1.3 Godell................................................................................................................ 12
6.2
Historical Exploration ............................................................................................ 12
6.3
Historical Exploration Results ............................................................................... 15
6.4
Historical Sample Preparation, Analyses and Security ........................................ 15
6.4.1 General Comments ........................................................................................... 15
6.4.2 Mt. Skukum ....................................................................................................... 15
6.4.3 Skukum Creek .................................................................................................. 16
6.4.4 Goddell.............................................................................................................. 17
6.5
Historical Data Verification for Skukum Creek and Goddell Deposits .................. 17
6.6
Historical Resources and Reserves ..................................................................... 18
6.6.1 Resource Estimate 2003 Skukum Creek and Goddell ...................................... 18
6.6.2 Results of Estimate ........................................................................................... 19
6.6.3 Resource Update 2007 Skukum Creek Deposit ............................................... 20
6.6.4 Results of Estimate ........................................................................................... 21
i
6.7
Historical Reserve Estimate of Lake Veins of Mt. Skukum Gold Deposit 1988 .... 21
7
GEOLOGICAL SETTING............................................................................................. 22
7.1
Regional Geology ................................................................................................. 22
7.2
Local Geology....................................................................................................... 25
7.2.1 Proterozoic to Paleozoic Metamorphic Rocks .................................................. 25
7.2.2 Probable Jurassic Volcanic and Siliclastic Rocks ............................................. 25
7.2.3 Intrusive Rocks ................................................................................................. 26
8
DEPOSIT TYPES ........................................................................................................ 31
9
Mineralization............................................................................................................... 32
9.1
Skukum Creek Deposit ......................................................................................... 32
9.2
Goddell Deposit .................................................................................................... 35
9.3
Mt. Skukum Deposit ............................................................................................. 37
10 EXPLORATION ........................................................................................................... 39
11 DRILLING .................................................................................................................... 40
11.1 Historical Drilling ................................................................................................... 40
12 Sampling Method and Approach ................................................................................. 41
13 SAMPLE PREPARATION, ANALYSES AND SECURITY ........................................... 42
14 Data Verification .......................................................................................................... 43
15 Adjacent Properties ..................................................................................................... 44
16 Mineral Processing and Metallurgical Testing ............................................................. 45
17 Mineral Resource and Mineral Reserve Estimates ...................................................... 46
18 Other Relevant Data and Information .......................................................................... 47
19 Interpretation and Conclusions .................................................................................... 48
19.1 Goddell ................................................................................................................. 48
19.2 Skukum Creek ...................................................................................................... 49
19.3 Raca ..................................................................................................................... 49
19.4 Charleston ............................................................................................................ 49
19.5 Mt. Skukum........................................................................................................... 49
19.6 Porter Structure .................................................................................................... 50
20 Recommendations ....................................................................................................... 51
20.1 Geological Surveys............................................................................................... 51
20.1.1 Mapping and Sampling .................................................................................. 51
20.1.2 Trenching ...................................................................................................... 51
20.1.3 Geochemical Surveys ................................................................................... 51
20.2 Exploration Program and Budget ......................................................................... 52
21 References .................................................................................................................. 55
22 Date and Signature Page ............................................................................................ 57
ii
TABLES
Table 1.1 Table 6.1 Table 6.2 Table 6.3 Table 6.4 Table 6.5 Table 6.6 Table 7.1 Table 16.1 Table 20.1 Summary of the Phase 1 Property Exploration Budget for 2011-2012 ........... iii Drilling and drifting conducted at the Skukum Creek Resource area
(1985 to 2008) .............................................................................................. 13 Drilling and drifting conducted at the Goddell Resource area
(1987 to 2004) .............................................................................................. 14 Drilling Conducted at Mt. Skukum (1982 to 1999) ........................................ 15 2003 Summary of Skukum Creek Resources Using a 3 g/t Cut-off Grade ... 20 2003 Summary of Goddell Resources Using a 3 g/t Cut-off Grade .............. 20 2007 Summary of Rainbow 2 and Berg Zones of Skukum Creek
Resources..................................................................................................... 21 Stratigraphy Units of the Tagish Property ..................................................... 24 Results of Historical Mineral Processing and Metallurgical Tests Prior to
2000 .............................................................................................................. 45 Summary of the Property Exploration Budget for 2011-2012 ....................... 53 FIGURES
Figure 4.1
Figure 4.2
Figure 5.1
Figure 7.1
Figure 9.1
Figure 9.2
Figure 9.3
Location and Access of the Property .............................................................. 6
Mineralized Zones and Infrastructure Relative to Property Boundaries ......... 8
Camp Layout on the Property Site ................................................................ 11
SimplifiedGeology Map of the Tagish Property ............................................ 23
Section 1400E of Skukum Creek .................................................................. 34
4375E Section of Goddell ............................................................................. 36
Simplified Geology Plan of the Mt. Skukum Deposit .................................... 38 APPENDICES
APPENDIX A MINERAL TENURE AMC 711039 : September 2011
iii
2
INTRODUCTION
AMC Mining Consultants (Canada) Ltd (AMC) was commissioned by New Pacific Metals Corp
(New Pacific) to review a NI 43-101 report written by a non-independent consultant in the
employ of New Pacific. The report was reviewed by the B.C. Securities Commission; the review
identified disclosure issues and this report is meant as an independent technical report
compliant with Canadian National Instrument 43-101 (NI 43-101) for the Tagish Lake Gold
Property (Tagish).
The author is the “Qualified Person” pursuant to NI 43-101 and is responsible for preparing this
technical report. In preparation of this technical report the author visited the site 25 July through
28 July 2011. Mr. O’Connor reviewed the available historical exploration documents with Mr.
Gerhard Jacob (exploration geologist) and Mr. Alex Zhang (chief exploration geologist) of New
Pacific. The documents are listed in the reference section.
The main sources of information are from the historical published and internal technical reports
prepared by registered professionals including Chris Naas, P.Geo., CME Consultants Inc.;
Douglas Roy, P.Eng., and Patrick Hannon, P.Eng., of MineTech International Limited; Todd
Johnson, P.Eng.; B.W.R. McDonald, M.Sc; R.J.Roger, P.Eng.; A.J. MacDonald, Ph.D, etc., as
listed in the reference list.
AMC has reviewed and relied on the descriptions of sampling approaches, procedures and
analysis methods from various published and internal technical reports of the operating
companies at different stages.
4
3
RELIANCE ON OTHER EXPERTS
In the disclosure of information relating to legal, title and related issues (see Section 4), AMC
has relied on information provided by the Mining Recorder of Whitehorse, Yukon, and from New
Pacific.
5
4
PROPERTY DESCRIPTION AND LOCATION
4.1
Location
Tagish is located 84 km by road south of Whitehorse, Yukon within the Whitehorse Mining
District (Figure 4.1). The 178 km2 property consists of 982 full or fractional mineral quartz claims
and three full Crown Grants. All claims are active and in good standing. The approximate center
coordinates of Tagish in degrees and minutes is Longitude: 135° 20’W and Latitude: 60° 10’ N.
Figure 4.1
4.2
Location and Access of the Property
Tenure
New Pacific announced in a press release on January 5, 2011, that it had completed the
acquisition of the 100% interest in Tagish Lake Gold Corp. (TLG) through a court-approved plan
of arrangement under the Business Corporations Act of British Columbia. TLG will operate as a
wholly owned subsidiary of New Pacific. TLG’s main asset is Tagish, which under previous
operators was named the “Skukum Property”.
The list of mineral claims is presented in Appendix A.
According
to
the
Mineral
Tenure
Commissioners
office
website,
http://www.emr.gov.yk.ca/mining/mineral_tenure_commissioners_land_yukon.html, the following
is required to retain the property:
6
“Continued tenure to the mineral rights is dependent upon work performed on the claim or a
group of claims. When work has been done on a claim and is being used for the renewal of that
claim, a full report of the work done must be submitted to the Mining Recorder Office. A renewal
certificate will not be issued until the report and/or survey has been approved for the value
required.
The Quartz Mining Act (QMA) does not specify work to be performed, except in dollar terms.
Renewal of a quartz claim requires that $100 of work be done per claim, per year, based on the
Schedule of Representation Work outlined in the QMA. Where work is not performed, the
claimant may make a payment in lieu of work. The fee for payment in lieu is $100 per claim per
year plus $5 for the certificate of work per claim per year.”
The QMA does entitle TLG to all “minerals” (as that term is defined in section 1 of the act) that
lie within the claim boundaries continued down vertically, but does not include limestone,
marble, clay, gypsum, or any building stone when mined for building purposes, earth, ash, marl,
gravel, sand, or any element that may, in the opinion of the Yukon government, form a portion of
the agricultural surface of the land.
4.3
Property Description
The property boundaries are located by the claim posts which were placed to mark the
perimeter claims. Figure 4.2 and Figure 5.1 display the mineralized zones, mine workings,
infrastructure and important natural features on Tagish.
4.4
Permits, Royalties, and Liabilities
TLG currently holds a Mining Land Use Permit (MLUP, Approval No. LQ00080a) for Tagish,
which is valid until October 2011. TLG submitted an amendment to the current MLUP for
underground drilling at the Goddell decline. A Schedule 3 Notification was issued by the Yukon
Government in May 2011 to allow for the dewatering at the Goddell portal in an effort to prepare
for the 2011 underground drilling and exploration program.
TGL submitted a new Class 3/4 MLUP, a Type B Water Use License Application, and a Yukon
Environmental and Socio-economic Assessment Act Application (YESAA) to the Yukon
Government on May 13, 2011 to effect a 2012-2016 advanced exploration program at the
Property. AMC is not aware of any litigation potentially, or environmental liabilities affecting
Tagish.
7
Figure 4.2
Mineralized Zones and Infrastructure Relative to Property Boundaries
8
5
ACCESSIBILITY,
PHYSIOGRAPHY
CLIMATE,
LOCAL
5.1
Topography, Elevation, and Vegetation
RESOURCES,
INFRASTRUCTURE
AND
Tagish is located in the Wheaton River valley in the Coast Range Mountains of the southern
Yukon Territory. The broad, flat, valley floor, at about 1000m elevation, is semi-arid with
approximately 370 mm of precipitation per year, with about half falling as rain in the summer.
Nearby peaks, rising to 2,300m, receive considerably greater amounts of precipitation, primarily
as snow.
The most common types of trees are white and black spruce, balsam fir, pine, tamarack, aspen,
and balsam poplar. Wildflowers, including magenta fireweed, anemones, yellow potentilla,
monkshood, arctic poppy, harebell, wild rose, lupines, lousewort, wintergreen and beardtongue
are common. Vegetation around the site consists mainly of coniferous trees, willows and
poplars. Alpine grass, lichen, and smaller shrubs are present above the treeline at about
1500m.
5.2
Accessibility and Proximity to Population Centre
Tagish is accessible via the Alaska Highway, approximately 24 km from Whitehorse city center
the turn off to the paved Klondike Highway is taken. Approximately 18 km is the connection with
the gravel Annie Lake Road then 46 km further is the entrance to the Tagish property (Figure
4.1). The mineralized target zones are connected by small gravel roads. A heliport is available
at the camp.
Whitehorse, the Yukon capital (population 26,500), is the closest significant population center.
The Whitehorse economy relies in part on the state of Yukon mining, and many of the
businesses that provide services to the mining industry are headquartered in the city. Surface
access to Whitehorse is provided by a network of highways, including the international Alaska
Highway connecting the Yukon with the Alaska, British Columbia, and Alberta highway
networks. Whitehorse is served by the Erik Nielsen Whitehorse International Airport and has
scheduled service to Vancouver, Calgary, Edmonton, Fort Simpson, Yellowknife as well as
Fairbanks, Alaska and Frankfurt, Germany during the summer months.
5.3
Climate
The climate around Whitehorse can be classified as sub-arctic and alpine. The average summer
high and low temperatures are 20°C and 7.6°C, respectively while the average winter high and
low temperatures are -14°C and -23°C. Temperatures can reach as high as 35ºC in summer
and as low as -50 º C in winter. The surrounding area is semi-arid and receives approximately
160 mm of rain and 145 cm of snow each year for a total of 270 mm of precipitation. The mean
temperature is above zero between mid-April and mid-October, or six months per year. The air
pressure is lower than standard at around 92 kPa. The prevailing winds are South-Southeast
with an average yearly speed of 14 km/h, with extreme hourly speeds up to 70 km/h and
extreme gust speeds up to 100 km/h. Permafrost is present on the North facing slopes and
higher elevations of the surrounding hills. South facing slopes thaw to shallow depth during
summer. The exploration program operates year around.
9
5.4
5.4.1
Infrastructure
Surface Rights, Power and Water
Figure 4.2 displays the sufficiency of surface rights for a mining operation. A diesel generator
with a capacity of 180 kW is the main electrical power source for the camp, installed in May
2011; two smaller generators, each 40 kW, are utilized for standby and other applications in the
operation. The previous operator used water from the Wheaton River. The present camp facility
uses two boreholes as a water source. Recirculated water from the settling ponds adjacent to
the Skukum Creek 1300 portal and the Goddell portal is used for the underground mine
rehabilitation work, the underground exploration drilling, and the surface drilling programs.
5.4.2
Tailings and Waste Storage
There is an existing tailings pond near the mill with an estimated capacity of 700,000 tonnes
(Figure 4.2). The topography is suitable to establish waste rock storage areas or to expand the
tailings storage capacity. There is potential for a portion of the tailings to be used as mine
backfill.
5.4.3
Processing Plant (Mill)
There is an existing mill, left over from the previous Mt Skukum mining operation (Figure 5.1). It
consists of crushing, grinding, cyanidation, and Merrill-Crowe precipitation. It is housed in a preengineered steel building and has a rated capacity of 270 tonnes per day. There has been some
vandalism and/or removal of electrical and other fixtures of the plant infrastructure.
5.4.4
Underground Development
Two adits access the Rainbow Zone on the 1300m and 1350m levels. Footwall drifts run parallel
the Rainbow Zone, toward and into the Kuhn Zone. The adit and footwall drifts are potentially
large enough (approximately 3x3 mm) for production purposes. Numerous crosscuts access the
main mineralized zone on both levels. A decline provides access to the 1275, 1250, and 1225m
levels, all of which are used for diamond drilling. A raise connects the 1300 and 1350m levels in
the Rainbow Zone and a vertical ventilation raise connects all levels with the surface at an
elevation of approximately 1450m. Two raises connect the 1300 and 1350m levels within the
Rainbow and Kuhn main mineralized zones. The latter provides the only access to the 1350m
sublevel within the Kuhn Zone.
5.4.5
Other Structures
There is a pre-engineered steel structure service building with 250m2 of floor space used for the
exploration program. Also a full-service 50 person camp facility and a six-room office trailer,
both of which are heated (Figure 5.1).
5.4.6
Local Labour Resources
There is skilled and unskilled mine labour available in the region.
10
Figure 5.1
Camp Layout on the Property Site
11
6
HISTORY
Information in this section is primarily derived from the report “Review of the Skukum Property”
prepared in 2001 by CME Consulting Ltd (CME), for TGL.
In 1981, Agip Canada Ltd (Agip) discovered gold in the Skukum area. The discovery
precipitated a staking rush. The subsequent exploration resulted in the discoveries of the
Skukum Creek deposit by Omni in 1985 and the Goddell Gully deposit by Berglynn Resources
Inc in 1988.
6.1
6.1.1
History of Ownership
Mt Skukum
Between February 1986 and August 1988, Mount Skukum Gold Mines Limited, a joint venture
between Total Erickson Resources Ltd and Agip, produced 77,796 ounces of gold from 223,439
tons (or tonnes - reporting is inconsistent). Most of the mill feed came from a single vein in the
oxidized Main Cirque Zone.
Wheaton River Minerals Ltd (Wheaton) purchased 820 claims in July 1991 to hold 100%
interest in the property. Omni purchased the Mt Skukum claims and the mill from Wheaton in
September 1994.
Omni re-staked 22 claims before 1996. During 1996-1997, Omni and Trumpeter Yukon Gold
(TYG) jointly staked 135 claims (50/50 interest). During 1999, CME re-staked 25 full or fractional
claims on behalf of the TYG/Omni partnership.
6.1.2
Skukum Creek
The Skukum Creek deposit, was first staked by Omni with 138 claims in 1984. Omni expanded
its land position by 44 claims by reaching an agreement in 1985 with Skukum Gold Inc. Omni
staked or acquired additional claims between 1986-1998, bringing its total holding to 356 claims.
Skukum Gold Inc and Omni formed a joint venture in 1988. The agreement was terminated in
1990. Ownership reverted back to Omni. Wheaton optioned the property in 1991. That option
was renegotiated in 1992, Wheaton's option eventually expired. Omni and TYG amalgamated in
2000 to form TLG.
6.1.3
Godell
Omni optioned it from an Arkona/276 Taurus Ventures Ltd partnership in 1995. The TYG/Omni
partnership staked an additional 69 claims north of the property, covering the camp and mill site.
They were registered under BYG Natural Resources. Before TLG was formed in 2000, all
claims that were not registered in either Omni's or TYG's name were transferred to Omni.
6.2
Historical Exploration
The historical exploration on the claims comprising the holdings of TLG is well documented in
Naas reports of 2001, 2003, 2005, and 2007. Johnson 2010, and Roy and Hannon 2003 are
also sources of exploration history.
12
Historical exploration consisted of surface geological surveys, geochemical surveys, ground and
airborne geophysical surveys, trenching, underground development, and surface and
underground drilling. Approximately 121,000m was drilled in more than 910 holes, and
7,630 mm of underground drifting and crosscutting were developed for the three deposits. The
following summary drilling tables are sourced from the above documents.
Table 6.1
Drilling and drifting conducted at the Skukum Creek Resource area (1985 to
2008)
Total amount of drilling
completed (m)
Years drilling
and/or
underground
development
completed
Amount of Drift
Completed
(m)
Companies Involved
23 (s)
2,322.61 (s)
1985
0
Aurum
55 (s)
8,301.47 (s)
1986
0
Aurum
69 UG and 11(s)
2,624.03 (s) 4,821.97
(UG)
1987
823; collar the
1,300 metre
portal
Aurum and Omni
Resources Inc.
13 UG 24 (s)
1,416 (UG) 5,165 (s)
1988
1,571; collar the
1350 m portal
Skukum Gold Inc. and
Omni Resources Inc.
15 UG
1,647 UG
1996
100
Omni Resources Inc.
7 (s)
2,739 (s)
1997
ND
Omni Resources Inc.
Total Number of
Drill holes
completed
5 (s)
1,321.9 (s)
1998
ND
Omni Resources Inc.
4 (s)15 UG
1,502.35 (s) 2,502.52 UG
2001
ND
TLGC
5 UG
248 UG
2003
586
TLGC
14 UG
913.4 UG
2005
ND
TLGC
72 UG
6,446.21 UG
2006
400
TLGC
13 UG
1,783.4 UG
2007
570
TLGC
3 UG
342.6 UG
2008
0
TLGC
TOTALS 129 (s)
219 UG
23,976.36 (s) 20,121.1
UG
1985-2008
4,050
Various
NOTES: UG = Underground; (s) = surface; TLGC = Tagish Lake Gold Corp.; ND = no data.
The Skukum Creek 1,300 metre portal was collared in January 1987. Source from T.W. Johnson and J.Fan, 2010.
13
Table 6.2
Drilling and drifting conducted at the Goddell Resource area (1987 to 2004)
Years drilling and/or
underground
development
completed
Total amount of
Total Number of Drill
drilling completed
holes completed
(m)
Amount of
Drift
Completed
(m)
Companies Involved
1987
13 (s)
2,857.19 (s)
0
Berglynn Resources
Inc. and Skukum Gold
Inc.; Skukum
Ventures
1988
4 (s)
1,976.33 (s)
0
Skukum Gold
1990
7 (s)
1,573.08 (s)
0
Skukum Gold
1995
5 (s)
2,855.4 (s)
0
Aurum
1996-1997
40 UG
9,242.55 (UG)
780
Trumpeter Yukon Gold
and Omni
Resources
2003
3 (s)
974.74 (s)
0
TLGC
2004
2(s)
~900 (s)
0
TLGC and
Yukon Government
2008
3 UG
342.6 UG
0
TLGC
1987-2008
TOTALS 34 (s)
43 UG
~11,136.74 (s)
9,585.15 UG
780
Various
NOTES: UG = Underground; (s) = surface; TLGC = Tagish Lake Gold Corp.; ND = no data.
The Goddell Gully has also been referred to as the Golden Tusk Zone and the PD Zone, and
the Main Zone in previous reports; the Golden Tusk Zone stratigraphically overlies the PD. Zone
by about 350m. The Goddell Gully portal was collared in 1996 and is located at 1,017.86m
portal elevation. The two drill holes completed in 2004, numbers GG03 and GG04, should to be
compiled into the Skukum drillhole database. (Johnson and Fan, 2010).
14
Table 6.3
Years of
Drilling
Total Number of Total amount of
Drill holes
drilling
completed
completed (m)
Target Zones
Companies Involved
1982
29
3,325.80
Main Cirque
Agip
1983
40
4,380.52
Main Cirque, Brandy
Agip
1984
61
6,097.50
Brandy, cirque, lake
Agip
1985
6
168.42
Cirque
Ericson
1986
72
8,864.96
Brandy, Cirque, lake
Mount Skukum Gold Mining
17,125.47
Evening, ocean,
midnight, pika, falls,
lake, Cirque, fox,
wunder, brandy, gully
1987
6.3
Drilling Conducted at Mt. Skukum (1982 to 1999)
153
1988
106
12,373.45
Ocean, morning, pika,
tango, lake, Cirque,
fox, kiwi, brandy,
sulphide
1989
14
3,214.73
Ocean, tango, goat
1991
3
576.38
Ocean
Wheaton River Mineral
1997
5
608.08
Ocean
Omni
Historical Exploration Results
The exploration results are primarily discussed under Historic Resource Estimates.
6.4
6.4.1
Historical Sample Preparation, Analyses and Security
General Comments
Samples were analyzed at a number of laboratories, including Acme Analytical Laboratories Ltd,
Bondar-Clegg Laboratories, and Chemex Labs, all located in Vancouver, British Columbia.
Northern Analytical of Whitehorse, Yukon, Little Salmon Analytical of Carmacks, Yukon and
Barringer-Magenta of Calgary, Alberta were also utilized. All laboratories conducted internal
quality control procedures such as using standards and blanks as control samples and repeat
assays. There are no documents available that describe the quality control measures taken by
the previous operators. Since 1986 all results of assays are documented as printed copies in
binders and are stored at the camp office. The assay results are accompanied by certified
copies. The following is a description for the three deposits within the Tagish property.
6.4.2
Mt. Skukum
No information was available concerning sampling or quality control procedures used for the Mt.
Skukum deposit. A small analytical laboratory was set up on site during exploration and mining
phases. Assaying procedures are unknown. Several external laboratory certificates were
discovered, but those represent only a small portion of the number of assays that were carried
out. No specific information on sample security was discovered.
15
6.4.3
Skukum Creek
Prior to 2001
The available information indicates that all Skukum Creek samples were assayed by third party
laboratories. No control samples are known to have been submitted by the Property owner,
though some samples of higher grade were sent for re-assay at a second laboratory. Surface
samples were analyzed using multi-element ICP with higher grade samples being re-assayed
by fire assay. Drill core samples were almost exclusively fire assayed, though some were
assayed using unspecified geochemical analyses.
Metallic fire assays on selected samples were carried out to determine if coarse-grained gold
was present. Results suggested that the gold was fine-grained. A notice regarding proper core
handling procedures was found at the existing core logging facility, though no specific
information on sample security was discovered.
2001 and After
Records indicate that the practices employed in sample preparation, analysis and security
followed industry practices and that they were in compliance with NI 43-101 standards and
regulations. Sample preparation and analysis were carried out in accredited commercial
laboratories including Eco-Tech Laboratory Ltd (Eco-Tech), based in Kamloops, BC and Acme
Labs, based in Vancouver, BC.
In 2002, samples were analyzed by ACME Labs (ISO 9002 certified), who applied multi-element
analysis by ICP-ES after acid digestion. ICP-MS analysis after aqua regia digestion was used
for gold. When gold values were greater than 900 ppb or silver values were greater than 100
ppm, they were re-analyzed using fire assay techniques. Bondar Clegg Canada Ltd (ISO 9002
certified) of North Vancouver, BC carried out check analyses (Naas, 2002).
Eco-Tech Laboratory Ltd (Eco-Tech), based in Kamloops, BC has carried out TLG’s assaying
since 2003. Samples are weighed to 30 grams and fused along with proper fluxing materials.
The bead is digested in aqua regia and analyzed on an atomic absorption instrument. Overrange values for rocks are re-analyzed using fire assay and AAS finish methods. Appropriate
reference materials accompany the samples through the process allowing for quality control
assessment.
Security was considered during diamond drilling. When a hole was approaching the mineralized
zone, an experienced CME representative was constantly present at the rig. The core was
never left unsupervised and was taken by the CME representative to a locked room at the end
of shift. No one could enter the room without supervision. The core was cut using a rock saw
and half the sample was placed in a sample bag. The bag was then heat-sealed and placed
back in the locked room. A CME representative transported the samples to a reputable courier
in Whitehorse where the accredited preparation laboratory organized transportation of pulp
samples to assay labs by courier.
16
6.4.4
Goddell
Third party laboratories appear to have analyzed all of the samples from Goddell Gully. Soil
samples were analyzed for gold using unspecified geochemical methods. Silver and base
metals results are also reported, but by what process those analyses were made is unknown.
Drill core samples were analyzed for gold using both fire assay and unspecified geochemical
methods. Silver and base metals were also inconsistently assayed. During the late 1990s,
surface samples were analyzed using multi-element ICP and unspecified geochemical methods
with higher-grade samples being re-assayed using fire assay analysis. Metallic fire assays on
selected higher-grade samples were carried out.
6.5
Data Verification used for Historical Resource Estimate of the Skukum Creek and
Goddell Deposits
CME carried out a sample verification program in 1999 as part of a due diligence study. Six
diamond drill holes were selected for re-sampling, four of which were from the Rainbow Zone of
the Skukum Creek deposit and two of which were from the P.D. Zone of the Goddell Gully
deposit. Forty-six samples were re-assayed using fire assay analysis and multi-element ICP.
The re-assay was carried out by Chemex Labs of Vancouver, BC, while ACME Analytical
Laboratories Ltd, also of Vancouver carried out the original assaying. Except for three samples,
the verification samples showed acceptable correlation with historical counterparts/samples. It
was thought that mislabeling may have been the reason behind the three samples with poor
correlation. When the entire main mineralized zone of the drill hole from which the three
samples were taken was re-sampled, acceptable correlation with historical results was obtained.
In 2003, when Roy, P.Geo, of MineTech did a resource estimate, several verification samples
were selected from existing drill core and channel samples to confirm the presence of
mineralization. A total of five samples were selected. For the Skukum Creek deposit, one
sample was selected from 1980s exploration, one from 1990s exploration, and one from
underground channel sampling. From Goddell Gully, one sample was selected from 1980s
exploration and one from 1990s exploration. Four additional verification channel samples were
taken near historical samples in the Rainbow Zone on the 1,350, 1,300, and 1,250m levels. The
results confirmed the presence of gold in all samples and silver in the Skukum Creek samples.
The four core samples more accurately verified the original samples. Of those, two returned
lower gold grades than the original samples, one returned a similar grade, and one returned a
much higher grade. The channel samples were not taken in exactly the same locations as the
original samples; however, they confirmed the presence of gold and silver in the underground
workings. As such, Mr. Roy was satisfied with the data verification.
In 2007 when Roy was retained by TLG to do a resource update of the Berg Zone and Rainbow
Zone of Skukum Creek, he took several measures to verify the data. The verification measures
include database checks for logical errors, checking the data file provided by TLG against the
original assay certificates, taking verification samples from drill cores and checking a face
sample taken from the 1,300 metre level. Roy concluded the results of verification sampling
were within acceptable limits.
17
6.6
Historical Resources and Reserves
There are numerous historical estimates of resources and reserves of the deposits in Tagish
completed by in-house professionals of numerous companies and third party consultants since
late 1980s. The most recent estimates were made by MineTech in 2003 on the Skukum Creek
deposit and Goddell deposit and a 2007 resource update on the Skukum Creek deposit. The Mt.
Skukum gold deposit has a historical reserve estimate dated 1988.
The following is a summary of the historical estimates. No new exploration drilling has occurred
since the above mentioned estimates were published. All of the following estimates are
being treated as historical estimates by New Pacific. A Qualified Person has not done
sufficient work to classify the historical estimates in this section as current mineral
resources or mineral reserves.
A Qualified Person should review the models that were created for the historical
resources to confirm all the mineralization was outlined. The models should be rerun at
current metal prices used for resource estimates. The historical resources should not be
relied upon until the mineralization review is completed and the models are rerun at
current metal prices.
The historical estimates in this section use the categories set out in sections 1.2 of the NI
43-101 Standards of Disclosure for Mineral Projects.
6.6.1
Historical Resource Estimate 2003 Skukum Creek and Goddell
For the purpose of this section the new NI 43-101 definition of historical resource is
used. The historical estimate has not been verified by New Pacific as a current mineral
resource and the estimate was prepared prior to New Pacific acquiring the property.
MineTech was commissioned by TLG to complete a resource estimate for the Skukum Creek
and Goddell deposits in August 2002, and this work was completed in June, 2003 with the
technical report “Tagish Lake Gold Corporation Skukum Creek and Godell Gully Deposits”. The
historical estimate uses metal prices of $300 Au and $4.50 Ag. The metal prices used are
significantly lower than current metal prices and the estimate may not reflect the resource at
current prices. The estimate uses the category definitions of resources as per section 1.2 of the
instrument.
Data Verification and Site Visit
MineTech reviewed all technical reports provided by TLG and by CME, and examined the
QA/QC program that formed the basis for the sampling system. Roy visited Tagish in
September 2002 during a diamond drilling campaign supervised by CME, collected samples
and verified the presence of gold and silver mineralization through an independent assay
laboratory (ALS Chemex based in Vancouver), observed the sampling system, and discussed
the geological setting with the site geologists.
Methods of Estimation used for the Historical Mineral Resources
The resource estimate was done using MicroLynx resource estimating and mine planning
software. All drilling and underground channel sampling data was checked for errors and
sample statistics were examined.
18
For Skukum Creek, all sample data were collected as of the end of 2002, totaling 5,135 gold
samples and 4,885 silver samples. For Goddell, there were 3,949 core samples in total. At
Skukum Creek, specific gravity was estimated using inverse distance weighting. At Goddell, an
average specific gravity value of 2.7 t/m3 was used as no specific gravity sampling had been
carried out.
At Skukum Creek, drilling and sampling data were translated to 475,000m west and 6,675,000m
south and rotated clockwise 35°. Drilling and channel samples were downhole composited or
regularized over one metre intervals. Equivalent gold grades were calculated for each
composited silver sample; however, gold and silver grades were calculated separately for each
block. The equivalent grade was equal to the silver grade multiplied by the ratio $4.50/$300 or
0.015, where $4.50 and $300 were the average respective silver and gold prices (in $US per
troy ounce).
Cross sections were created to show geology and the equivalent gold grades at 1:1000 scale
spaced 25m apart in the Rainbow and Kuhn Zones, and 50m apart in the Ridge Zone. Shear
zone geology and an outline of "higher grade" material greater than 5 g/t within the shear zone
were outlined on hard copies of the sections. Both shear zone and high grade outlines were
digitized and solid models were made, producing eight shear zone subzones and twelve
"outline" subzones.
The high grade outline model was used to construct a block model with dimension of 2m3, subblocked five times across strike and twice down-dip. Concurrently, a polygonal resource
estimate was carried out, consisting of calculating the average grade of all samples within each
section that were within the outline. Calculating the area of each section and multiplying that by
the section width and average specific gravity gave the mass of each section. Measured
Resources were identified as blocks that were within 15m from two underground channel
samples, Indicated Resources were identified as blocks that were within the outline and were
less than 25m away from at least two samples.
At Goddell, the same procedure for outlining geology was used as for outlining geology at
Skukum Creek. An outline value (not an economical cut-off value) was created using 5 g/tonne
as a guide for the outline's outer limits. East-west sections were created at 1:1,000 scale using
a section spacing of 50m, except for a 100m portion over which a 25m spacing was used. Two
zones were outlined and a specific gravity of 2.7 t/m3 was used. A block model was constructed
with block dimensions of 2m3. Each block was subdivided five times across the strike dimension
and twice in the vertical dimension to allow finer geology resolution. A polygonal method was
used to estimate resources. Indicated Resource was defined as within 15m of sampling and
Inferred Resources within 25m of sampling.
6.6.2
Results of Estimate
A summary of the estimate results are shown in Tables 6.4 and 6.5 below. The total contained
metal does not consider metallurgical recovery. An equivalent gold cut-off grade was calculated
using $300 and $4.50 ($US per ounce) for gold and silver prices, respectively. Tonnage value of
each zone is individually rounded. The subtotal is the rounded sum of the non-rounded values.
19
Table 6.4
2003 Summary of Skukum Creek Resources Using a 3 g/t Cut-off Grade
Measured
Zone
Tonnes
Au
Grade
(g/t)
Indicated
Ag
Grade
(g/t)
Ridge
Measured+Indicated
Tonnes
Au
Grade
(g/t)
Ag
Grade
(g/t)
Tonnes
Au
Grade
(g/t)
Ag
Grade
(g/t)
60,000
5.14
145
60,000
5.14
145.00
Kuhn
51,000
10.88
95
260,000
5.19
127
310,000
6.12
122.00
Rainbow
165,000
3.79
266
550,000
6.05
198
710,000
5.53
214.00
Subtotal
220,000
5.46
226
870,000
5.73
173
1,080,000
5.68
184.00
Inferred
Ag
Grade
(g/t)
Zone
Tonnes
Au Grade
(g/t)
Ridge
68,000
5.56
157
Kuhn
39,000
4.02
129
Rainbow
43,000
5.53
225
Subtotal
150,000
5.15
169
Table 6.5
2003 Summary of Goddell Resources Using a 3 g/t Cut-off Grade
Indicated
6.6.3
Inferred
Zone
Tonnes
Au Grade
(g/t)
Metal (oz)
Tonnes
Au Grade
(g/t)
Metal (oz)
PD
400,000
9.55
123,000
350,000
8.11
91,000
Resource Update 2007 Skukum Creek Deposit
In November 2006, TLG again retained MineTech to do an update of the resource of the
Skukum Creek deposit based on drilling on the Rainbow 2 and Berg Zones between 2003 and
the end of 2006. A technical report titled “A Resource Report Update for the Skukum Property”
was released in August 2007.
The 2007 historical estimate was an update to the resources on the Goddell property
based on drilling in the Rainbow 2 and Berg Zones. These zones are in addition to the
zones in the 2003 historical estimate.
The metal prices used in 2007 were $650 for Au and $13 for Ag.
Data Verification and Site Visit
Roy was the principal author of the resource report. He visited the project site in May 2007,
spoke with site geologists, reviewed the QA/QC procedures, inspected the site and
underground workings and verified assay data by both checking data against original assay
certificates and taking verification samples. He concluded that the sample preparation, assay
procedures and security measures were adequate, and the results of verification sampling were
within acceptable limits (Roy and Hannon, 2007).
20
Methods of Mineral Resource Estimate
The resource estimate was done using Micromine Version 10.1.2. Prior to estimate, the
supplied data was checked for logical errors. Gold equivalent was calculated based on metal
prices of gold at US$650 and silver at US$13 per troy ounce to establish cut-off grade for the
purpose of outlining mineralized zones and reporting resources, but block value was estimated
separately for gold and silver. Top-cut values were set at 35 g/t for gold and 350 g/t for silver.
Mineralized zones were interpreted on paper and then digitized in computer. A cut-off grade of 2
g/tonne of gold-equivalent over a minimum horizontal width of 1.2m was used. Inverse-distance
weighting was chosen for grade estimation. Separate two-dimensional block models were
created for each zone. Block dimensions were 5m x 5m (in the East and Elevation directions).
Block thickness values (North direction) were calculated during the estimation process. The
geometry of each zone was constrained by the geological outlines. Grade estimation was
carried out using inverse distance weighting with a power of two. Horizontal thickness values
were calculated for each drilling intercept and inverse distance (ID) weighting with a power of
three was used to estimate block thickness values. Block specific gravity values were also
estimated using inverse distance weighting with a power of two.
Indicated Resource was defined as within the outlined geology and within 20m of at least two
drilling intercepts, and Inferred Resource as within the outlined geology but within 40m of at
least one drilling intercept. There was no Measured Resource category since no samples were
from underground channel sampling.
6.6.4
Results of Estimate
The resource estimate results in 2007 for Rainbow 2 and Berg zones are summarized in
Table 6.6 using cut-off grades of 3 g/t and 4 g/t gold equivalent respectively (Roy and Hannon
2007, p.37 and p.41):
Table 6.6
2007 Summary of Rainbow 2 and Berg Zones of Skukum Creek Resources
Indicated
Cut-off
(g/t
Tonnes
AuEq)
6.7
Au
Grade
(g/t)
Inferred
Ag
Au Metal Ag Metal
Grade
Tonnes
(oz)
(oz)
(g/t)
Au
Grade
(g/t)
Ag
Grade
(g/t)
Au Metal Ag Metal
(oz)
(oz)
3.0
126,000
8.0
101
32,408
409,000
101,000
7.2
99
23,380
321,000
4.0
110,000
8.8
108
31,000
382,000
81,000
8.4
106
21,876
276,000
1988 Historical Reserve Estimate of Lake Veins of Mt. Skukum Gold Deposit
There were various versions of historical mineral reserve estimates of the Mt. Skukum deposit.
The most frequently cited historical reserve estimate is the one of the Lake zones in an
unpublished report by Macdonald of Agip in 1988. There was inadequate supporting data for the
author to validate the estimate and the author does not consider the estimate to be reliable for
public disclosure. The Lake Veins are mentioned in this section for the sole reason that the
prospect has high exploration potential in the Lake Veins area.
21
7
GEOLOGICAL SETTING
The Mt. Skukum, Skukum Creek and Goddell mineralization are geologically situated in a
subvolcanic to volcanic caldera system which is underlain by a dome (or several dome)
complexes. Subvolcanic stocks, dykes and breccias follow extensional and transtensional
tectonic features of the stratovolcanic and volcanic edifices. The mineralization pulses were syn
to late-tectonic and related to the Tertiary volcanism.
7.1
Regional Geology
The regional geological setting of the Skukum project area is described in Hart and Radloff
(1990), from which the following information is summarized.
The project area is located within the Intermontane Belt of the Canadian Cordillera. The oldest
rocks in the area are comprised of domains and screens of probable Paleozoic gneiss, assigned
to the Nisling Terrane by Hart and Radloff (1990), and Jurassic andesitic volcanic and
siliciclastic sedimentary rocks of the Stikine Terrane and Whitehorse Trough overlap
assemblage. Stratigraphic and contact relationships are commonly obscured by the many
intrusions associated with the Coast Plutonic Complex. Strata of the Jurassic Whitehorse trough
are affected by a series of open to tight, northwest-trending folds that probably formed in Upper
Jurassic to Lower Cretaceous time, approximately coeval with activity of the Skeena Fold Belt to
the south in British Columbia. The folds are superimposed on earlier, probably pre-Triassic,
metamorphic fabrics and the northwest-trending Tally-Ho shear zone, a major Late Triassic
shear zone that is developed approximately 15 km to the northeast of the project area and
which forms the easternmost limit of exposures of the Nisling Terrane.
Mesozoic plutonic rocks, which underlie much of the project area, separate the Jurassic units
and Nisling Assemblage into isolated domains and screens. Major intrusions include the
Alligator Quartz Monzonite and the late Triassic or early Jurassic K-feldspar megacrystic
Bennett Granite that are widespread east of the Wheaton River in the Skukum project area. The
most abundant rock types in the region comprise metaluminous Cretaceous intrusions of the
Coast Plutonic Complex, which are subdivided into several plutonic suites by Hart and Radloff
(1990). The dominant Cretaceous suites in the project area include the Mt. McIntyre plutonic
suite (96 to 119 Ma), comprising the Mt. Ward granite and Carbon Hill quartz monzonite, and
the Whitehorse plutonic suite (116 to 119 Ma), locally represented by the Mt. McNeil
granodiorite pluton. Isolated accumulations of mid- to late-Cretaceous volcanic rocks of
intermediate composition of the Mt. Nansen Group are present regionally and are approximately
coeval with the Coast Plutonic Complex.
At the Skukum property, these rock types occur on the eastern flanks of Carbon Hill and
southeast of Goddell Gully near the Becker-Cochran prospect, where they comprise green tuff
and tuff breccia that unconformably overlie the Bennett Granite and Jurassic strata.
Late Cretaceous and Early Paleocene brittle dextral displacement associated with widespread
dextral displacement throughout the Cordillera is related to reactivation of the Triassic Tally-Ho
shear zone. This phase of displacement formed a brittle fault system, termed the Llewellyn fault
by Hart and Radloff (1990), which exploited parts of the earlier Tally-Ho structure.
22
Subsidiary faults generated during this tectonic episode may subsequently have been
remobilized during Eocene volcanic activity to locally form caldera-bounding structures; these
may also have acted as permeable structural sites for the formation of the late-volcanic vein
deposits hosted by faults and shear zones in the Skukum project area.
Figure 7.1
SimplifiedGeology Map of the Tagish Property
23
Table 7.1
Stratigraphy Units of the Tagish Property
ERA
PERIOD
FORMATION
LITHOLOGY
Quaternary
Unconsolidated surface alluvium
Pleistocene
Glacial and glaciofluvial deposits
Cenozoic
Erosional Interval
Late Paleocene
to
Early Eocene
Skukum Group (Mt.
Skukum Volcanic
Complex)
Felsic to intermediate volcanic flows, breccias,
ash to lapilli tuffs and related epiclastic rocks and
pyroclastic flows, felsic dyke emplacement,
quartz veining and mineralization.
Paleocene - Unconformity (Intrusive Contact)
Middle
Cretaceous
Coast Plutonic
Complex (Mount
McIntyre Plutonic
Suite)
Carbon Hill Plug: recessive, granular weathering
biotite-quartz monzonite and granophyric,
hornblende and alkali-feldspar granite
Mid-Cretaceous
dykes, plugs
Siliceous pale green, saccharoidal rhyolite and
aplite
(Whitehorse Plutonic
Suite)
Mr. Anderson Pluton: Biotite and porphyritic
hornblende granodiorite.
Mount Nansen
Group (Carbon Hill
Volcanics)
Undifferentiated volcanics, andesite flows and
breccias, tuffaceous andesite.
Lower Cretaceous - Erosional Unconformity
Mesozoic
Late
Jurassic
Tantalus Formation
Chert pebble conglomerate,
polymictic conglomerate and related siliciclastic
rocks.
Late Jurassic
Volcanics
Andesite porphyry flows, breccia, epiclastic
rocks.
Erosional Unconformity
Early Jurassic
Alligator Quartz
Monzonite
Foliated hornblende-quartz monzonite to
granodiorite
Bennett Granite
Megacrystic, potassium feldspar-hornblende
granite to granodiorite to quartz monzonite.
Erosional Unconformity
Paleozoic and
Older (?)
Late Triassic
to Paleozoic
Nisling Assemblage
Rusty weathering metavolcanic schists, quartzite
and marble; minor black argillite.
(After G. L. Wesa and T. M. Elliott, 1999)
24
7.2
Local Geology
The local geology at the Skukum property is shown in Figure 4.2. The following local geology
descriptions were taken from Naas (2004).
7.2.1
Proterozoic to Paleozoic Metamorphic Rocks
Metamorphic rocks of the Nisling Terrane underlie the western extent of the Property
(Charleston area), and occur as isolated roof pendants in the Chieftain Hill and Goddell areas of
the Property. The encountered metamorphic rocks comprise three units, the Nisling and Nasina
assemblages as well as undifferentiated gneiss.
Nisling Assemblage
The Nisling Assemblage is comprised of rusty-brown weathering, competent non-fissile biotite,
muscovite-quartz feldspar schist, quartzite and marble. A planar foliation is well developed
parallel to compositional layering. Compositional layering is observed in the schists and
quartzites from 1-2 cm wide and from 1-100m wide in the marbles.
Nasina Assemblage
These rocks are very similar to the Nisling Assemblage in composition but distinguishable by
graphitic, commonly garnet-bearing quartz schists and lesser marble. The best exposures are
seen to the west of Mt. Skukum. The rocks are also well foliated but fissile due to partings on
the graphitic layers. The typical lithology is garnet-muscovite, garnet-graphite schists and
carbonaceous quartzite.
Undifferentiated Gneiss
Feldspar-hornblende orthogneiss with minor biotite, epidote, and chlorite are found on Chieftain
and Carbon Hills in the Wheaton River area. This unit is not in actual contact with the other two
but has been included in the Nisling Terrane based on descriptions and other relationships
determined by other workers.
7.2.2
Probable Jurassic Volcanic and Siliclastic Rocks
Conglomerate
Pebble conglomerate is present in several drill holes completed historically at the eastern end of
the Rainbow zone, immediately southwest of Skukum Creek. The unit is composed of clastsupported conglomerate with rounded clasts of chert and quartzite in a pale green sericitic
matrix. This unit probably belongs to the Jurassic Tantalus Formation (Hart and Radloff, 1990).
It is present in an area of no outcrop and core is incomplete and partially lost for the holes
containing this unit, so its contact relationships and orientation could not be assessed.
Conglomerate that has been mapped along the southeastern flanks of Chieftain Hill by Mt.
Skukum Mines (unpublished mine maps; Hart and Radloff 1990), and which is intercalated with
Jurassic volcanic rocks, may also correlate with this unit.
25
Intermediate Volcanic Rocks
Holes drilled in the Rainbow East zone (RACA97-1 to RACA97-3) first pass through thick,
recent talus of fresh Tertiary volcanic rocks, and then intersect pale grey,
sericite+pyrite±magnetite altered, locally plagioclase±pyroxene porphyritic volcanic rocks of
probable intermediate composition. Main rock types include massive, grey lapilli to block tuff
and tuff breccia, and massive porphyritic flows or sub-volcanic intrusive rocks. These units are
distinct from the fresh Tertiary volcanic units present in talus higher on the slope. Their altered
state, close spatial association with Jurassic conglomerate of the Tantalus Formation that is
present immediately across Skukum Creek, and occurrence of Cretaceous intrusive rocks within
them suggest that they may correlate with Jurassic pyritic andesitic volcanic rocks present on
the eastern flank of Chieftain Hill 2 km to the northeast. Since these volcanic units are present in
an area of poor exposure under talus, their contact relationships with adjacent rock types is
unknown.
7.2.3
Intrusive Rocks
Ten types of intrusive rocks of widely variable composition and texture are identified underlying
the Property. In general, the rocks comprise at least three larger intrusive masses and
numerous dykes, including andesitic and rhyolitic dykes of Tertiary age. The dykes are most
abundant within and immediately adjacent to major fault zones, which probably provided the
structural control for their emplacement. In some cases, the appearance of certain types of
dykes can be significantly modified by hydrothermal alteration and lead to confusion in
assignment.
7.2.3.1
Pre-Tertiary Intrusions
Biotite-hornblende granodiorite (Mt. McNeil pluton; Cretaceous)
Within the Skukum project area, the Mt. McNeil pluton underlies the valley of Berney Creek, Mt.
Reid and the south side of Skukum Creek, immediately to the south of the Mt. Skukum volcanic
complex. Hart and Radloff (1990) report a 111 Ma U-Pb zircon age from the pluton in the
Skukum project area. This intrusion is the most common host rock to the Skukum Creek
deposits. It is characterized by large, euhedral hornblende grains that locally exceed 1 cm in
length but which are mostly 3 to 6 mm long. The unit is coarse-grained and equigranular to
seriate. It typically contains approximately 10% hornblende, 5% biotite, 25 to 30% quartz, 30 to
35% plagioclase and 20% K-feldspar, providing an IUGS classification as biotite-hornblende
granodiorite. Fresh rock contains abundant magnetite. Partially disaggregated cognate xenoliths
of fine-grained diorite are common. Where fresh, it is strongly and evenly magnetic. Hornblende
and biotite have been at least partially replaced by greenish chlorite in even the freshest
samples. Alteration is pervasive and much stronger close to major shear zones.
K-Feldspar megacrystic biotite-hornblende granite (Bennett Stock; Triassic-Jurassic)
Drill holes completed in the Rainbow East zone on the northeast side of Skukum Creek (holes
RACA97-1 to 3) intersected a foliated K-feldspar megacrystic granite, which based on textural
and mineralogical similarities is interpreted to be the Bennett granite which is widespread in the
region. Doherty and Hart (1988) report a U-Pb zircon age for the Bennett granite of about
220 Ma, although other U-Pb dates in the region return approximately 175 Ma (J. K. Mortensen,
pers. comm. 2002).
26
This unit is broadly similar to the biotite-hornblende Mt. McNeil granodiorite at Skukum Creek,
but is distinguished by (i) the presence of megacrysts of euhedral K-feldspar up to several
centim in size in a coarse-grained, equigranular matrix; and (ii) a higher K-feldspar/plagioclase
ratio. It is properly called granite. This unit is invariably altered near veins and shear zones.
Porphyritic hornblende monzonite to quartz monzonite
This unit is present as irregular bodies and dark dykes within the Mt. McNeil pluton in the vicinity
of the Skukum Creek deposits. It commonly contains inclusions of the Mt. McNeil granodiorite.
The unit typically has a salt and pepper texture that reflects subequal concentrations of euhedral
hornblende prisms and equant, white plagioclase phenocrysts. The groundmass is dark and
fine-grained. Some variations on this rock type contain minor quartz. Plagioclase phenocrysts
typically form approximately 40% of the rock, but locally exceed 50% requiring it to be called a
porphyry. The moderate response to K-feldspar staining is consistent with monzonite. This rock
type is common in the Skukum Creek area, but it was not observed at Goddell Gully or Chieftain
Hill. Where present within or near mineralized shear zones, this unit is invariably altered. The
rock locally contains minor cognate diorite xenoliths, but their concentration is markedly less
than in the Mt. McNeil granodiorite.
Biotite-pyroxene monzodiorite
This rock type was observed only in the Skukum Creek area within the Taxi zone, and in DDH
98GE-1 located southeast of the Rainbow and Kuhn zones. In the Taxi zone, a diorite cross
cuts the Mt. McNeil granodiorite, whereas at Golden Eagle an opposite relationship was
observed. The intrusions in each example are medium-grained and equigranular. Quartz is
locally present in minor (<5%) concentrations, and the rock is moderately magnetic. Biotite and
pyroxene together make up 30 to 35% of the rock. Kfeldspar staining indicates that this rock
type is most appropriately described as a biotite-pyroxene monzodiorite or quartz monzodiorite.
Both dioritic bodies that were encountered have a weak foliation and are cut by chloritic and/or
sericitic veinlets.
Biotite granite
This is a medium-grained, equigranular intrusive rock that occurs locally in the Taxi zone and in
drill holes south of the Kuhn Fault. It typically has no or only minor alteration or fabric. Dykes of
this rock type cross cut the Mt. McNeil granodiorite, but were not observed in contact with other
intrusions. The rock is moderately magnetic and the only ferromagnesian phase is biotite. It is
cut locally by chlorite or sericite veinlets.
Hornblende-biotite quartz monzonite (Carbon Hill pluton of Mt. McIntyre Plutonic Suite)
This is the main host rock to the Goddell Gully and Porter fault zones on the east side of the
Wheaton River valley. Hart and Radloff (1990) report a poorly constrained K-Ar date of
96±15 Ma for this intrusion, which is broadly consistent with 107 to 110 Ma U-Pb zircon results
obtained from other plutons of the same plutonic suite in the area. It is a medium-grained,
equigranular rock with subequal K-feldspar and plagioclase and about 20% combined
hornblende and biotite. It is moderately magnetic, but less so than the Mt. McNeil stock. It has
invariably been affected by strong alteration where close to the Goddell Gully and Porter fault
zones. No temporal relationships were observed with other intrusions except for cross-cutting
Tertiary rhyolite and andesite dykes.
27
Pegmatites and aplites
These were observed mainly in the Mt. McNeil granodiorite in the Skukum Creek area. They are
most abundant in areas that are also cut by biotite granite dykes, to which they might be related.
They are late magmatic features that are cut by minor shear zones and altered. None of these
dykes observed during this study exceed 0.5m in width (most are <5 cm wide), and they are
widely dispersed through the host intrusions. One small aplite graded to a core of clear quartz, a
pattern common to aplites in many systems.
7.2.3.2
Pre-Tertiary Volcanics (Mt. Skukum Volcanic Complex)
The complex is an early Eocene, bimodal sequence of sub-aerial volcanic and volcaniclastic
rocks that have been deposited over approximately 140 km2. The complex trends northeast in a
20 by 11 km ellipsoid, bounded by faults to the south and east, and divided into two parts by two
north-south trending faults. The eastern part has been down dropped by as much as 300m
relative to the western block (Pride, 1986). The eastern portion of the complex is comprised of
mainly felsic pyroclastic rocks intercalated with brecciated flow-banded and spherulitic rhyolite
lava flows. These felsic units are particularly thick in the northeastern and southeastern parts of
the complex where prominent large-scale arcuate fracture systems, large slump blocks, vent
facies pyroclastic rocks and other features indicate centres of volcanism and associated
margins of nested caldera subsidence. The western block is underlain by at least 850m of
andesite, which hosts the Mt. Skukum gold deposit. The andesite unconformably overlies the
basement of metamorphic Nisling Terrane and intrusive Coast Plutonic Complex on a highly
irregular erosional surface (Jago, 1991).
The understanding of the stratigraphy of the Mt. Skukum Volcanic Complex has evolved over
time by the various workers. The following terminology is based on the work of Hart and Radloff
(1990):
Ibex Formation: dark, vitreous, flow-banded rhyodacite flows with sparse feldspar phenocrysts
and welded tuff and common granitic fragments. This unit may or may not be part of the
Skukum Group but is found overlain by Butte Creek Formation.
Mount Reid Formation: Massive, hematitic, clast-supported, cobble and boulder conglomerate
with locally derived basement fragments.
Butte Creek Formation: consists of three sub-units of well-bedded, pastel coloured felsic and
altered felsic pyroclastic rocks with layers of grey, green and purple layers interlayered
epiclastic sediments and tuffs, and undivided tuff and epiclastics.
Watson River Formation: massive to poorly-bedded, dark-brown and purple to pale green
columnar-jointed andesite and andesite porphyry flows, as well as pale green dacitic to
andesitic lithic tuff.
Vesuvius Formation: consists of a variety of rhyolite tuffs and flows, lithic tuffs, and a collapse
breccia of large blocks of flow-banded rhyolite. The various sub-units range in colour from dark
reddish-brown to green and tan to grey.
28
7.2.3.3
Tertiary Dykes and Stocks
Andesite dykes
These intrusions are widespread throughout the project area, but are generally most common
within or adjacent to major fault zones (rhyolite dykes below). The most common types are
either aphanitic and dark grey, or have a porphyritic texture defined by hornblende and
plagioclase. Both types of dyke may be altered and locally mineralized. Some of the aphanitic
dykes may be narrow equivalents of the porphyritic monzonite phase described above. The
porphyritic examples are relatively more common at Goddell Gully. Staining indicates that the
dykes are actually monzonite and porphyritic hornblende monzonite, with lesser andesite. The
andesite was observed to cut most of the pre-Tertiary phaneritic intrusive rocks. Some andesite
dykes are older than some rhyolite dykes. Several types of andesite dyke are probably present
in the area, but additional work needs to be done. Andesite dykes that intrude pre-Tertiary rocks
in the region may represent subvolcanic feeders to the Mt. Skukum volcanic complex.
Rhyolite dykes
These intrusions comprise a diverse group of felsic dykes that are variable in mineralogy,
texture, and their spatial and temporal relationships to hydrothermal alteration and
mineralization. Rhyolite dykes were observed to cut most intrusions on the Property, but have
variable timing relative to andesites as noted above, suggesting multiple pulses of both intrusive
types. Like the andesite dykes, rhyolite dykes commonly have a spatial association with, or are
developed within, major east- and northeast-trending fault systems. In the Skukum Creek and
Chieftain Hill areas, typical rhyolite characteristics include a buff to light grey colour, and an
aphanitic texture with up to 10% clear, rounded to square and locally resorbed quartz
phenocrysts (mostly <3 to 4 mm in size). Prominent flow banding is well developed near the
contacts of many of the larger dykes.
Three distinctive quartz±K-feldspar porphyritic dykes that are present in the Goddell Gully area
along the Goddell fault belong to the rhyolite dyke group. These have been termed the North,
Central and South marker dykes in old drill logs, based on a consistent and predictable
distribution along strike. The North and South Marker dykes lack flow banding and have a
higher concentration of K-feldspar phenocrysts and more variable concentrations of quartz
phenocrysts than the Central Marker dyke. The Central Marker dyke has well-developed flow
banding, overall texture, equant quartz phenocrysts, and alteration and disseminated pyrite that
makes it much more similar to the mineralized rhyolite dykes at Skukum Creek. The relative age
of the three rhyolite dykes at Goddell was not established.
A single, narrow spherulitic rhyolite dyke was observed in the Ridge Zone. It is characterized by
spherules <4 mm in size and several percent disseminated pyrite; the age of this intrusion
relative to other types of rhyolite dyke is unknown but similar intrusions at Mount Skukum were
considered by McDonald et al. (1990) to be among the youngest rock types in the area.
Post-hydrothermal amygdaloidal andesite dykes
These occur in several places at Skukum Creek. They are invariably fresh and undeformed,
even where located close to known mineralization, and are consequently interpreted as posthydrothermal. These dykes range up to several metres in width. They have a fine-grained to
aphanitic, dark-colored groundmass, and are distinguished by white to clear amygdules infilled
29
by quartz and/or calcite. Similar dykes were interpreted to be the latest stage of intrusive activity
in the vicinity of the Mount Skukum mine (McDonald et al., 1990).
Alteration
Zones of strong porphyry type alteration can be observed across the entire Property. Stronger
alterations occur along the fault controlled and affected outcrops. The dominating secondary
(alteration) mineral besides the classic iron oxide (hematite) and iron hydroxide minerals
(goethite, limonite) is sericite. Its occurrence is widely spread indicating hydrothermal fluids
penetrated the various igneous host rocks.
30
8
DEPOSIT TYPES
There are three known precious metal deposits on the Tagish Lake Property. They can be
divided into three deposit types: epithermal auriferous quartz-calcite vein type, mesothermal
gold-silver quartz sulphide vein type and the third one is an epithermal shear zone hosted
disseminated sulphide associated gold deposit.
Epithermal auriferous quartz-calcite vein type
This type includes the zones of Lake, Main Cirque, Brandy and others at Mt. Skukum. Low
temperature auriferous quartz-calcite veins emplaced along open space of fractures and faults
formed at shallow level of Tertiary volcanic rocks of the Mt. Skukum volcanic caldera complex.
Both gold grade and zone thickness change dramatically along strike and down-dip directions
with frequent swelling and pinch-out. Free gold has been identified in the rocks and the
mineralized veins contain little sulphides.
Mesothermal gold-silver quartz sulphide vein type
This type includes the zones at Skukum Creek, such the Rainbow Zone, Kuhn Zone, Raca Zone
and other zones at the deposit. The mineralized vein at Charleston is also of this type.
Mineralized quartz sulphide vein are emplaced along the contact of rhyolite dikes with
surrounding intermediate to felsic intrusive rocks of Mesozoic age. The rhyolite dykes and
mineralized veins are usually associated with shear zones and faults. The veins contain high
grade gold and silver as well as varying amounts of base metals.
Shear zone hosted disseminated sulphide associated gold deposit
Goddell is typical for this deposit type. Mineralization is hosted and controlled by shear zones.
Strongly altered intermediate-felsic dykes and fractured intrusive rocks contain densely
disseminated arsenopyrite and pyrite with which gold is closely associated.
The Becker-Cochran antimony deposit is of the epithermal quartz-sulphide, with stibnite as the
dominating sulphide mineral, vein-type hosted in shear zones. Mineralized veins swell and pinch
out frequently along strike and down-dip. The sheared host rock is strongly altered.
31
9
MINERALIZATION
9.1
Skukum Creek Deposit
Skukum Creek is a structurally controlled, quartz-sulphide vein type, mesothemal polymetalic
gold-silver deposit hosted in Mid-Cretaceous biotite-hornblende granodiorite of the Mt. McNeil
pluton.
The Skukum Creek deposit comprises two principal mineralization zones which are the Rainbow
Zone and the Kuhn-Ridge Zone. Two minor zones are situated between them. They are the
Sterling Zone and the Berg Zone. An additional small zone, called Rainbow-North Zone, is
located close to the north footwall of the Rainbow Zone. The western section of the Rainbow
Zone was historically called Rainbow Two Zone. A separate zone called Raca Zone is located
to the north of the Skukum Creek. Raca has similar mineralization to that of all other zones of
the Skukum Creek deposit, and might be the northeast extension of the Rainbow Zone.
At Skukum Creek, all mineralized zones display similar mineralization and alteration. Gold-silver
mineralization is associated with quartz sulphide veins and vein breccias. Sulphide minerals
include pyrite, chalcopyrite, arsenopyrite, galena, sphalerite, stibnite, tetrahedrite, argentite,
electrum and native gold (Baril and Lang 1989), suggesting a gold-silver dominated polymetal
nature of mineralization. The mineralized veins are mostly associated with rhyolite and andesite
dykes and emplaced along the contacts between dykes and granodiorite wallrock. The veins,
breccias, dykes and anastomosing shears form an integrated package which emplaced along
northeast trending dilational splay faults off the regional Bernie Creek fault-Wheaton River
lineament.
Rainbow Zone
The Rainbow Zone strikes 50°-55°, generally dipping south at more than 70°-80° and locally of
subvertical dip angles. The drill defined strike length is about one kilometer, but the east section
of about 260m long (previously called Rainbow and Road zones) has been most intensely
drilled and is of the most significant importance. Measured plus indicated resources have been
obtained to the elevation of 1050m level (360m below surface). The zone bounds by a rhyodacite dyke (called Portal Dyke) to the East and is open at depth and to the West. Beyond the
Portal Dyke the continuity of the Rainbow Zone is unknown due to thick overburden and lack of
drilling. The west section of 700m long is not well exposed on surface due to talus covers, and
was discovered and drill defined during the underground exploration campaigns implemented by
CME Consulting from 2003 to 2007. Underground drilling incurred mostly about 100m up and
down dip from the 1,300m level. The western section of the zone was also called the Rainbow 2
Zone in CME’s exploration documents (Naas et al. 2003, 2004, 2005, 2007)
Kuhn-Ridge Zone
The Kuhn-Ridge Zone is located to the south of the Rainbow Zone. It is sub-parallel to the
Rainbow Zone with similar dip angle and direction. The total strike length is about one kilometer,
but only the west 600m portion has been drilled. The best drilled part is the middle 200m long
part where it intersects the Sterling and Berg zones where mineralization exhibits zoned
intensity or plunging. The Kuhn-Ridge Zone is open along strike and down dip, but the east
portion has never been sufficiently drill tested and the Kuhn gully is probably its surface
expression. Similar to the Rainbow Zone, it may be cut off by the portal dike to the east.
32
Sterling Zone
The Sterling Zone is a structural step-over connection between the Rainbow Zone and the
Kuhn-Ridge Zone. It strikes NNE and dips east at a steep angle. Its surface expression is a
small gully between the Rainbow Zone and the Kuhn-Ridge zone. The strike length is about
300m, and it merges into the Rainbow Zone and Kuhn-Ridge Zone on either end. Although it
has not been sufficiently drilled at depth, the most highly mineralized portion appears to be
located near surface and close to the intersections with the Rainbow and Kuhn-Ridge Zones.
Berg Zone
The Berg Zone is a new discovery from a 2006 underground exploration drill program and was
further explored in 2007 from the 1,300m level drift. It is also a step-over link between the
Rainbow Zone and Kuhn-Ridge Zone. It strikes ENE, near sub-vertically but dips slightly south.
Along its strike close to the west end intersection with the Rainbow Zone, mineralization
increases.
Rainbow-North Zone
The Rainbow-North Zone is also a newly discovered zone by CME’s underground drill
programs. However, it is not separately named in CME’s exploration reports. The zone is in the
north footwall of and parallel to the Rainbow Zone. The sporadically drilled strike length is about
600m. To the east, it may follow a small gully on surface to the north of the Rainbow Zone
however it has not yet been drill tested. Along its strike, mineralization increases near the west
end intersection with the Rainbow Zone.
Raca Zone
The Raca Zone is a separate mineralization zone to the north of the Skukum Creek and it might
be the east extension of the Rainbow Zone as it is roughly on Rainbow’s strike extension and
displays very similar mineralization. The strike length is unknown as the outcrop is covered by
surface talus and it has not been sufficiently drilled yet. From the information obtained from
limited drilling it is obvious the zone is dipping south at a steep angle.
Although the zone’s resource potential is unknown due to limited drilling, the discovery of the
zone does provide direction to explore for new mineralized zones to the northeast extension
corridor of the Rainbow and Kuhn zones. This corridor covers a strike length of about 2 km,
located to the east limit of the Mt. Skukum Volcanic Complex, and extending from the Skukum
Creek in the south to Chieftain Hill to the north.
33
Figure 9.1
Section 1400E of Skukum Creek
34
9.2
Goddell Deposit
The Goddell deposit is a structurally-controlled, disseminated sulphides-associated gold deposit
hosted in the near east-west trending Goddell Fault Zone.
There are two mineralized zones that were recognized based on completed exploration work up
to this point: the Goddell Gully Zone (GG Zone) and the PD Zone. The GG Zone is sporadically
exposed on surface in the Goddell Gully area with limited amounts of surface drilling
intersecting the zone above the elevation of approximately 1,150m. The PD Zone is mainly
intersected by underground drilling below the elevation of 870m. There is a gap of
approximately 300 vertical metres between the two zones, but they are generally assumed to be
two splays of a single mineralized zone, rather than two separate zones. However, based upon
data review and section re-interpretation, it is recognized that the GG Zone and the PD Zone
may be two separate zones. The two zones strike in roughly the same direction but have
different dip angles. The merge (MG) of the two zones might explain the high grade and several
metre wide intercepts intersected in the PD Zone by underground drilling. The outcrop of the PD
Zone at surface seems to be is obscured by thick surface talus and has not been located on
surface.
The mineralization at Goddell is mainly characterized by abundant disseminated sulphides
contained in intermediate to felsic dykes and breccias within the Goddell fault zone. Rich, fine,
acicular arsenopyrite is the indication of high grade gold. Other sulphides include pyrite, stibnite,
sphalerite and jamesonite. Compared to the PD Zone at greater depths the near surface GG
Zone contains an higher abundance of stibnite pods. Besides the sulphide associated
mineralization, that the gold mineralization is commonly associated with intensely microfractured and argillically altered quartz monzonite with no visible sulphides between multiple
felsic dykes.
Goddell Gully Zone
The zone is also referred to as GG Zone (historically called Black Breccia zone or BB zone). It is
sporadically exposed in the Goddell Gully area. Surface mapping in the Gully area indicates that
mineralization is associated with east-west trending rhyolite dykes hosted in the Goddell fault
and shear system, consisting of sulphides within quartz, barite, calcite and clay gouge. Close to
surface, stibnite pods form the dominant mineralization of the zone (Roger, 1997). Shear
comminuted pyrite imparted a black color to the zone. The zone strikes in a roughly east-west
direction and is sub-vertical, consisting of multiple, discontinuous subparallel veins within a 5075m wide zone of intense shearing, brecciation and alteration cutting quartz monzonite. The
total strike length is unknown due to a limited amount of drilling and poor surface exposure
along strike, but the sporadically exposed portion in the gully area is about 500m. To the West,
the zone is hidden beneath the Wheaton River valley sediments, and to the East up on top of
the plateau it is covered by thick surface talus.
PD Zone
The PD Zone is defined by underground drilling. Historically the surface Golden Task zone (GT
zone) was thought to be the surface extension of the PD zone. However a desk study by NEW
PACIFIC of old data indicates the PD zone is likely a separate zone from the GG zone. The
projected surface outcrop is about 200m to the south of the Goddell fault. It strikes nearly eastwest and is sub-vertical but generally dipping north. The drilled strike length is about 400m. The
35
intersection with the GG zone produced a wide high grade zone (Merge Zone) evidenced by
underground drilling.
Figure 9.2
4375E Section of Goddell
36
9.3
Mt. Skukum Deposit
The Mt. Skukum deposit is a structurally-controlled, high level epithermal quartz-calcite gold
vein deposit, hosted in andesite flows and tuffs of the Mt. Skukum Volcanic Complex of Tertiary
age.
The auriferous quartz calcite veins occur in shears and fault zones along caldera margin and
are associated with collapse of nested calderas (Jago, 1991). The most common gold-bearing
mineral is electrum. The veins contain small amounts of sulphides. Three veins, the Main Cirque
Zone, Lake Zone and Brandy zone were systematically explored with drilling. Mining was only
conducted at the Main Cirque Zone from February 1986 to August 1988. Additionally, there are
a few satellite auriferous veins with insufficient drill exploration near the three veins.
Main Cirque Zone
The Main Cirque Zone strikes 030° to 040° across the valley floor area of the Main Cirque. It is
hosted in an east-dipping, high angle fault zone called the Main Cirque Fault, which is an
average of 10m wide, striking 030° to 040° and dipping 80° east. The ore zone comprises
multiple emplacement, electrum- and native silver-bearing quartz-calcite-sericite veins with
marginal stockwork and gouge zones (Doherty, 1984; McDonald, 1987). The ore zone has
strike length of about 200m and average width of 5m, and was mined over a vertical distance of
80m from an elevation of 1,650m to surface at 1,730m (McDonald et. al., 1988).
Lake Zone
The Lake Zone is located 520m west of the Main Cirque Zone in the west cliff of Main Cirque.
The zone comprises two interconnected veins hosted in gently westwards dipping, propylitic altered, porphyritic andesite and andesitic pyroclastic rocks (McDonald et. al., 1988). The veins
occur as massive, fine-to-coarse grained quartz-calcite-sericite veins, breccias and stockwork.
Drilling indicated two subparallel veins, LV1 and LV2, striking 014° and dipping west, and a
vertical vein trending 020° called LV2-45 (McDonald et. al., 1988). These veins average less
than one m wide but locally are up to a few metres wide and more than 600m along strike.
Brandy Zone
The Brandy Zone is about 360m to the west of the Main Cirque Zone. It comprises a series of
up to six subparallel auriferous quartz-calcite veins striking 014° and dipping to the west at
55° to 70°. These veins occur across a width of 150m and over a strike length of 650m
(McDonald et. al., 1988). The vein minerals consist of quartz, calcite, sericite and visible
electrum. Veins range in width from 0.08m to 2.0m and average 0.2m wide.
37
Figure 9.3
Simplified Geology Plan of the Mt. Skukum Deposit
38
10
EXPLORATION
The present operator, New Pacific, has not completed sufficient exploration work to warrant
discussion in this section. The exploration program of previous operators is discussed in the
history section of this report. A budgeted exploration program is discussed in the
recommendation section of this report.
39
11
DRILLING
There are no current resource or reserve estimates included in this report in which drilling by
New Pacific would be a factor. Below is a historical reference of past operators at Tagish.
11.1 Historical Drilling
Tagish has had exploration drilling activity since the early 1980s. A total of approximately
121,500m of core drilling has been completed from both surface and underground. Most of the
drilling is for exploration and resource definition at Mt. Skukum, Skukum Creek and Goddell.
Detailed descriptions of the underground drill programs at Skukum Creek after 2001 are
included in the annual technical reports prepared for TLG.
Historical drilling prior to 2002 was described in various annual exploration and assessment
reports prepared at different stages by different property owners such as Agip Canada Ltd,
Trumpeter Yukon Gold Ltd (TYG), Omni Resources Inc. (Omni), Mount Skukum Gold Mines
Limited, Total Energold Corp. and Total Erickson Resources Ltd.
On site at the mill and camp, over 20,000m of diamond drill core is stored from previous drilling
programs starting in 1984 at Skukum Creek, Goddell, Chieftain Hill and Mt. Skukum. Some core
is stored near the confluence of Berney Creek and Skukum Creek. Some of the core racks
collapsed due to heavy snow loads during the winters.
40
12
SAMPLING METHOD AND APPROACH
The present operator, New Pacific, has not completed sufficient work on the property to warrant
comment in this section. AMC is aware that a documented protocol is in place for future
exploration programs.
41
13
SAMPLE PREPARATION, ANALYSES AND SECURITY
The present operator, New Pacific, has not completed sufficient exploration work to warrant
discussion of this section. AMC is aware that a documented protocol is in place for future
exploration programs.
42
14
DATA VERIFICATION
The present operator, New Pacific, has not completed sufficient work on the property to warrant
data verification. Summaries of previous operator’s data verification can be found in the history
section of this report.
43
15
ADJACENT PROPERTIES
There are no adjacent properties that have not been discussed in previous sections of this
report.
44
16
MINERAL PROCESSING AND METALLURGICAL TESTING
From 1988 to 2006, various types of mineral processing and metallurgical test work have been
completed on the ore of the Skukum Creek gold-silver deposit. A summary appears below of the
results of historical tests prior to the year 2000 (Table 16.1).
The most recent metallurgical test program was completed by Doug Warkentin, P.Eng.
(Metallurgy) of Cantest Ltd., based in Burnaby, British Columbia (Warkentin, 2006). Tests
included grinding and flotation to produce bulk sulphide concentrates, as well as cyanidation of
the flotation concentrates to determine gold and silver recovery. Additional tests included
cleaner flotation to evaluate possible concentrate quality, and ore characterization tests,
including head assays, acid base accounting for environmental issues, specific gravity and bond
work index determination. Settling tests were also conducted on flotation tailings. Test results
are summarized below:
•
Flotation Recovery: gold 96%, silver and lead 88%, zinc 84%
•
Grade of concentrate: 75g/t Au, 3000 g/t Ag, 7% Pb and 5% Zn.
•
Cyanidation of concentrate: up to 90% for gold and 87% for silver from concentrate.
Although the best results were achieved with the cyanidation of the concentrates, New Pacific is
investigating the economic feasibility of simply producing and shipping flotation concentrate to
smelters.
Table 16.1
Year
Results of Historical Mineral Processing and Metallurgical Tests Prior to
2000
Company Tested by
1988
Omni
1993
Wheaton
1997
BYG
1999
CME
Types of Tests
Results
Bacon, Donaldson and
Grinding, cyanidation,
Associates under the direction
and flotation of a bulk
of Orocon Inc. and Melis
sulphide concentrate.
Engineering Ltd.
Gold recovery 90-98%
Silver recovery 93-98%
Melis Engineering
Bioleaching
gold recovery 92%,
silver recovery 95%
Process Research Associates
Ltd.
Flotation/cyanide
leaching
gold recovery 92%,
silver recovery 95%
Flotation, cyanidation
and pressure oxidation
Flotation recovery 95% of gold
and silver, total recovery after
cyanidation 75% for gold and
72% for silver, increase to 92%
for gold and silver by pressure
oxidation increases
Laurion Consulting Inc.
45
17
MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES
There are no current mineral resources or reserves for Tagish. Historical resources and
reserves are discussed in the history section of this report. New Pacific is not treating the
historical resources and reserves as current.
46
18
OTHER RELEVANT DATA AND INFORMATION
Dewatering is underway at the Goddell portal. Drill stations have been constructed for
underground drilling and a drill program is underway. A surface drill program is underway.
Access roads and drill pads were built to commence surface drilling at Skukum Creek.
Underground drilling is underway at Skukum Creek underground.
New Pacific initiated an Environmental Assessment Study for Tagish.
47
19
INTERPRETATION AND CONCLUSIONS
Exploration activities on Tagish were executed by numerous operators since the early 1980s.
The activities were mostly focused on the three deposits: Mt. Skukum, Skukum Creek and
Goddell. A large amount of exploration information has been generated. The author reviewed
the available reports on the historical work in the preparation of this report. In the author’s
opinion, there is no current resource estimate for Tagish. More exploration work is justifiable
given that the project is at an advanced exploration to pre-development stage. Based on the
results of reviewing historical exploration data, the author reasonably believes Tagish has
further upside potential as an exploration property.
With respect to each known deposit and important mineral showing on the Property, the
following interpretations and conclusions are made by the author of this report.
19.1 Goddell
Goddell is an altered and mineralized shear structure striking roughly E-W from Wheaton River
Valley to Becker Cochran antimony deposit for a strike length of about 6 km. Historical
exploration mostly focused on the Goddell Gully portion which is about 1,000m long on strike.
Old drilling only focused on the PD zone at an area of 400m along strike from section 4200E to
section 4600E and in a vertical extent of 170m from 870m level to 700m level.
Results of data review and sectional study indicate the drill defined area is likely the merge of
the two zones (PD and GG). The merge zone extends down dip and on strike. The merge could
result in increase of both width and intensity (grade) of mineralization and provide prospective
drill targets. The existing decline is about 780m long, providing drill access for underground
drilling for a same strike extent. This area could be the immediate drill target for 2011 drill
campaign.
The entire Goddell structure is of a large, almost of regional scale, size and the Goddell Gully
area is only a small portion. Throughout the whole structure along strike, results of historical
surface geological surveying including chip sampling, soil sampling, mapping and trenching
indicate that epithermal mineralization exists along the structure. The Becker Cochran antimony
occurrence and the gold and mercury soil anomalies in the Horseshoe area which is located
between the Goddell Gully and Becker Cochran, are good indications for epithermal gold
mineralization. However, no sizable ore grade mineralization was located in past exploration.
It is likely that sizable mineralization has not been discovered due to extensive thick talus
covering, or the gold mineralization is controlled by elevation as the case at Goddell, which
means gold mineralization occurs at the elevation of below 900m level. If this is the case, the
Goddell decline should be extended to the East to provide more access for underground drill
testing of the target area below the 900m level, where the “Merge zone” of PD and GG zones
could exist.
In conclusion, the Goddell structure is a very prospective target for exploration as historical
exploration results warrant further work.
48
19.2 Skukum Creek
Skukum Creek is a mesothermal, quartz sulphide, vein-type, gold-silver polymetallic deposit.
Historical exploration focused on the Rainbow-Kuhn zone area to the south of Skukum Creek.
Most drilling was done from the 1,300m level drift on a strike extent of 1,000m by vertical extent
of 700m. Besides the major Rainbow and Kuhn-Ridge zones, there are minor zones such as
Berg Zone, Sterling Zone and Rainbow North Zone. Historical NI 43-101 resource estimates
completed by Roy and Hannon in 2003 and 2007 reported a total of Measured and Indicated
Resources. However, New Pacific is not treating these estimates as current.
Although a total of about 44,000m of drilling had been done in the past, there are still substantial
open areas of each zone to be tested. The down dip extension of all zones beyond 1,000m level
remains untested. The high grade shoots appear to rake to the east. eastwards. Future drilling
should target the “high grade” shoots.
19.3 Raca
Raca Zone stays to the north of the Skukum Creek and on the north east extension of the
Rainbow zone. Mineralization style is identical to that of Rainbow zone. The gold-silver
polymetallic quartz sulphide vein emplaced along the contact of rhyolite dykes with megacrystic
granite.
Only four holes were drilled and all hit the mineralization. The four holes only cover an area of
80m on strike extent by vertical extent of 140m. The drilled area is a very small portion of the
potential Raca mineralized trend which is at least 1.5 km long as indicated by results of surface
rock chip and soil sampling. In addition there are multiple potential mineralized zones
associated with north east trending rhyolite dykes. Chip sample results of Westmont Resources
indicate gold mineralization exists along the dykes but was never drill tested.
It is the author’s conclusion that the Raca trend has the potential of host multiple Rainbow style
mineralization zones.
19.4 Charleston
The mineralization style of the Charleston vein is very similar to that of the mineralized zones at
Skukum Creek. Quartz sulphide veins contain some high grade gold and silver as well as base
metals. Chip sampling along surface outcrop and at underground faces generated very good
values of gold and silver. However the vein was never drill tested due to access difficulty. The
author believes Charleston is a good drill target for future exploration.
19.5 Mt. Skukum
Mt. Skukum witnessed extensive exploration in the 1980s and had two years of commercial gold
production at the Main Cirque vein from 1986 to 1988. Mineralization at Mt. Skukum is high level
epithermal auriferous quartz calcite veins and stockworks hosted in open fractures in Tertiary
andesitic volcanic rocks. Both grade and width of individual veins change dramatically in short
distance of both strike and down dip.
49
The author’s opinion is that Mt. Skukum deserves more exploration and definition drilling. The
current high commodity price will justify more efforts in the area; however, it may not be the top
priority due to access difficulty and erratic nature of mineralization.
19.6 Porter Structure
The Porter structure is about 2 km to the south of and roughly parallel to the Goddell
mineralized zone. It is a strongly altered fault zone of over 100m of width, disturbed by the
emplacement of intermediate to felsic volcanic dykes. Historical exploration focused on the
valley bottom and the north side, including surface soil and rock chip sampling, mapping, a
small amount of aditing and drilling, and generated very promising results of silver and base
metals. To the north of the structure, mineralization is mostly narrow quartz sulphide vein type,
and the existing results are not considered sufficient to warrant any drill testing work. There may
exist a sizable vein type and other types of mineralization under the extensive thick talus
covering, and more geology surveying should be done to define drill test targets.
More interesting is the south side of the valley. A very limited amount of historical soil and rock
chip sampling generated elevated to anomalous values of copper (hundreds ppm up to
1,300 ppm) and molybdenum (tens of ppm up to 300 ppm). A pyritic halo in felsic intrusive rocks
covers an area of 200m by 200m.
In general the author believes there may be potential for porphyry style mineralization in the
area and anticipates that it may occur at depths below the 800m underground levels. This
possibility could be tested and drill targets defined using geophysical surveys.
50
20
RECOMMENDATIONS
The technical team of New Pacific conducted an extensive review and study of the historical
exploration results on Tagish. Based on the results of the review, New Pacific reasonably
believes that there is potential for new mineral resource discoveries on Tagish with further
exploration, and as such has generated a series of priority exploration targets. To test these
targets, various exploration methods will be employed including geological surveying,
geochemical and geophysical surveying as well as diamond drilling. The total budget for these
exploration programs is $16.5 million and was approved by the New Pacific board of directors
on 20 May 2011. The author has reviewed and concurs with the proposed program.
20.1 Geological Surveys
20.1.1
Mapping and Sampling
Although the Skukum project is in a highly advanced stage, there are remaining areas within the
claim boundaries which require further geological investigation. These areas include Carbon
Hill, Charleston Vein/Trend, Skukum Creek deposit-Chieftain Hill corridor, headwater area of the
Skukum Creek, the south extension into the Alunite Cap area of the Lake and Main Cirque
zones as well as their northern extension into the Middle Cirque area.
At Carbon Hill, anomalous results were generated from past prospecting activities in the gully
area where bedrock is well exposed. The results from different historical stages should be
compiled, reviewed and verified by the new programs to generate additional drill targets in
combination and correlation with other exploratory surveys. The Goddell Gully and the Antimony
Creek are areas of high interest.
Rock sampling includes continuous outcrop chip samples, grab samples and float samples as
well as soil sampling.
20.1.2
Trenching
Trenching will be applied where results of former rock and chip sampling and geochemical
anomalies indicate near surface mineralization. Initial machinery-supported trenching will be
perpendicular to the anticipated strike of the mineralization. If a mineralized trend is identified,
excavations will follow the mineralization along strike. The following areas for trenching are:
Charleston vein, Goddell fault, Porter fault, Skukum Creek Deposit-Chieftain Hill corridor and
other areas indicated by geochemical anomalies.
Total material being excavated for trenching over a five-year period is estimated at 10,000m3.
20.1.3
Geochemical Surveys
Geochemical surveys of soil and talus fines will be carried out with special emphasis on (but not
limited to) the Carbon Hill area as the Tertiary Mt. Skukum volcanic rock area was surveyed by
Mt. Skukum Gold Mining during the 1980s. The purpose of the survey is to identify the strike
extent of known mineralized zones such as the Goddell and Porter faults and to locate new
mineralization in areas between them where the geomorphology results in cover of bedrock by
talus and scree.
51
Sampling will be done on 200m spacing grid lines with 20m station intervals. Contour sampling
will be implemented where grid sampling is impeded by steep slopes. The survey grid will be
consistent with geophysical grids. Geochemical surveys will likely be completed following an
airborne geophysical survey as the airborne survey may provide preferential locations for
geochemical surveys. If both geophysical and geochemical surveys produce anomalous results,
drill targets will be determined.
The area immediately south of the Porter structure should be surveyed by contour and grid soil
sampling in due course to confirm if the gossanous area in felsic intrusions has economic
mineralization potential.
20.2 Exploration Program and Budget
For the 2011-2012 period, the following exploration program is recommended, which includes
24,000m of surface drilling and 36,000m of underground drilling (60,000m in total) with a total
estimated expenditures of $16.5 million. The planned expenditures are broken down with the
estimated costs, as follows:
1. Surface infrastructure ($678,000) -- The sum includes expansion of the camp from
25 persons to 50 persons by refurbishing an 11,000 ft2 camp facility already on site, refurbishing
a 5,000 ft2 geological office, core logging facility and repairing some access roads.
2. Equipment ($1.39-million) -- This sum includes the purchase of generators, pumps,
ventilation, electronic, communication and camp office equipment.
3. Surface drilling and geophysics ($4.61 million) -- A total of 24,000m of surface drilling is
planned, of which 5,500m will be at the Raca site. The surface drilling is planned to test in areas
of historical drilling and surface gold anomalies. In addition, several regional gold-silver targets
have been planned for about 18,500m of surface drilling, including the Charleston gold-silver
showing, and a copper-molybdenum anomaly at the Porter alteration structure zone. Concurrent
with this surface drilling, an airborne geophysical survey of 1,000 line kilometres and ground
survey of 40 line kilometres.
4. Underground drilling at Goddell ($4.39 million) -- Dewatering, rehabilitation and new drill
station preparation at Goddell portal. Two underground drill rigs are planned to be utilized to
carry out about 23,000m of underground drilling in approximately 60 holes. The underground
drilling will focus on the area of 1,000m long and 600m down or up dip of the PD zone and the
Merged zone.
5. Skukum Creek underground drilling ($3.12 million) -- At the Skukum Creek site, located at
about 6 km southwest from the Goddell Portal, 13,000m of underground drilling (in about
50 holes) is planned to target depth extensions of four mineralized zones where historical
drilling has only focused on portions of the four mineralized zones and only to about 300m from
the surface.
6. Permitting ($840,000) – New Pacific plans to initiate the environmental assessment study for
the Property, which is required to apply for the Quartz mining licence. It will also carry out a
feasibility study, using an in-house technical team combined with outside consulting firms.
52
7. General operations ($1.44 million) -- These costs are for general operations such as camp
operations, safety measures, and salaries and administration.
Based on the review of the exploration reports, past operator status and existing infrastructure,
the author is of the belief that further exploration on Tagish is warranted. The author agrees
with the exploration budget for Phase 1 presented in Table 1.1 which would collect additional
information on Tagish.
Table 20.1
Summary of the Property Exploration Budget for 2011-2012
Budgeted
Amount $
Measurement
Unit of
Measure
Unit Cost $
Surface construction
New Camp
284,900
10,908
SQFT
26.12
Geology building
262,200
5,200
SQFT
50.42
11,500
900
SQFT
12.81
Road regrading & rebuilding
120,000
24
km
5,000
Subtotal
678,600
claim
408
25
Dry room expansion
Equipment
Mining, Ventilation, Power generators - Goddell
614,800
Mining, Ventilation, Power generators Skukum
385,300
Office and computer equipment - Geology
Environmental equipment
Equipment for general operation
Subtotal
86,400
5,000
305,900
1,397,400
Surface exploration
Reporting & assessment
387,400
Staking & mapping
224,800
551
37,900
1,500
ea
24,000
metre
Sampling
Geophysics
456,800
Surface drilling
3,508,400
Subtotal
4,615,300
146.2
Goddell Underground Exploration
Site preparation
Dewatering
Subtotal
446,500
128,100
16,200,000
3,729,400
23,000
litre
0.01
metre
162.1
91,100
4,395,100
Skukum Underground Exploration
Site preparation
Dewatering
Subtotal
583,000
134,300
19,160,352
2,350,400
13,000
litre
0.01
metre
180.8
59,800
3,127,500
Studies
Environmental Study
266,700
Subtotal
266,700
General operation
53
General operation
Subtotal
Total
Budgeted
Amount $
Measurement
1,399,500
8
Unit of
Measure
month
Unit Cost $
174,938
46,300
1,445,800
15,926,400
Phase 2
Contingent on the program as tabled for Phase 1 being successful in gathering a suitable level
of information on the geology (sufficient to estimate an Indicated Resource), as well as
engineering, legal, operating, economic, social, and environmental factors involved with Tagish.
The author would agree New Pacific’s budget amount for a Feasibility study budget as
presented in Table 1.2.
Table 1.2 Summary of the Phase 2 Property Exploration
Feasibility Study
Budgeted
Amount $
Measurement
Unit of
Measure
Unit Cost $
575,900
54
21
REFERENCES
B.Y.G Natural Resources Inc., 1997. Skukum Creek Property (Rainbow Zone) Feasibility Study
by Normand Lecuyer Enterprise Inc.
Doherty, R.L. and Hart, C.J.R., 1988. Preliminary geology of Fenwick Creek (105D/3) and
Alligator Lake (105D/6) map area. Exploration and Geological Services Division, Yukon Region,
Indian and Northern Affairs Canada, Open File 1988-2 (2maps) 1:50,000 scale.
Freeze, J.C. 1986. Westmount Resources Limited, Geological Report on the Raca Claims 8-11,
Chieftain Hill Property, Whitehorse Mining Division, Assessment Report # 091769.
Hart, C.J.R. and Radloff, J.K., 1990. Geology of the Carcross, Fenwick Creek , Alligator Lake,
Whitehorse and part of Robinson Map area (105D/2,3,6,11 & 7), Yukon. Exploration and
Geological Services Division, Indian and Northern Affairs Canada, Open File 1990-4, 113p.
Jacob, G.K.W., 2011. Quality Control and Quality Assurance Practices for core sampling,
Tagish Lake Gold Corp., in-house procedure paper, April 2011.
Jago, B.C, 1991. the Alunite Cap, a part of the Mount Skukum Property. Wheaton River
Minerals Ltd.
Johnson, T.W. and Jinsheng Fan, 2010. Skukum Project Exploration Report for 2009
Geochemical and Geophysical.
Keyser, J.H., 1989. Summary Report on the Wheaton Gold Property.,
Lang, J. and Rhys, D., 2002. Field and Petrographic Evaluation of Structural Geology, Alteration
and Mineralization in the Skukum Creek Project Area, Yukon Territory, With Recommendations
for Exploration,
Macdonald, A.J. and Z. Rognoni, Z., 1988. Lake Zone Reserves, Mt. Skukum: An Independent
Appraisal.
Macdonald, A.J., 1988. Geological Observations Mount Skukum Gold Mine, unpublished report.
Macdonald, A.J., 1988. Cirque Zone Ore Reserve Mount Skukum Gold Mine, unpublished
report.
McDonald, B.W.R.; Haslinger, R.J.;Zuran, R.J. 1988. Mt Skukum Project, 1988 Exploration.
Unpublished report, Total Energold Corp.-Agip Canada Ltd. Joint Venture 1988.
McDonald, B.W.R.; Haslinger, R.J.; Zuran, R.J. and James, D.R.J., 1990. Mt. Skukum Project,
Exploration 1989. unpublished report. Total Energold Corp.-Agip Canada Ltd. Joint Venture.
Naas, C.O. and Roger R.J., 1999. Data Compilation Report on the Wheaton River Property for
Trumpeter Yukon Gold Inc. CME & Company.
Naas, C.O. and Roger R.J., 2000. Report on the 2000 Summer Work Program at the Skukum
Property, Whitehorse Mining District, Yukon for Trumpeter Yukon Gold Inc. by CME &
Consulting Ltd..
Naas, C.O., 2001. Review of the Skukum Property, Whitehorse Mining District, Yukon Territory
for Tagish Lake Gold Corp. by CME Consulting Ltd.
Naas, C.O. and Roger R.J., 2002. Exploration Program Technical Report Geological,
Geochemical and Diamond Drilling Exploration of the Skukum Property, Whitehorse Mining
District, Yukon Territory, Canada for Tagish Lake Gold Corp. CME Consulting Ltd.
55
Naas, C.O. and Roger R.J., 2003. Technical Report Phase II Geological, Geochemical,
Surveying and Diamond Drilling Exploration of the Skukum Property, Whitehorse Mining District,
Yukon Territory, Canada for Tagish Lake Gold Corp. by CME Consulting Ltd., February 24,
2003
Naas, C.O. and Roger R.J., 2004. Technical Report Phase III Underground Geological Mapping
and Diamond Drilling of the Skukum Creek Deposit, Skukum Property, Whitehorse Mining
District, Yukon Territory, Canada for Tagish Lake Gold Corp. by CME Consulting Ltd., April 27,
2004
Naas, C.O. and Roger R.J., 2004. Technical Report Phase III Geological, Geochemical,
Diamond Drilling and Data Compilation of the Carbon Hill, Skukum Property, Whitehorse Mining
District, Yukon Territory, Canada for Tagish Lake Gold Corp. by CME Consulting Ltd., April 30,
2004
Naas, C.O. and Roger R.J., 2005. Technical Report Phase IV Underground Diamond Drilling of
the Skukum Creek Deposit, Skukum Property, Whitehorse Mining District, Yukon Territory,
Canada for Tagish Lake Gold Corp. by CME Consulting Ltd., October 28, 2005
Naas, C.O. and Roger R.J., 2007. Technical Report Phase V Underground Diamond Drilling of
the Skukum Creek Deposit, Skukum Property, Whitehorse Mining District, Yukon Territory,
Canada for Tagish Lake Gold Corp. by CME Consulting Ltd., July 21, 2007
Roger, R.J., Goddell Gully Mineral Deposits Review of 1996-7 Exploration Program, Omni
Resources Inc., Mount Skukum Mineral Property, Yukon Territory, October 1997
Roger, R. J., 1996. Omni Resource Inc., Wheaton River Mineral Property, Yukon Territory,
Technical Evaluation Report, July 1996
Roger,R.J. 1996. Omni Resource Inc., Wheaton River Mineral Property, Yukon Territory,
Skukum Creek Mineral Deposit, Review of 1996 Exploration Program.
Roy, W.D. and Hannon, P. 2003. Resource Report Tagish Lake Gold Corporation Skukum
Creek and Goddell Gully Deposits.
Roy, W. D. and Hannon, P., 2007. Resource Report Update for the Skukum Property, Wheaton
River, Yukon, Canada.
Tenney,D. 1997. Omni Resources Inc. and Trumpeter Yukon Gold Inc., Skukum Creek Mine,
Yukon Territory, Rainbow Zone Report on Reserves.
Wesa, G.L. and Elliott, T.M., 1999. Geological and Geochemical Report on the Goddell/Carbon
Hill Property (MOM, POP, BERG, TECH, MIL & MB Claims), Whitehorse Mining District, Yukon
Territory, Canada.
56
22
DATE AND SIGNATURE PAGE
CERTIFICATE OF QUALIFIED PERSON
Tagish Lake Gold Property Whitehorse Mining District NI 43 101 Report
for New Pacific Metals Corp.
Date 2 September 2011
Brian F. J. O’Connor, P.Geo.
I, Brian F J O’Connor, P.Geo. as an author of this report entitled “Tagish Lake Gold Property Whitehorse
Mining District NI 43 101 Report”, prepared for New Pacific Metals Corp., dated September 2, 2011, do
hereby certify that:
1.
I am a Consulting Geologist with AMC Mining Consultants (Canada) Ltd. My office address is Suite
1330, 200 Granville Street, Vancouver, British Columbia, Canada V6C 1S4.
2.
I am a graduate of the University of New Brunswick in 1985 with a Bachelor of Science degree in
Geology.
3.
I am a registered member of the Association of Professional Engineers and Geoscientists of BC. I
have continually worked as a geologist for a total of 26 years. My relevant experience for the
purpose of the Technical Report is:
•
•
•
•
•
Twenty-three years of experience as a geologist in mining and exploration environments.
Preparation of numerous reviews and reports on exploration and mining projects in Canada and
around the world.
Chief Geologist with two mining companies in the province of British Columbia.
Senior Geologist with mining and exploration companies in New Brunswick, Quebec, Ontario
and British Columbia.
Over 6 years experience specific to the exploration, evaluation and the mining of narrow vein
deposits.
4.
I have read the definition of "qualified person" set out in National Instrument 43-101 ("NI43-101") and
certify that by reason of my education, affiliation with a professional association (as defined in NI43101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the
purposes of NI43-101.
5.
I visited the Tagish Lake Gold Property 25 July through 28 July 2011.
6.
I am responsible for the preparation of this report, dated 2 September 2011.
7.
I am independent of the Issuer applying the test set out in Section 1.4 of National Instrument 43-101.
8.
I have had no prior involvement with the property that is the subject of the Technical Report.
9.
I have read National Instrument 43-101, and the Technical Report has been prepared in compliance
with National Instrument 43-101 and Form 43-101F1.
10. To the best of my knowledge, information and belief, the Technical Report contains all scientific and
technical information that is required to be disclosed to make the technical report not misleading.
Dated this 2nd day of September, 2011
Signed and Sealed, Brian F J O’Connor
Brian F J O’Connor P. Geo.
Principal Geologist
57
APPENDIX A
MINERAL TENURE
58
Grant
Number
Reg
Type
Claim
Name
YB07446
Quartz
BERG
YB07447
Quartz
YB07448
YB07449
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
1
Tagish Lake Gold Corp. - 100%
Active
YB67217
Quartz
MIL
BERG
2
Active
YB67218
Quartz
Quartz
BERG
3
Active
YB67219
Quartz
BERG
4
Active
YB67220
YB07450
Quartz
BERG
5
Active
YB07451
Quartz
BERG
6
YB07452
Quartz
BERG
7
YB07453
Quartz
BERG
8
YB07454
Quartz
BERG
YB07455
Quartz
YB07456
Quartz
YB07457
Claim
Owner
Status
52
Active
MIL
53
Active
Quartz
MIL
54
Active
Quartz
MIL
55
Active
YB67221
Quartz
MIL
56
Active
Active
YB67222
Quartz
MIL
57
Active
Active
YB67223
Quartz
MIL
58
Active
Active
YB67224
Quartz
MIL
59
Active
9
Active
YB67225
Quartz
MIL
60
Active
BERG
10
Active
YB67226
Quartz
MIL
61
Active
BERG
11
Active
YB67227
Quartz
MIL
62
Active
Quartz
BERG
12
Active
YB67228
Quartz
MIL
63
Active
YB07460
Quartz
BERG
15
Active
YB67229
Quartz
MIL
64
Active
YB07461
Quartz
BERG
16
Active
YB67230
Quartz
MIL
65
Active
YB07466
Quartz
BERG
21
Active
YB67231
Quartz
MIL
66
Active
YB07467
Quartz
BERG
22
Active
YB67232
Quartz
MIL
67
Active
YB07474
Quartz
BERG
29
Active
YB67233
Quartz
MIL
68
Active
YB07475
Quartz
BERG
30
Active
YB67234
Quartz
MIL
69
Active
YB07476
Quartz
BERG
31
Active
YA81767
Quartz
MOM
1
Active
YB07477
Quartz
BERG
32
Active
YA81768
Quartz
MOM
2
Active
YB07478
Quartz
BERG
33
Active
YA81769
Quartz
MOM
3
Active
YB07479
Quartz
BERG
34
Active
YA81770
Quartz
MOM
4
Active
YB07480
Quartz
BERG
35
Active
YA81771
Quartz
MOM
5
Active
YB07481
Quartz
BERG
36
Active
YA81772
Quartz
MOM
6
Active
YB07482
Quartz
BERG
37
Active
YA81773
Quartz
MOM
7
Active
YB07483
Quartz
BERG
38
Active
YA81774
Quartz
MOM
8
Active
YB07484
Quartz
BERG
39
Active
YA81775
Quartz
MOM
9
Active
YB07485
Quartz
BERG
40
Active
YA81776
Quartz
MOM
10
Active
YB07486
Quartz
BERG
41
Active
YA81781
Quartz
MOM
15
Active
YB07487
Quartz
BERG
42
Active
YA81782
Quartz
MOM
16
Active
YB07488
Quartz
BERG
43
Active
YA81783
Quartz
MOM
17
Active
YB07489
Quartz
BERG
44
Active
YA81784
Quartz
MOM
18
Active
YB07490
Quartz
BERG
45
Active
YA81785
Quartz
MOM
19
Active
YB07499
Quartz
BERG
54
Active
YA81786
Quartz
MOM
20
Active
YB07501
Quartz
BERG
56
Active
YA81787
Quartz
MOM
21
Active
YB07503
Quartz
BERG
58
Active
YA81788
Quartz
MOM
22
Active
YB07505
Quartz
BERG
60
Active
YA81789
Quartz
MOM
23
Active
YB07507
Quartz
BERG
62
Active
YA81790
Quartz
MOM
24
Active
YB07509
Quartz
BERG
64
Active
YA81791
Quartz
MOM
25
Active
YB07511
Quartz
BERG
66
Active
YA81792
Quartz
MOM
26
Active
YB07513
Quartz
BERG
68
Active
YA81793
Quartz
MOM
27
Active
AMC : 711039 - Appendix A : Mineral Tenure
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YB07517
Quartz
BERG
YB07519
Quartz
YB07521
YB07523
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
72
Active
YA81795
Quartz
MOM
BERG
74
Active
YA81796
Quartz
Quartz
BERG
76
Active
YA81797
Quartz
BERG
78
Active
YA81798
YB07525
Quartz
BERG
80
Active
YB07527
Quartz
BERG
82
YB07529
Quartz
BERG
84
YB07531
Quartz
BERG
86
YB07533
Quartz
BERG
YB07535
Quartz
YB07537
Quartz
YB07539
Claim
Number
Claim
Owner
Status
29
Active
MOM
30
Active
Quartz
MOM
31
Active
Quartz
MOM
32
Active
YA81799
Quartz
MOM
33
Active
Active
YA81800
Quartz
MOM
34
Active
Active
YA81801
Quartz
MOM
35
Active
Active
YA81802
Quartz
MOM
36
Active
88
Active
YA81803
Quartz
MOM
37
Active
BERG
90
Active
YA81804
Quartz
MOM
38
Active
BERG
92
Active
YA81805
Quartz
MOM
39
Active
Quartz
BERG
94
Active
YA81806
Quartz
MOM
40
Active
YB07540
Quartz
BERG
95
Active
YA81807
Quartz
MOM
41
Active
YB07597
Quartz
BERG
152
Active
YA81808
Quartz
MOM
42
Active
YB07598
Quartz
BERG
153
Active
YA81809
Quartz
MOM
43
Active
YB07599
Quartz
BERG
154
Active
YA81810
Quartz
MOM
44
Active
YB07601
Quartz
BERG
156
Active
YA81813
Quartz
MOM
47
Active
YB07602
Quartz
BERG
157
Active
YA81814
Quartz
MOM
48
Active
YB07603
Quartz
BERG
158
Active
YA81815
Quartz
MOM
49
Active
YB07604
Quartz
BERG
159
Active
YA81816
Quartz
MOM
50
Active
YB07605
Quartz
BERG
160
Active
YA81817
Quartz
MOM
51
Active
YC18781
Quartz
CHAR
1
Active
YA81818
Quartz
MOM
52
Active
YC18782
Quartz
CHAR
2
Active
YA81819
Quartz
MOM
53
Active
YC18783
Quartz
CHAR
3
Active
YA81820
Quartz
MOM
54
Active
YC18784
Quartz
CHAR
4
Active
YA81821
Quartz
MOM
55
Active
YC18785
Quartz
CHAR
5
Active
YA81822
Quartz
MOM
56
Active
YC18786
Quartz
CHAR
6
Active
YA81823
Quartz
MOM
57
Active
YC18787
Quartz
CHAR
7
Active
YA81824
Quartz
MOM
58
Active
YC18788
Quartz
CHAR
8
Active
YA81825
Quartz
MOM
59
Active
YC18789
Quartz
CHAR
9
Active
YA81826
Quartz
MOM
60
Active
YC18790
Quartz
CHAR
10
Active
YA81828
Quartz
MOM
62
Active
YC18791
Quartz
CHAR
11
Active
YA81829
Quartz
MOM
63
Active
YC18792
Quartz
CHAR
12
Active
YA81830
Quartz
MOM
64
Active
YC18793
Quartz
CHAR
13
Active
YA81831
Quartz
MOM
65
Active
YC18794
Quartz
CHAR
14
Active
YA81832
Quartz
MOM
66
Active
YC18795
Quartz
CHAR
15
Active
YA81833
Quartz
MOM
67
Active
YC18796
Quartz
CHAR
16
Active
YA81834
Quartz
MOM
68
Active
YC18797
Quartz
CHAR
17
Active
YA81835
Quartz
MOM
69
Active
YC18798
Quartz
CHAR
18
Active
YA81836
Quartz
MOM
70
Active
YC18799
Quartz
CHAR
19
Active
YA81837
Quartz
MOM
71
Active
Grant
Number
Reg
Type
Claim
Name
YC18800
Quartz
CHAR
YC18801
Quartz
YC18802
YC18803
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Owner
Status
20
Active
YA81838
Quartz
MOM
72
Active
CHAR
21
Active
YA81839
Quartz
MOM
73
Active
Quartz
CHAR
22
Active
YA81840
Quartz
CHAR
23
Active
YA81841
Quartz
MOM
74
Active
Quartz
MOM
75
Active
YC18804
Quartz
CHAR
24
Active
YA81842
Quartz
MOM
76
Active
YC18805
Quartz
CHAR
25
Active
YA81843
Quartz
MOM
77
Active
YC18806
Quartz
CHAR
26
YC18807
Quartz
CHAR
27
Active
YA81844
Quartz
MOM
78
Active
Active
YA81845
Quartz
MOM
79
Active
YC18808
Quartz
CHAR
28
Active
YA81846
Quartz
MOM
80
Active
YC18809
Quartz
YC18810
Quartz
CHAR
29
Active
YA81847
Quartz
MOM
81
Active
CHAR
30
Active
YA82000
Quartz
MOM
82
Active
YC18811
Quartz
CHAR
31
Active
YA82001
Quartz
MOM
83
Active
YC18812
Quartz
CHAR
32
Active
YA82002
Quartz
MOM
84
Active
YC18813
Quartz
CHAR
33
Active
YA82003
Quartz
MOM
85
Active
YC18814
Quartz
CHAR
34
Active
YA82004
Quartz
MOM
86
Active
YC18815
Quartz
CHAR
35
Active
YA82005
Quartz
MOM
87
Active
YC18816
Quartz
CHAR
36
Active
YA82006
Quartz
MOM
88
Active
YC18817
Quartz
CHAR
37
Active
YA82007
Quartz
MOM
89
Active
YC18818
Quartz
CHAR
38
Active
YA93743
Quartz
OMNI
1
Active
YC18819
Quartz
CHAR
39
Active
YA93744
Quartz
OMNI
2
Active
YC18820
Quartz
CHAR
40
Active
YA93745
Quartz
OMNI
3
Active
YC18821
Quartz
CHAR
41
Active
YA93746
Quartz
OMNI
4
Active
YC18822
Quartz
CHAR
42
Active
YA93747
Quartz
OMNI
5
Active
YC18823
Quartz
CHAR
43
Active
YA93748
Quartz
OMNI
6
Active
YC19347
Quartz
CHAR
44
Active
YA93749
Quartz
OMNI
7
Active
YC19348
Quartz
CHAR
45
Active
YA93750
Quartz
OMNI
8
Active
YC19349
Quartz
CHAR
46
Active
YA93751
Quartz
OMNI
9
Active
YC19350
Quartz
CHAR
47
Active
YA93752
Quartz
OMNI
10
Active
YC19351
Quartz
CHAR
48
Active
YA93753
Quartz
OMNI
11
Active
YC19352
Quartz
CHAR
49
Active
YA93754
Quartz
OMNI
12
Active
YC19353
Quartz
CHAR
50
Active
Y 75415
Quartz
POP
1
Active
YC19354
Quartz
CHAR
51
Active
Y 75416
Quartz
POP
2
Active
YC19355
Quartz
CHAR
52
Active
Y 75417
Quartz
POP
3
Active
YA74385
Quartz
CHIEF
2
Active
Y 75418
Quartz
POP
4
Active
YA74395
Quartz
CHIEF
12
Active
Y 75419
Quartz
POP
5
Active
YA74396
Quartz
CHIEF
13
Active
Y 75420
Quartz
POP
6
Active
YA74397
Quartz
CHIEF
14
Active
Y 75421
Quartz
POP
7
Active
YA74398
Quartz
CHIEF
15
Active
Y 75422
Quartz
POP
8
Active
YA74399
Quartz
CHIEF
16
Active
Y 75423
Quartz
POP
9
Active
YA74400
Quartz
CHIEF
17
Active
Y 75424
Quartz
POP
10
Active
YA74401
Quartz
CHIEF
18
Active
Y 75425
Quartz
POP
11
Active
Claim
Name
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YA74402
Quartz
CHIEF
YA74403
Quartz
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
19
Active
Y 75426
Quartz
POP
CHIEF
20
Active
Y 75427
Quartz
POP
Claim
Number
Claim
Owner
Status
12
Active
13
Active
YA74404
Quartz
CHIEF
21
Active
Y 75428
Quartz
POP
14
Active
YA74405
Quartz
CHIEF
22
Active
YA81468
Quartz
POP
15
Active
YA74406
Quartz
CHIEF
23
Active
YA81469
Quartz
POP
16
Active
YA74407
Quartz
CHIEF
24
Active
YA81470
Quartz
POP
17
Active
YA74408
Quartz
CHIEF
25
Active
YA81471
Quartz
POP
18
Active
YA74409
Quartz
CHIEF
26
Active
YA81472
Quartz
POP
19
Active
YA74410
Quartz
CHIEF
27
Active
YA81473
Quartz
POP
20
Active
YA74415
Quartz
CHIEF
32
Active
YA81474
Quartz
POP
21
Active
YA74416
Quartz
CHIEF
33
Active
YA81475
Quartz
POP
22
Active
YA74417
Quartz
CHIEF
34
Active
YA81476
Quartz
POP
23
Active
YA74418
Quartz
CHIEF
35
Active
YA81477
Quartz
POP
24
Active
YA74419
Quartz
CHIEF
36
Active
YA81478
Quartz
POP
25
Active
YA74420
Quartz
CHIEF
37
Active
YA81479
Quartz
POP
26
Active
YA74421
Quartz
CHIEF
38
Active
YA81480
Quartz
POP
27
Active
YA74422
Quartz
CHIEF
39
Active
YA81481
Quartz
POP
28
Active
YA74423
Quartz
CHIEF
40
Active
YA81482
Quartz
POP
29
Active
YA74424
Quartz
CHIEF
41
Active
YA81483
Quartz
POP
30
Active
YA74425
Quartz
CHIEF
42
Active
YA81484
Quartz
POP
31
Active
YA74426
Quartz
CHIEF
43
Active
YA81485
Quartz
POP
32
Active
YA74427
Quartz
CHIEF
44
Active
YA81486
Quartz
POP
33
Active
YA74428
Quartz
CHIEF
45
Active
YA81487
Quartz
POP
34
Active
YA74429
Quartz
CHIEF
46
Active
YA81488
Quartz
POP
35
Active
YA74430
Quartz
CHIEF
47
Active
YA81489
Quartz
POP
36
Active
YA74431
Quartz
CHIEF
48
Active
YA81490
Quartz
POP
37
Active
YA74432
Quartz
CHIEF
49
Active
YA81491
Quartz
POP
38
Active
YA74435
Quartz
CHIEF
52
Active
YA81492
Quartz
POP
39
Active
YA74436
Quartz
CHIEF
53
Active
YA81493
Quartz
POP
40
Active
YA74437
Quartz
CHIEF
54
Active
YA81494
Quartz
POP
41
Active
YA74438
Quartz
CHIEF
55
Active
YA81495
Quartz
POP
42
Active
YA74439
Quartz
CHIEF
56
Active
YA81496
Quartz
POP
43
Active
YA74440
Quartz
CHIEF
57
Active
YA81497
Quartz
POP
44
Active
YA74441
Quartz
CHIEF
58
Active
YA81498
Quartz
POP
45
Active
YA74442
Quartz
CHIEF
59
Active
YA81499
Quartz
POP
46
Active
YA74443
Quartz
CHIEF
60
Active
YA81500
Quartz
POP
47
Active
YA74444
Quartz
CHIEF
61
Active
YA81501
Quartz
POP
48
Active
YA74445
Quartz
CHIEF
62
Active
YA81502
Quartz
POP
49
Active
YA74446
Quartz
CHIEF
63
Active
YA81503
Quartz
POP
50
Active
YA74447
Quartz
CHIEF
64
Active
YA81504
Quartz
POP
51
Active
YA74448
Quartz
CHIEF
65
Active
YA81505
Quartz
POP
52
Active
Grant
Number
Reg
Type
Claim
Name
YA74449
Quartz
CHIEF
YA74450
Quartz
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
66
Active
YA81506
Quartz
POP
CHIEF
67
Active
YA81507
Quartz
POP
Claim
Number
Claim
Owner
Status
53
Active
54
Active
YA74451
Quartz
CHIEF
68
Active
YA81508
Quartz
POP
55
Active
YC14135
Quartz
CL
6
Active
YA81509
Quartz
POP
56
Active
YC14136
Quartz
CL
7
Active
YA81510
Quartz
POP
57
Active
YC14137
Quartz
CL
8
Active
YA81511
Quartz
POP
58
Active
YC14138
Quartz
CL
9
Active
YA81512
Quartz
POP
59
Active
YC14139
Quartz
CL
10
Active
YA81513
Quartz
POP
60
Active
YC14140
Quartz
CL
13
Active
YA81514
Quartz
POP
61
Active
YC14141
Quartz
CL
14
Active
YA81515
Quartz
POP
62
Active
YC14142
Quartz
CL
15
Active
YA81516
Quartz
POP
63
Active
YC14143
Quartz
CL
16
Active
YA81517
Quartz
POP
64
Active
YC14144
Quartz
CL
17
Active
YA81518
Quartz
POP
65
Active
YC14145
Quartz
CL
18
Active
YA81519
Quartz
POP
66
Active
YC14148
Quartz
CL
21
Active
YA81520
Quartz
POP
67
Active
YC14149
Quartz
CL
22
Active
YA81521
Quartz
POP
68
Active
YC14150
Quartz
CL
23
Active
YA81522
Quartz
POP
69
Active
YC14151
Quartz
CL
24
Active
YA81523
Quartz
POP
70
Active
YC14152
Quartz
CL
25
Active
YA86194
Quartz
POP
71
Active
YC14156
Quartz
CL
29
Active
YA86195
Quartz
POP
72
Active
YC14157
Quartz
CL
30
Active
YA86196
Quartz
POP
73
Active
YB66982
Quartz
DG
1
Active
YA86197
Quartz
POP
74
Active
YB66983
Quartz
DG
2
Active
YA86198
Quartz
POP
75
Active
YB66984
Quartz
DG
3
Active
YA86199
Quartz
POP
76
Active
YB66985
Quartz
DG
4
Active
YA86200
Quartz
POP
77
Active
YB66986
Quartz
DG
5
Active
YA86201
Quartz
POP
78
Active
YB66987
Quartz
DG
6
Active
YA86202
Quartz
POP
79
Active
YB66988
Quartz
DG
7
Active
YA86203
Quartz
POP
80
Active
YB66989
Quartz
DG
8
Active
YA86204
Quartz
POP
81
Active
YB66990
Quartz
DG
9
Active
YA86205
Quartz
POP
82
Active
YB66991
Quartz
DG
10
Active
YA86206
Quartz
POP
83
Active
YB66992
Quartz
DG
11
Active
YA86207
Quartz
POP
84
Active
YB66993
Quartz
DG
12
Active
YA86208
Quartz
POP
85
Active
YB66994
Quartz
DG
13
Active
YA86209
Quartz
POP
86
Active
YB66995
Quartz
DG
14
Active
YA86210
Quartz
POP
87
Active
YB66996
Quartz
DG
15
Active
YA86211
Quartz
POP
88
Active
YB66997
Quartz
DG
16
Active
YA86212
Quartz
POP
89
Active
YB66998
Quartz
DG
17
Active
YA86213
Quartz
POP
90
Active
YB66999
Quartz
DG
18
Active
YA86214
Quartz
POP
91
Active
YB67000
Quartz
DG
19
Active
YA86215
Quartz
POP
92
Active
YB67001
Quartz
DG
20
Active
YA86216
Quartz
POP
93
Active
Grant
Number
Reg
Type
Claim
Name
YB67002
Quartz
DG
YB67003
Quartz
YA81543
YA81544
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
21
Active
YA86217
Quartz
POP
DG
22
Active
YA86218
Quartz
Quartz
ERN
1
Active
YA86219
Quartz
ERN
2
Active
YA86220
YA81545
Quartz
ERN
3
Active
YA81546
Quartz
ERN
4
YA81547
Quartz
ERN
5
YA81548
Quartz
ERN
6
YA81549
Quartz
ERN
YA81550
Quartz
YA81551
Quartz
YA81552
Claim
Number
Claim
Owner
Status
94
Active
POP
95
Active
Quartz
POP
96
Active
Quartz
POP
97
Active
YA86221
Quartz
POP
98
Active
Active
YA86222
Quartz
POP
99
Active
Active
YA86223
Quartz
POP
100
Active
Active
YA93378
Quartz
POP
101
Active
7
Active
YA86224
Quartz
POP
101
Active
ERN
8
Active
YA93379
Quartz
POP
102
Active
ERN
9
Active
YA86225
Quartz
POP
102
Active
Quartz
ERN
10
Active
YA86226
Quartz
POP
103
Active
YA81553
Quartz
ERN
11
Active
YA93382
Quartz
POP
103
Active
YA81554
Quartz
ERN
12
Active
YA86227
Quartz
POP
104
Active
YA81555
Quartz
ERN
13
Active
YA93383
Quartz
POP
104
Active
YA81556
Quartz
ERN
14
Active
YA93384
Quartz
POP
105
Active
YA81557
Quartz
ERN
15
Active
YA93385
Quartz
POP
106
Active
YA85503
Quartz
ERN
16
Active
YA93386
Quartz
POP
107
Active
YA85504
Quartz
ERN
17
Active
YA93387
Quartz
POP
108
Active
YA85505
Quartz
ERN
18
Active
YA93388
Quartz
POP
109
Active
YA85506
Quartz
ERN
19
Active
YA93389
Quartz
POP
110
Active
YA85507
Quartz
ERN
20
Active
YA93390
Quartz
POP
111
Active
YA85508
Quartz
ERN
21
Active
YA93391
Quartz
POP
112
Active
YA85509
Quartz
ERN
22
Active
YA93392
Quartz
POP
113
Active
YA85511
Quartz
ERN
24
Active
YA93393
Quartz
POP
114
Active
YA85512
Quartz
ERN
25
Active
YA93394
Quartz
POP
115
Active
YA85513
Quartz
ERN
26
Active
YA93395
Quartz
POP
116
Active
YA85514
Quartz
ERN
27
Active
YA94672
Quartz
POP
117
Active
YA85515
Quartz
ERN
30
Active
YA94673
Quartz
POP
118
Active
YA85516
Quartz
ERN
31
Active
YA94674
Quartz
POP
119
Active
YA85517
Quartz
ERN
32
Active
YA94675
Quartz
POP
120
Active
YA85518
Quartz
ERN
33
Active
YA94676
Quartz
POP
121
Active
YA93875
Quartz
GLEE
1
Active
YA94677
Quartz
POP
122
Active
YA93876
Quartz
GLEE
2
Active
YB97801
Quartz
PUP
29
Active
YA93877
Quartz
GLEE
3
Active
YB97802
Quartz
PUP
30
Active
YA93878
Quartz
GLEE
4
Active
YA78390
Quartz
PUP
RAC
85
Active
YA93879
Quartz
GLEE
5
Active
Y 60275
Quartz
A
8
Active
YA93880
Quartz
GLEE
6
Active
Y 60276
Quartz
A
9
Active
10
Active
11
Active
1
Active
RAC
RAC
YA93881
Quartz
GLEE
7
Active
Y 60277
Quartz
A
YA93882
Quartz
GLEE
8
Active
Y 60278
Quartz
A
YA93883
Quartz
GLEE
9
Active
YA92922
Quartz
RAC
STEN
Grant
Number
Reg
Type
Claim
Name
YA93884
Quartz
GLEE
YA93885
Quartz
YA93886
YA93890
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Owner
Status
10
Active
YA92923
Quartz
STEN
2
Active
GLEE
11
Active
YA92924
Quartz
STEN
3
Active
Quartz
GLEE
12
Active
YA92925
Quartz
GLEE
16
Active
YA92926
Quartz
STEN
4
Active
Quartz
STEN
5
Active
YA93891
Quartz
GLEE
17
Active
YA92927
Quartz
STEN
6
Active
YA93892
Quartz
GLEE
18
Active
YA92928
Quartz
STEN
7
Active
YA93893
Quartz
GLEE
19
YA93894
Quartz
GLEE
20
Active
YA92929
Quartz
STEN
8
Active
Active
YA92930
Quartz
STEN
9
Active
YA93896
Quartz
GLEE
22
Active
YA92931
Quartz
STEN
10
Active
YA93911
Quartz
YA93912
Quartz
GLEE
37
Active
YA92932
Quartz
STEN
11
Active
GLEE
38
Active
YA92933
Quartz
STEN
12
Active
YA93913
Quartz
GLEE
39
Active
YA92934
Quartz
STEN
13
Active
YA93914
Quartz
GLEE
40
Active
YA92935
Quartz
STEN
14
Active
YA93915
Quartz
GLEE
41
Active
YA92936
Quartz
STEN
15
Active
YA93916
Quartz
GLEE
42
Active
YA92937
Quartz
STEN
16
Active
YA93917
Quartz
GLEE
43
Active
YA92938
Quartz
STEN
17
Active
YA93918
Quartz
GLEE
44
Active
YA92940
Quartz
STEN
19
Active
YA93919
Quartz
GLEE
45
Active
YA92941
Quartz
STEN
20
Active
YA93920
Quartz
GLEE
46
Active
YA92942
Quartz
STEN
21
Active
YA93993
Quartz
GLEE
59
Active
YA92943
Quartz
STEN
22
Active
YA93994
Quartz
GLEE
60
Active
YA92944
Quartz
STEN
23
Active
YA93995
Quartz
GLEE
61
Active
YA92945
Quartz
STEN
24
Active
YA93996
Quartz
GLEE
62
Active
YA92946
Quartz
STEN
25
Active
YA93997
Quartz
GLEE
63
Active
YA92947
Quartz
STEN
26
Active
YA93998
Quartz
GLEE
64
Active
YA92948
Quartz
STEN
27
Active
YA93999
Quartz
GLEE
65
Active
YA92949
Quartz
STEN
28
Active
YA94000
Quartz
GLEE
66
Active
YA92950
Quartz
STEN
29
Active
YA94001
Quartz
GLEE
67
Active
YA92951
Quartz
STEN
30
Active
YA94002
Quartz
GLEE
68
Active
YA92952
Quartz
STEN
31
Active
YA94003
Quartz
GLEE
69
Active
YA92953
Quartz
STEN
32
Active
YA94004
Quartz
GLEE
70
Active
YA92954
Quartz
STEN
33
Active
YA94005
Quartz
GLEE
71
Active
YA92955
Quartz
STEN
34
Active
YA94006
Quartz
GLEE
72
Active
YA92956
Quartz
STEN
35
Active
YA94007
Quartz
GLEE
73
Active
YA92957
Quartz
STEN
36
Active
YA94008
Quartz
GLEE
74
Active
YA92958
Quartz
STEN
37
Active
YA94009
Quartz
GLEE
75
Active
YA92959
Quartz
STEN
38
Active
YA94010
Quartz
GLEE
76
Active
YA92960
Quartz
STEN
39
Active
YA94011
Quartz
GLEE
77
Active
YA92961
Quartz
STEN
40
Active
YA94012
Quartz
GLEE
78
Active
YA92962
Quartz
STEN
41
Active
YA94013
Quartz
GLEE
79
Active
YA92963
Quartz
STEN
42
Active
YA94014
Quartz
GLEE
80
Active
YA92964
Quartz
STEN
43
Active
Claim
Name
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YB95941
Quartz
HO
YB95942
Quartz
YB95943
YB95944
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Owner
Status
1
Active
YA92965
Quartz
STEN
44
Active
HO
2
Active
YA92966
Quartz
STEN
45
Active
Quartz
HO
3
Active
YA82362
Quartz
HO
4
Active
YA82363
Quartz
TECH
1
Active
Quartz
TECH
2
Active
YB95945
Quartz
HO
5
Active
YA82364
Quartz
TECH
3
Active
YB95946
Quartz
HO
6
Active
YA82365
Quartz
TECH
4
Active
YB95947
Quartz
HO
7
YB95948
Quartz
HO
8
Active
YB97764
Quartz
TECH
5
Active
Active
YB26465
Quartz
TECH
6
Active
YB95949
Quartz
HO
9
Active
YA82368
Quartz
TECH
7
Active
YB95950
Quartz
YB95951
Quartz
HO
10
Active
YA82369
Quartz
TECH
8
Active
HO
11
Active
YA82370
Quartz
TECH
9
Active
YB95952
Quartz
HO
12
Active
YA82371
Quartz
TECH
10
Active
YB95953
Quartz
HO
13
Active
YA82372
Quartz
TECH
11
Active
YB95954
Quartz
HO
14
Active
YA82373
Quartz
TECH
12
Active
YB95955
Quartz
HO
15
Active
YA82374
Quartz
TECH
13
Active
YB95956
Quartz
HO
16
Active
YB97763
Quartz
TECH
14
Active
YB95957
Quartz
HO
17
Active
YA82376
Quartz
TECH
15
Active
YB95958
Quartz
HO
18
Active
YA82377
Quartz
TECH
16
Active
YB95959
Quartz
HO
19
Active
YA82378
Quartz
TECH
17
Active
YB95960
Quartz
HO
20
Active
YA82379
Quartz
TECH
18
Active
YB95961
Quartz
HO
21
Active
YA86013
Quartz
TECH
19
Active
YB95962
Quartz
HO
22
Active
YA86014
Quartz
TECH
20
Active
YB95963
Quartz
HO
23
Active
YA86015
Quartz
TECH
21
Active
YB95964
Quartz
HO
24
Active
YA92145
Quartz
TECH
22
Active
YB95965
Quartz
HO
25
Active
YA92146
Quartz
TECH
23
Active
YB95966
Quartz
HO
26
Active
YA92147
Quartz
TECH
24
Active
YB95967
Quartz
HO
27
Active
YA92148
Quartz
TECH
25
Active
YB95968
Quartz
HO
28
Active
YA92149
Quartz
TECH
26
Active
YB95969
Quartz
HO
29
Active
YA92150
Quartz
TECH
27
Active
YB95970
Quartz
HO
30
Active
YA92151
Quartz
TECH
28
Active
YA92967
Quartz
KIR
1
Active
YA92152
Quartz
TECH
29
Active
YA92968
Quartz
KIR
2
Active
YA92153
Quartz
TECH
30
Active
YA92969
Quartz
KIR
3
Active
YA92154
Quartz
TECH
31
Active
YA92970
Quartz
KIR
4
Active
YA92155
Quartz
TECH
32
Active
YA92971
Quartz
KIR
5
Active
YA92156
Quartz
TECH
33
Active
YA92972
Quartz
KIR
6
Active
YA92157
Quartz
TECH
34
Active
YA92973
Quartz
KIR
7
Active
YA92158
Quartz
TECH
35
Active
YA92974
Quartz
KIR
8
Active
YA92159
Quartz
TECH
36
Active
YA92975
Quartz
KIR
9
Active
YA92160
Quartz
TECH
37
Active
YA92976
Quartz
KIR
10
Active
YA92161
Quartz
TECH
38
Active
YA92977
Quartz
KIR
11
Active
YA92162
Quartz
TECH
39
Active
Claim
Name
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YA92978
Quartz
KIR
YA92979
Quartz
YA92980
YA92981
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Owner
Status
12
Active
YA92163
Quartz
TECH
40
Active
KIR
13
Active
YA92833
Quartz
TEX
1
Active
Quartz
KIR
14
Active
YA92834
Quartz
KIR
15
Active
YA92835
Quartz
TEX
2
Active
Quartz
TEX
3
Active
YA92982
Quartz
KIR
16
Active
YA92836
Quartz
TEX
4
Active
YA92983
Quartz
KIR
17
Active
YA92837
Quartz
TEX
5
Active
YA92984
Quartz
KIR
18
YA92985
Quartz
KIR
19
Active
YA92838
Quartz
TEX
6
Active
Active
YA92839
Quartz
TEX
7
Active
YA92986
Quartz
KIR
20
Active
YA92840
Quartz
TEX
8
Active
YA92987
Quartz
YA92988
Quartz
KIR
21
Active
YA92841
Quartz
TEX
9
Active
KIR
22
Active
YA92842
Quartz
TEX
10
Active
YA92989
Quartz
KIR
23
Active
YA92843
Quartz
TEX
11
Active
YA92990
Quartz
KIR
24
Active
YA92844
Quartz
TEX
12
Active
YA92991
Quartz
KIR
25
Active
YA92845
Quartz
TEX
13
Active
YA92992
Quartz
KIR
26
Active
YA92846
Quartz
TEX
14
Active
YA92993
Quartz
KIR
27
Active
YA92847
Quartz
TEX
15
Active
YA92994
Quartz
KIR
28
Active
YA92848
Quartz
TEX
16
Active
YA92995
Quartz
KIR
29
Active
YA92849
Quartz
TEX
17
Active
YA92996
Quartz
KIR
30
Active
YA92850
Quartz
TEX
18
Active
YA92997
Quartz
KIR
31
Active
YA92851
Quartz
TEX
19
Active
YA92998
Quartz
KIR
32
Active
YA92852
Quartz
TEX
20
Active
YA92999
Quartz
KIR
33
Active
YA92853
Quartz
TEX
21
Active
YA61199
Quartz
KUKU
1
Active
YA92854
Quartz
TEX
22
Active
YA61200
Quartz
KUKU
2
Active
YB66866
Quartz
TM
1
Active
YA61201
Quartz
KUKU
3
Active
YB66867
Quartz
TM
2
Active
YA61202
Quartz
KUKU
4
Active
YB66868
Quartz
TM
3
Active
YA61203
Quartz
KUKU
5
Active
YB66869
Quartz
TM
4
Active
YA61204
Quartz
KUKU
6
Active
YB66870
Quartz
TM
5
Active
YA61207
Quartz
KUKU
9
Active
YB66871
Quartz
TM
6
Active
YA61208
Quartz
KUKU
10
Active
YB66872
Quartz
TM
7
Active
YA61209
Quartz
KUKU
11
Active
YB66873
Quartz
TM
8
Active
YA61210
Quartz
KUKU
12
Active
YB66874
Quartz
TM
9
Active
YA61211
Quartz
KUKU
13
Active
YB66875
Quartz
TM
10
Active
YA61212
Quartz
KUKU
14
Active
YB66876
Quartz
TM
11
Active
YA61213
Quartz
KUKU
15
Active
YB66877
Quartz
TM
12
Active
YA61214
Quartz
KUKU
16
Active
YB66878
Quartz
TM
13
Active
YA61215
Quartz
KUKU
17
Active
YB66879
Quartz
TM
14
Active
YA61216
Quartz
KUKU
18
Active
YB66881
Quartz
TM
16
Active
YA61217
Quartz
KUKU
19
Active
YB66882
Quartz
TM
17
Active
YA61218
Quartz
KUKU
20
Active
YB66883
Quartz
TM
18
Active
YA61219
Quartz
KUKU
21
Active
YB66884
Quartz
TM
19
Active
Claim
Name
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YB97767
Quartz
KUKU
YA61221
Quartz
YA61222
YA61223
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
22
Active
YB66885
Quartz
TM
KUKU
23
Active
YB66886
Quartz
Quartz
KUKU
24
Active
YB66887
Quartz
KUKU
25
Active
YB66888
YA61224
Quartz
KUKU
26
Active
YA61225
Quartz
KUKU
27
YA61226
Quartz
KUKU
28
YA61227
Quartz
KUKU
29
YA61228
Quartz
KUKU
YA61229
Quartz
YA61230
Quartz
YA61231
Claim
Owner
Status
20
Active
TM
22
Active
Quartz
TM
23
Active
Quartz
TM
24
Active
YB66889
Quartz
TM
25
Active
Active
YB66890
Quartz
TM
26
Active
Active
YB66891
Quartz
TM
27
Active
Active
YB66892
Quartz
TM
28
Active
30
Active
YB66893
Quartz
TM
29
Active
KUKU
31
Active
YB66894
Quartz
TM
30
Active
KUKU
32
Active
YB66895
Quartz
TM
31
Active
Quartz
KUKU
33
Active
YB66896
Quartz
TM
32
Active
YA61232
Quartz
KUKU
34
Active
YB66899
Quartz
TM
35
Active
YA61233
Quartz
KUKU
35
Active
YB66900
Quartz
TM
36
Active
YA61234
Quartz
KUKU
36
Active
YB66901
Quartz
TM
37
Active
YA61235
Quartz
KUKU
37
Active
YB66902
Quartz
TM
38
Active
YA61236
Quartz
KUKU
38
Active
YB66903
Quartz
TM
39
Active
YA61237
Quartz
KUKU
39
Active
YB66904
Quartz
TM
40
Active
YA61238
Quartz
KUKU
40
Active
YB66905
Quartz
TM
41
Active
YA61239
Quartz
KUKU
41
Active
YB66906
Quartz
TM
42
Active
YA61241
Quartz
KUKU
43
Active
YB66907
Quartz
TM
43
Active
YA61243
Quartz
KUKU
45
Active
YB66908
Quartz
TM
44
Active
YA61244
Quartz
KUKU
46
Active
YB66909
Quartz
TM
45
Active
YA61245
Quartz
KUKU
47
Active
YB66910
Quartz
TM
46
Active
YA61246
Quartz
KUKU
48
Active
YB66911
Quartz
TM
47
Active
YA61624
Quartz
KUKU
50
Active
YB66912
Quartz
TM
48
Active
YA61639
Quartz
KUKU
65
Active
YB66913
Quartz
TM
49
Active
YA61640
Quartz
KUKU
66
Active
YB66914
Quartz
TM
50
Active
YA61671
Quartz
KUKU
97
Active
YB66915
Quartz
TM
51
Active
YA61672
Quartz
KUKU
98
Active
YB66916
Quartz
TM
52
Active
YA61673
Quartz
KUKU
99
Active
YB66917
Quartz
TM
53
Active
YA61674
Quartz
KUKU
100
Active
YB66918
Quartz
TM
54
Active
YA61768
Quartz
KUKU
194
Active
YB66919
Quartz
TM
55
Active
YA61770
Quartz
KUKU
196
Active
YB66920
Quartz
TM
56
Active
YA61771
Quartz
KUKU
197
Active
YB66921
Quartz
TM
57
Active
YA61772
Quartz
KUKU
198
Active
YB66922
Quartz
TM
58
Active
YA61773
Quartz
KUKU
199
Active
YB66923
Quartz
TM
59
Active
YA61824
Quartz
KUKU
250
Active
YB66924
Quartz
TM
60
Active
YA61825
Quartz
KUKU
251
Active
YB66925
Quartz
TM
61
Active
YA61856
Quartz
KUKU
282
Active
YB66926
Quartz
TM
62
Active
YA61857
Quartz
KUKU
283
Active
YB66927
Quartz
TM
63
Active
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YB67028
Quartz
LB
YB67029
Quartz
YB67030
YB67031
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
1
Active
YB66928
Quartz
TM
LB
2
Active
YB66929
Quartz
Quartz
LB
3
Active
YB66930
Quartz
LB
4
Active
YB66931
YB67032
Quartz
LB
5
Active
YB67033
Quartz
LB
6
YB67034
Quartz
LB
7
YB67035
Quartz
LB
8
YB67036
Quartz
LB
YB67037
Quartz
YB67038
Quartz
YB67039
Claim
Owner
Status
64
Active
TM
65
Active
Quartz
TM
66
Active
Quartz
TM
67
Active
YB66932
Quartz
TM
68
Active
Active
YB66933
Quartz
TM
69
Active
Active
YB66934
Quartz
TM
70
Active
Active
YB66935
Quartz
TM
71
Active
9
Active
YB66936
Quartz
TM
72
Active
LB
10
Active
YB66937
Quartz
TM
73
Active
LB
11
Active
YB66938
Quartz
TM
74
Active
Quartz
LB
12
Active
YB66939
Quartz
TM
75
Active
YB67040
Quartz
LB
13
Active
YB66940
Quartz
TM
76
Active
YB67041
Quartz
LB
14
Active
YB66941
Quartz
TM
77
Active
YB67042
Quartz
LB
15
Active
YB66942
Quartz
TM
78
Active
YB67043
Quartz
LB
16
Active
YB66943
Quartz
TM
79
Active
YB67044
Quartz
LB
17
Active
YB66944
Quartz
TM
80
Active
YB67045
Quartz
LB
18
Active
YB66945
Quartz
TM
81
Active
YB67046
Quartz
LB
19
Active
YB66946
Quartz
TM
82
Active
YB67047
Quartz
LB
20
Active
YB66947
Quartz
TM
83
Active
YB67048
Quartz
LB
21
Active
YB66948
Quartz
TM
84
Active
YB67049
Quartz
LB
22
Active
YB66949
Quartz
TM
85
Active
YB67050
Quartz
LB
23
Active
YB66950
Quartz
TM
86
Active
YB67051
Quartz
LB
24
Active
YB66951
Quartz
TM
87
Active
YB67052
Quartz
LB
25
Active
YB66952
Quartz
TM
88
Active
YB67053
Quartz
LB
26
Active
YB66953
Quartz
TM
89
Active
YB67054
Quartz
LB
27
Active
YB66954
Quartz
TM
90
Active
YA94610
Quartz
MB
1
Active
YB66955
Quartz
TM
91
Active
YA94611
Quartz
MB
2
Active
YB66956
Quartz
TM
92
Active
YA94612
Quartz
MB
3
Active
YB66957
Quartz
TM
93
Active
YB67166
Quartz
MIL
1
Active
YB66958
Quartz
TM
94
Active
YB67167
Quartz
MIL
2
Active
YB66959
Quartz
TM
95
Active
YB67168
Quartz
MIL
3
Active
YB66960
Quartz
TM
96
Active
YB67169
Quartz
MIL
4
Active
YB66961
Quartz
TM
97
Active
YB67170
Quartz
MIL
5
Active
YB66962
Quartz
TM
98
Active
YB67171
Quartz
MIL
6
Active
YB66963
Quartz
TM
99
Active
YB67172
Quartz
MIL
7
Active
YB66964
Quartz
TM
100
Active
YB67173
Quartz
MIL
8
Active
YB66965
Quartz
TM
101
Active
YB67174
Quartz
MIL
9
Active
YB66966
Quartz
TM
102
Active
YB67175
Quartz
MIL
10
Active
YB66967
Quartz
TM
103
Active
YB67176
Quartz
MIL
11
Active
YB66968
Quartz
TM
104
Active
Claim
Number
Grant
Number
Reg
Type
Claim
Name
YB67177
Quartz
MIL
YB67178
Quartz
YB67179
YB67180
Claim
Number
Claim
Owner
Status
Grant
Number
Reg
Type
Claim
Name
12
Active
YB66969
Quartz
TM
MIL
13
Active
YB66970
Quartz
Quartz
MIL
14
Active
YB66971
Quartz
MIL
15
Active
YB66972
YB67181
Quartz
MIL
16
Active
YB67182
Quartz
MIL
17
YB67183
Quartz
MIL
18
YB67184
Quartz
MIL
19
YB67185
Quartz
MIL
YB67186
Quartz
YB67187
Quartz
YB67188
Claim
Owner
Status
105
Active
TM
106
Active
Quartz
TM
107
Active
Quartz
TM
108
Active
YB66973
Quartz
TM
109
Active
Active
YB66974
Quartz
TM
110
Active
Active
YB66975
Quartz
TM
111
Active
Active
YB66976
Quartz
TM
112
Active
20
Active
YB66977
Quartz
TM
113
Active
MIL
21
Active
YB66978
Quartz
TM
114
Active
MIL
22
Active
YB66979
Quartz
TM
115
Active
Quartz
MIL
23
Active
YB66980
Quartz
TM
116
Active
YB67189
Quartz
MIL
24
Active
YB66981
Quartz
TM
117
Active
YB67190
Quartz
MIL
25
Active
YC07981
Quartz
TM
118
Active
YB67191
Quartz
MIL
26
Active
YC07982
Quartz
TM
119
Active
YB67192
Quartz
MIL
27
Active
YC07983
Quartz
TM
120
Active
YB67193
Quartz
MIL
28
Active
YC07984
Quartz
TM
121
Active
YB67194
Quartz
MIL
29
Active
YC07985
Quartz
TM
122
Active
YB67195
Quartz
MIL
30
Active
YC07986
Quartz
TM
123
Active
YB67196
Quartz
MIL
31
Active
YC07989
Quartz
TM
126
Active
YB67197
Quartz
MIL
32
Active
YC07990
Quartz
TM
127
Active
YB67198
Quartz
MIL
33
Active
YC07991
Quartz
TM
128
Active
YB67199
Quartz
MIL
34
Active
YC07992
Quartz
TM
129
Active
YB67200
Quartz
MIL
35
Active
YC07993
Quartz
TM
130
Active
YB67201
Quartz
MIL
36
Active
YC07994
Quartz
TM
131
Active
YB67202
Quartz
MIL
37
Active
YC07995
Quartz
TM
132
Active
YB67203
Quartz
MIL
38
Active
YC07996
Quartz
TM
133
Active
YB67204
Quartz
MIL
39
Active
YA82961
Quartz
TREE
1
Active
YB67205
Quartz
MIL
40
Active
YA82962
Quartz
TREE
2
Active
YB67206
Quartz
MIL
41
Active
YA82963
Quartz
TREE
3
Active
YB67207
Quartz
MIL
42
Active
YA82964
Quartz
TREE
4
Active
YB67208
Quartz
MIL
43
Active
YA82965
Quartz
TREE
5
Active
YB67209
Quartz
MIL
44
Active
Y 75547
Quartz
WH
1
Active
YB67210
Quartz
MIL
45
Active
Y 75548
Quartz
WH
2
Active
YB67211
Quartz
MIL
46
Active
Y 75549
Quartz
WH
3
Active
YB67212
Quartz
MIL
47
Active
Y 75550
Quartz
WH
4
Active
YB67213
Quartz
MIL
48
Active
Y 75551
Quartz
WH
5
Active
YB67214
Quartz
MIL
49
Active
Y 75552
Quartz
WH
6
Active
YB67215
Quartz
MIL
50
Active
Y 75553
Quartz
WH
7
Active
YB67216
Quartz
MIL
51
Active
Y 75554
Quartz
WH
8
Active
Claim
Number

TAGISH LAKE GOLD PROPERTY WHITEHORSE MINING

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