General Information
Secondary Commodities: gold, silver, antimony
Aliases: South Donahue, White Gold
Deposit Type(s): Porphyry-related Au
Location(s): 63.144170 N, -139.476390 W
NTS Mapsheet(s): 115O03
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No
Capsule
Work History
*This occurrence covers the Donahue gold zones and has been broken out from the McKinnon occurrence (Minfile Occurrence #115O 013) and given its own occurrence number
In Jan/2003 S. Ryan staked White cl 1-12 (YC23532) 8.5 km to the northwest. Ryan added White cl 13-46 (YC27120) in Jun/2003 and White cl 47-106 (YC25657) in Dec/2003. In Jan/2004 S. Ryan optioned the White claims to Madalena Ventures Inc, which carried out exploration programs in 2004 and 2005.
In Jun/2006 Madalena transferred its interest in the White claims to 638523 B.C. Ltd (Newco) a wholly-owned subsidiary of the company in order to concentrate on their oil and gas properties. The White claims option was dropped at the end of 2006 and the claims were returned to Ryan. In Mar/2007 S. Ryan staked White cl 107-118 (YC60626) 4 km to the northeast.
Staked within White cl 119-199 (YC60719)in early May/2007 by S. Ryan who on May 16, 2007 optioned the entire White claim block to Underworld Resources Ltd. Later in the summer Underworld carried out soil sampling, geological mapping, trenching, rock sampling and IP ground surveys on the claim block.
In Jul/2008 White cl 200-303 (YC75721) were added onto the northern boundary of the claim block. In 2008 Underworld Resources drilled 27 diamond drill holes (3 431 m) on the White claims. One hole (167.68 m) was collared to test the Donahue gold soil anomaly (this occurrence). In Oct/2008 Underworld staked White cl 304-376 (YC84213 to the south and east).
In 2009 Underworld carried out a three phase diamond drill program consisting of 25,670 m in 94 holes. The company drilled 3 holes at the Donahue gold zone (768.1 m), 5 holes at South Donahue gold zone (979.3 m - located 1.5 km to the south) In addition the company dug 2 trenches on the Donahue gold zone and 7 trenches on the South Donahue gold zone. The company also carried out regional mapping and sampling programs.
In Mar/2010 Kinross Gold Corp announced a proposed acquisition of all shares of Underworld Resources with the aim of acquiring control of the White Gold deposit and Underworld’s various exploration properties located in the Dawson region of the Yukon. In Apr/2010 Kinross announced its successful acquisition of 87% of the issued and outstanding common shares of Underworld Resources. Kinross immediately took steps to acquire the remaining shares of the company and on June 30, 2010 took Underworld Resources private resulting in Underworld Resources becoming a wholly-owned subsidiary of Kinross.
As a privately held company Underworld is not required to release exploration results. According to Yukon Exploration and Geology 2010, Kinross spent $14 000 000 exploring on both the White Gold and JP Ross properties (Minfile Occurrence #115O 160) located approximately 60 km to the northeast. Property-wide geological mapping, airborne geophysical surveys, soil sampling survey and over 25 000 m of diamond drilling was completed on the two properties.
Capsule Geology
The geology of the Stewart River Area was remapped by J. Ryan and S. Gordey (2004) of the Geological Survey of Canada beginning in 2000 as a component of the Ancient Pacific Margin NATMAP Project. The NATMAP Project is a interagency project initiated by the Geological Survey of Canada, Yukon Geology Program (now Yukon Geological Survey) and British Columbia Geological Survey Branch to understand the composition, relationships and metallogenic of poorly understood pericratonic terranes lying between the ancestral North American margin and those known with more certainty to be tectonically accreted. The Stewart River component focuses on the Yukon-Tanana terrane, comprising complexly deformed mostly (?) Paleozoic meta-igneous and metasedimentary rocks. In 2005 S. Gordey and J. Ryan released a geological compilation map for the Stewart River area. The map units generally remained the same as the 2004 geology map but age dates were changed to reflect new dates obtained through geochronology data.
J. Ryan reported that the Stewart River area is underlain by twice-transposed, amphibolite-facies gneiss and schist of mostly (?) Paleozoic age. These are intruded by younger plutonic rocks (Jurassic, Cretaceous and Eocene) and overlain by upper Cretaceous volcanic rocks. Metasiliclastic rocks are widespread and dominated by psammite and quartzite, with lesser pelite and rare conglomerate. Preliminary detrital zircon geochronology and geochronology for plutonic rocks constrain the siliclastic rocks to the Middle Paleozoic. Amphibolite interdigitates with and stratigraphically overlies the siliclastic rocks. Marble horizons ((?) reefs) occurs within the amphibolite and siliclastic rocks. Orthogneissic rocks with diorite, tonalite and granodiorite protoliths intrude both the siliclastic and amphibole assemblages; it is interpreted as a subvolcanic intrusive complex.
Geological mapping by J. Ryan and S. Gordey shows the area surrounding the occurrence is dominated by an intensely folded package of felsic psammites with lesser quartzite, conglomerate and rare marble horizons, interdigitated with amphiboles of probable volcaniclastic protolith. A felsic orthogneiss has been thrust to the northeast. This package has been thrust over a weakly deformed garnet-biotite gneissic unit. This contact defines the tectonostraigraphic boundary between the underlying, weakly deformed garnet-biotite gneissic unit and the overlying, intensely deformed assemblage. The deformed assemblage (and most likely the undeformed unit) is cross-cut by quartz monzonite dykes, up to two metres thick with a minimum of three generations of emplacement (observed from cross-cutting relationships) Large quartz diorite dykes, displaying no deformation, have also been mapped to the north and the south. A cap of mafic-ultramafic rock has been thrust on top of the stratigraphic pile.
The area surrounding this location is underlain by Devonian to Mississippian age psammite/quartz-mica schist. This portion of the White claims was not explored until 2007 at which time Underworld Resources carried out geological mapping and soil and rock sampling. The results were added to previous years results. Soil sampling to date across the White claim block outlined a large gold, arsenic and antimony soil anomaly measuring 8 by 3.5 km across the length of the claim block. The anomaly consists of numerous discrete gold anomalies with a threshold of 50 ppb gold.
Soil sampling in 2007 outlined the Donahue gold zone (soil anomaly – this occurrence). The Donahue gold zone measures 800 by 700 m with 35 of 374 samples exceeding 40 ppb gold. The average of the anomalous samples was 414 ppb gold with a maximum value of 9 019 ppb gold (Underworld press release 12 Feb/2008). Further soil sampling in 2008 outlined the South Donahue gold zone located 1.5 km to the south. The single 2008 diamond drill hole was collared towards the northwest end of the Donahue gold soil anomaly. Hole WD-015 returned 1.30 g/t gold over 1.0 m from a down hole depth of between 114.50 and 115.50 m.
Trenching, soil and rock sampling carried out in 2009 at the Donahue soil anomaly encountered, near surface gold mineralization similar in style to the Golden Saddle deposit (Minfile Occurrence # 115O 165). Diamond drill hole DN09-01collared on the Donahue soil anomaly returned 1.00 g/t gold over 2 m while hole DN09-03 returned 21.5 g/t over 0.73 m. Hole DN09-02 did not return any significant intersections (Underworld Press Release – Sep 10/2009).
The South Donahue gold zone occurs in similar host rocks to the Golden Saddle deposit and possesses similar geochemical signature. Diamond drilling intersected 1 to 5 m thick quartz veins hosted within an altered granitoid, however no significant values were returned from any of the five drill holes (Underworld Press Release – Oct 19/2009).
Since its take-over of Underworld Resources, Kinross Gold has not publicly released any detailed results from the White Gold project.
References
GORDEY, S.P. AND MAKEPEACE, A.J. 2003: Yukon Digital Geology, version 2.0, S.P. Gordey and A.J. Makepeace (comp); Geological Survey of Canada, Open File 1749 and Yukon Geological Survey, Open File 2003-9 (D).
GORDEY, S.P. AND RYAN, J.J. 2005. Geology, Stewart River Area (115N, 115 O and part of 115J), Yukon Territory; Geological Survey of Canada, Open File 4970, scale 1:250 000.
KINROSS GOLD CORP., May/2011. Web Site: www.kinross.com.
MORTENSEN, J.K., 1990. Geology and U-Pb geochronology of the Klondike district, west-central Yukon Territory. Canadian Journal of Earth Sciences, vol. 27, p. 903-914.
RYAN, J.J. AND GORDEY, S.P., 2002: Bedrock geology of Yukon-Tanana terrane in southern Stewart River map area, Yukon Territory; Geological Survey of Canada, Current Research 2002-A1, 11 p.
Ryan, J.J. ET AL., 2003: Update on bedrock geological mapping of the Yukon-Tanana terrane, southern Stewart River map area, Yukon Territory; Geological Survey of Canada, Current Research 2003-A9, 7 p.
Ryan, J.J. AND GORDEY, S.P., 2004; Geology Stewart River Area (Parts of 115N/1,2,7,8 and 115O/2- 12), Yukon Territory; Geological Survey of Canada, Open file 4641, scale 1:100 000.
RYAN. S., AND UNDERWORLD RESOURCES INC., Dec/2008. Assessment Report #095034 by S. Ryan and A. Fleming, (two reports).
SHIVES, R.B.K., ET. AL. (2002): Airborne multisensor geophysical survey, Stewart River area, Yukon Territory, Phase 1 and 2 (parts of 115N and 116B); Geological Survey of Canada, Open file 4311. (also Yukon Exploration and Geological Services Division, Open File 2002-17D).
SRK CONSULTING (CANADA) INC. Mar/2010. White Gold Property, Dawson Range, Yukon, Canada. By L Weirshauser, M Nowark and W. Barnett. (Project Number 2CU003.000).
UNDERWORLD RESOURCES INC, Annual Report 2007 – Management Discussion and Analysis p. 6, 2008 p. 7.
UNDERWORLD RESOURCES INC., Jul/2009. Assessment Report #095090 by H.K. Paulsen.
UNDERWORLD RESOURCES INC., Jun/2010. Assessment Report #095338 by H.K. Paulsen.
UNDERWORLD RESOURCES INC, News Release, 16 May/2007, 12 Feb/200818 Feb/2008, 17 Jun/2008, 23 Jul/2008, 27 Aug/2008, 24 Sep/2008, 28 Sep/2008, 24 Nov/2008, 6 May/2009, 12 Jun/2009, 23 Jun/2009, 10 Sep/2009, 19 Oct/2009, 28 Oct/2009, 5 Jan/2010, 19 Jan/2010, 27 Jan/2010, 11 Mar/2010, 26 Ap/2010, 30 Jun/2010.
UNDERWORLD RESOURCES INC., Oct/2009. Web Site: www.underworldresources.com
YUKON EXPLORATION AND GEOLOGY 2007, p. 15, 2008, p.15-16, 2009, p. 24-25, 55, 58, 2010, p. 26, 61, 65.
*This occurrence covers the Donahue gold zones and has been broken out from the McKinnon occurrence (Minfile Occurrence #115O 013) and given its own occurrence number
In Jan/2003 S. Ryan staked White cl 1-12 (YC23532) 8.5 km to the northwest. Ryan added White cl 13-46 (YC27120) in Jun/2003 and White cl 47-106 (YC25657) in Dec/2003. In Jan/2004 S. Ryan optioned the White claims to Madalena Ventures Inc, which carried out exploration programs in 2004 and 2005.
In Jun/2006 Madalena transferred its interest in the White claims to 638523 B.C. Ltd (Newco) a wholly-owned subsidiary of the company in order to concentrate on their oil and gas properties. The White claims option was dropped at the end of 2006 and the claims were returned to Ryan. In Mar/2007 S. Ryan staked White cl 107-118 (YC60626) 4 km to the northeast.
Staked within White cl 119-199 (YC60719)in early May/2007 by S. Ryan who on May 16, 2007 optioned the entire White claim block to Underworld Resources Ltd. Later in the summer Underworld carried out soil sampling, geological mapping, trenching, rock sampling and IP ground surveys on the claim block.
In Jul/2008 White cl 200-303 (YC75721) were added onto the northern boundary of the claim block. In 2008 Underworld Resources drilled 27 diamond drill holes (3 431 m) on the White claims. One hole (167.68 m) was collared to test the Donahue gold soil anomaly (this occurrence). In Oct/2008 Underworld staked White cl 304-376 (YC84213 to the south and east).
In 2009 Underworld carried out a three phase diamond drill program consisting of 25,670 m in 94 holes. The company drilled 3 holes at the Donahue gold zone (768.1 m), 5 holes at South Donahue gold zone (979.3 m - located 1.5 km to the south) In addition the company dug 2 trenches on the Donahue gold zone and 7 trenches on the South Donahue gold zone. The company also carried out regional mapping and sampling programs.
In Mar/2010 Kinross Gold Corp announced a proposed acquisition of all shares of Underworld Resources with the aim of acquiring control of the White Gold deposit and Underworld’s various exploration properties located in the Dawson region of the Yukon. In Apr/2010 Kinross announced its successful acquisition of 87% of the issued and outstanding common shares of Underworld Resources. Kinross immediately took steps to acquire the remaining shares of the company and on June 30, 2010 took Underworld Resources private resulting in Underworld Resources becoming a wholly-owned subsidiary of Kinross.
As a privately held company Underworld is not required to release exploration results. According to Yukon Exploration and Geology 2010, Kinross spent $14 000 000 exploring on both the White Gold and JP Ross properties (Minfile Occurrence #115O 160) located approximately 60 km to the northeast. Property-wide geological mapping, airborne geophysical surveys, soil sampling survey and over 25 000 m of diamond drilling was completed on the two properties.
Capsule Geology
The geology of the Stewart River Area was remapped by J. Ryan and S. Gordey (2004) of the Geological Survey of Canada beginning in 2000 as a component of the Ancient Pacific Margin NATMAP Project. The NATMAP Project is a interagency project initiated by the Geological Survey of Canada, Yukon Geology Program (now Yukon Geological Survey) and British Columbia Geological Survey Branch to understand the composition, relationships and metallogenic of poorly understood pericratonic terranes lying between the ancestral North American margin and those known with more certainty to be tectonically accreted. The Stewart River component focuses on the Yukon-Tanana terrane, comprising complexly deformed mostly (?) Paleozoic meta-igneous and metasedimentary rocks. In 2005 S. Gordey and J. Ryan released a geological compilation map for the Stewart River area. The map units generally remained the same as the 2004 geology map but age dates were changed to reflect new dates obtained through geochronology data.
J. Ryan reported that the Stewart River area is underlain by twice-transposed, amphibolite-facies gneiss and schist of mostly (?) Paleozoic age. These are intruded by younger plutonic rocks (Jurassic, Cretaceous and Eocene) and overlain by upper Cretaceous volcanic rocks. Metasiliclastic rocks are widespread and dominated by psammite and quartzite, with lesser pelite and rare conglomerate. Preliminary detrital zircon geochronology and geochronology for plutonic rocks constrain the siliclastic rocks to the Middle Paleozoic. Amphibolite interdigitates with and stratigraphically overlies the siliclastic rocks. Marble horizons ((?) reefs) occurs within the amphibolite and siliclastic rocks. Orthogneissic rocks with diorite, tonalite and granodiorite protoliths intrude both the siliclastic and amphibole assemblages; it is interpreted as a subvolcanic intrusive complex.
Geological mapping by J. Ryan and S. Gordey shows the area surrounding the occurrence is dominated by an intensely folded package of felsic psammites with lesser quartzite, conglomerate and rare marble horizons, interdigitated with amphiboles of probable volcaniclastic protolith. A felsic orthogneiss has been thrust to the northeast. This package has been thrust over a weakly deformed garnet-biotite gneissic unit. This contact defines the tectonostraigraphic boundary between the underlying, weakly deformed garnet-biotite gneissic unit and the overlying, intensely deformed assemblage. The deformed assemblage (and most likely the undeformed unit) is cross-cut by quartz monzonite dykes, up to two metres thick with a minimum of three generations of emplacement (observed from cross-cutting relationships) Large quartz diorite dykes, displaying no deformation, have also been mapped to the north and the south. A cap of mafic-ultramafic rock has been thrust on top of the stratigraphic pile.
The area surrounding this location is underlain by Devonian to Mississippian age psammite/quartz-mica schist. This portion of the White claims was not explored until 2007 at which time Underworld Resources carried out geological mapping and soil and rock sampling. The results were added to previous years results. Soil sampling to date across the White claim block outlined a large gold, arsenic and antimony soil anomaly measuring 8 by 3.5 km across the length of the claim block. The anomaly consists of numerous discrete gold anomalies with a threshold of 50 ppb gold.
Soil sampling in 2007 outlined the Donahue gold zone (soil anomaly – this occurrence). The Donahue gold zone measures 800 by 700 m with 35 of 374 samples exceeding 40 ppb gold. The average of the anomalous samples was 414 ppb gold with a maximum value of 9 019 ppb gold (Underworld press release 12 Feb/2008). Further soil sampling in 2008 outlined the South Donahue gold zone located 1.5 km to the south. The single 2008 diamond drill hole was collared towards the northwest end of the Donahue gold soil anomaly. Hole WD-015 returned 1.30 g/t gold over 1.0 m from a down hole depth of between 114.50 and 115.50 m.
Trenching, soil and rock sampling carried out in 2009 at the Donahue soil anomaly encountered, near surface gold mineralization similar in style to the Golden Saddle deposit (Minfile Occurrence # 115O 165). Diamond drill hole DN09-01collared on the Donahue soil anomaly returned 1.00 g/t gold over 2 m while hole DN09-03 returned 21.5 g/t over 0.73 m. Hole DN09-02 did not return any significant intersections (Underworld Press Release – Sep 10/2009).
The South Donahue gold zone occurs in similar host rocks to the Golden Saddle deposit and possesses similar geochemical signature. Diamond drilling intersected 1 to 5 m thick quartz veins hosted within an altered granitoid, however no significant values were returned from any of the five drill holes (Underworld Press Release – Oct 19/2009).
Since its take-over of Underworld Resources, Kinross Gold has not publicly released any detailed results from the White Gold project.
References
GORDEY, S.P. AND MAKEPEACE, A.J. 2003: Yukon Digital Geology, version 2.0, S.P. Gordey and A.J. Makepeace (comp); Geological Survey of Canada, Open File 1749 and Yukon Geological Survey, Open File 2003-9 (D).
GORDEY, S.P. AND RYAN, J.J. 2005. Geology, Stewart River Area (115N, 115 O and part of 115J), Yukon Territory; Geological Survey of Canada, Open File 4970, scale 1:250 000.
KINROSS GOLD CORP., May/2011. Web Site: www.kinross.com.
MORTENSEN, J.K., 1990. Geology and U-Pb geochronology of the Klondike district, west-central Yukon Territory. Canadian Journal of Earth Sciences, vol. 27, p. 903-914.
RYAN, J.J. AND GORDEY, S.P., 2002: Bedrock geology of Yukon-Tanana terrane in southern Stewart River map area, Yukon Territory; Geological Survey of Canada, Current Research 2002-A1, 11 p.
Ryan, J.J. ET AL., 2003: Update on bedrock geological mapping of the Yukon-Tanana terrane, southern Stewart River map area, Yukon Territory; Geological Survey of Canada, Current Research 2003-A9, 7 p.
Ryan, J.J. AND GORDEY, S.P., 2004; Geology Stewart River Area (Parts of 115N/1,2,7,8 and 115O/2- 12), Yukon Territory; Geological Survey of Canada, Open file 4641, scale 1:100 000.
RYAN. S., AND UNDERWORLD RESOURCES INC., Dec/2008. Assessment Report #095034 by S. Ryan and A. Fleming, (two reports).
SHIVES, R.B.K., ET. AL. (2002): Airborne multisensor geophysical survey, Stewart River area, Yukon Territory, Phase 1 and 2 (parts of 115N and 116B); Geological Survey of Canada, Open file 4311. (also Yukon Exploration and Geological Services Division, Open File 2002-17D).
SRK CONSULTING (CANADA) INC. Mar/2010. White Gold Property, Dawson Range, Yukon, Canada. By L Weirshauser, M Nowark and W. Barnett. (Project Number 2CU003.000).
UNDERWORLD RESOURCES INC, Annual Report 2007 – Management Discussion and Analysis p. 6, 2008 p. 7.
UNDERWORLD RESOURCES INC., Jul/2009. Assessment Report #095090 by H.K. Paulsen.
UNDERWORLD RESOURCES INC., Jun/2010. Assessment Report #095338 by H.K. Paulsen.
UNDERWORLD RESOURCES INC, News Release, 16 May/2007, 12 Feb/200818 Feb/2008, 17 Jun/2008, 23 Jul/2008, 27 Aug/2008, 24 Sep/2008, 28 Sep/2008, 24 Nov/2008, 6 May/2009, 12 Jun/2009, 23 Jun/2009, 10 Sep/2009, 19 Oct/2009, 28 Oct/2009, 5 Jan/2010, 19 Jan/2010, 27 Jan/2010, 11 Mar/2010, 26 Ap/2010, 30 Jun/2010.
UNDERWORLD RESOURCES INC., Oct/2009. Web Site: www.underworldresources.com
YUKON EXPLORATION AND GEOLOGY 2007, p. 15, 2008, p.15-16, 2009, p. 24-25, 55, 58, 2010, p. 26, 61, 65.
Location Map
Last Updated: Sep 12, 2012
Work History
| Year | Work Type | Comment |
|---|---|---|
| 2009 | Drilling: Diamond | Number of holes drilled: 8 Amount of work done: 1747.4 METRES Three holes (768.1 m) collared on Donahue, five holes (979.3) collared on South Donahue. |
| 2009 | Geology: Bedrock Mapping | Regional scale. |
| 2009 | Trenching | Total of Nine trenches. |
| 2008 | Drilling: Diamond | Number of holes drilled: 1 Amount of work done: 167.68 METRES Part of larger program. |
| 2007 | Geochemistry: Soil | |
| 2007 | Geology: Bedrock Mapping | Reconnaissance scale. |
| 2007 | Ground Geophysics: IP | Ground survey. |
| 2007 | Trenching |
Regional Geology - Terrane
Group: Intermontane
Affinity: W Laurentia
Name: Yukon-Tanana
Realm: peri-Laurentian
Regional Geology - Bedrock
Supergroup:
Group/Suite: Snowcap
Formation:
Member:
Terrane: Yukon-Tanana
Period Max: Ediacaran
Age Max: 635 MA
Period Min: Devonian
Age Min: 375 MA
Rock Major: Fp-qtz-mica gneiss, schist
Rock Minor:
Reference: Bailey (2013) - UBC MSc thesis
Geological Unit (1M): PDS
Geological Unit (250K): PDS1
Assessment Reports that overlap occurrence
| Report Number | Year | Title | Worktypes | Holes Drilled | Meters Drilled |
|---|---|---|---|---|---|
| 097276 | 2018 | 2018 Geochmical, Geophysical, Geological and Drilling Assessment Report | Orthophoto - Airphotography, Diamond - Drilling, Reverse Circulation - Drilling, Rock - Geochemistry, IP - Ground Geophysics, Resistivity - Ground Geophysics | 60 | 18647.05 |
| 097246 | 2017 | Geochemical, Geophysical, Geological, and Drilling Assessment Report: White Gold Project | Electromagnetic - Airborne Geophysics, Magnetic - Airborne Geophysics, Orthophoto - Airphotography, Diamond - Drilling, Reverse Circulation - Drilling, Rock - Geochemistry, Soil - Geochemistry | 35 | 5272.19 |
| 096402 | 2012 | 2012 Exploration Report, White Gold Claim Blocks | Rock - Geochemistry, Rock - Geochemistry, Soil - Geochemistry, Soil - Geochemistry, Gamma-ray Spectrometry - Ground Geophysics, Gamma-ray Spectrometry - Ground Geophysics, Prospecting - Other, Prospecting - Other, Backhoe - Trenching, Backhoe - Trenching | ||
| 096215 | 2011 | White Gold, 2011 Surface Exploration Report | Rock - Geochemistry, Rock - Geochemistry, Silt - Geochemistry, Silt - Geochemistry, Soil - Geochemistry, Soil - Geochemistry, Regional Bedrock Mapping - Geology, Regional Bedrock Mapping - Geology, Prospecting - Other, Prospecting - Other, Backhoe - Trenching, Backhoe - Trenching | ||
| 096207 | 2010 | High resolution Airborne Geophysical Report on the White and the Black Fox Group | Electromagnetic - Airborne Geophysics, Gamma-Ray Spectrometry - Airborne Geophysics | ||
| 096206 | 2010 | Geological and Geochemical Report on the White Groups and Black Fox | Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Prospecting - Other, Backhoe - Trenching | ||
| 095338 | 2009 | Report on the 2009 Diamond Drill, Geological and Geochemical Work Program on the White Gold, Black Fox, Yellow, JP Ross and Maisy Properties | All Weather Road - Development, Surface, Diamond - Drilling, Drill Core - Geochemistry, Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Detailed Bedrock Mapping - Geology, Metallurgical Tests - Lab Work/Physical Studies, Prospecting - Other, Environmental Assessment/Impact - Studies, Resource Estimate - Studies, Backhoe - Trenching | 94 | 25891.67 |
| 095090 | 2008 | Drilling - Geochemical - Geological Report on the BLACK FOX CATH CATHY CCC WHITE and WS Claims | Diamond - Drilling, Drill Core - Geochemistry, Rock - Geochemistry, Soil - Geochemistry, Detailed Bedrock Mapping - Geology, Regional Bedrock Mapping - Geology, Backhoe - Trenching, Hand - Trenching | 27 | 3433 |
| 095034 | 2007 | Geochemical Geological Report White Claims | Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, IP - Ground Geophysics, Prospecting - Other, Backhoe - Trenching | ||
| 094646 | 2005 | Report on the Line Cutting on the White Property | Line Cutting - Other | ||
| 094607 | 2005 | Report on the Soil Geochemistry on the White Property | Soil - Geochemistry, Magnetics - Ground Geophysics | ||
| 094508 | 2003 | Geochemical Report White Claims | Rock - Geochemistry, Soil - Geochemistry, Prospecting - Other |
