General Information
Primary Commodities: copper, gold, silver, molybdenum
Aliases: Whitehorse Copper
Deposit Type(s): Skarn
Location(s): 60.5780 N, -134.96 W
NTS Mapsheet(s): 105D11
Hand Samples Available at YGS: No
Capsule
The Whitehorse Copper Belt is located west of Whitehorse and contains 30+ mines, deposits and showings. By 1900, most of the important deposits had been discovered and the first small ore shipment was made that year. Many of the occurrences in the Copper Belt are skarns. The skarns form on or near the contact between the Whitehorse batholith and the Lewes River group. The Whitehorse batholith is commonly a grey coarse-grained hornblende granite and ranges from quartz monzonite to granodiorite to diorite. The Lewes River group contains numerous different rock types, most importantly of which is the limestone group, which is essential in the formation of skarns in the area. A small number of occurrences within the Copper Belt are vein and/or replacement and occur within the Whitehorse batholith granite.
The Keewenaw deposit is an oval-shaped zone about 500 feet (152 m) long and 250 feet (76 m) wide. The zone trends southeasterly and there are numerous dark, fine-grained diorite dykes (< 10 - 30 ft. wide, < 3 - 9 m wide) which cut the granite at a southeast trend. The granite is cut by felsite dykes and by feldspar porphyry dykes that also strike southeasterly. The oval shaped zone contains bornite and malachite and the fine-grained granite is strongly altered to epidote and chlorite with numerous fine-grained veinlets and fractures. The silicate chrysocolla is present in some rock cuts. Sheared granite zones contain bornite and occasional malachite.
Production during 1971 totalled 151 770 tonnes of ore at 1.02% and produced 1 596 tonnes of refined metal at 99% Cu. Calculated reserves at the end of 1971 totalled 202 653 tonnes of ore at 1.06 Cu.
The Keewenaw deposit is an oval-shaped zone about 500 feet (152 m) long and 250 feet (76 m) wide. The zone trends southeasterly and there are numerous dark, fine-grained diorite dykes (< 10 - 30 ft. wide, < 3 - 9 m wide) which cut the granite at a southeast trend. The granite is cut by felsite dykes and by feldspar porphyry dykes that also strike southeasterly. The oval shaped zone contains bornite and malachite and the fine-grained granite is strongly altered to epidote and chlorite with numerous fine-grained veinlets and fractures. The silicate chrysocolla is present in some rock cuts. Sheared granite zones contain bornite and occasional malachite.
Production during 1971 totalled 151 770 tonnes of ore at 1.02% and produced 1 596 tonnes of refined metal at 99% Cu. Calculated reserves at the end of 1971 totalled 202 653 tonnes of ore at 1.06 Cu.
Location Map
Last Updated: Apr 15, 2019
Work History
Year | Work Type | Comment |
---|---|---|
2014 | Pre-existing Data: Research/Summarize | |
1998 | Geochemistry: Rock | |
1998 | Geochemistry: Soil | |
1970 | Development, Surface: All Weather Road | |
1970 | Development, Underground: Drifting/Raising | |
1970 | Drilling: Diamond | |
1966 | Studies: Feasibility | |
1964 | Drilling: Diamond | |
1964 | Ground Geophysics: IP |
Regional Geology - Terrane
Group: Intermontane
Affinity: W Laurentia
Name: Stikinia
Realm: peri-Laurentian
Regional Geology - Bedrock
Supergroup:
Group/Suite: Lewes River
Formation: Aksala
Member: Hancock
Terrane: Stikinia
Period Max: Triassic
Age Max: 217 MA
Period Min: Triassic
Age Min: 204 MA
Rock Major: conglo/limestone/dolostone
Rock Minor: chert
Reference: Wheeler (1961) - GSC Map 1093A
Geological Unit (1M): uTrAK
Geological Unit (250K): uTrAK2
Assessment Reports that overlap occurrence
Report Number | Year | Title | Worktypes | Holes Drilled | Meters Drilled |
---|---|---|---|---|---|
097154 | 2017 | Preliminary Geological Mapping on the Dennis 3, Lobo 1, and Gem 1 Claims | Bedrock Mapping - Geology, Prospecting - Other | ||
096680 | 2014 | Summary Report Documenting the Cowley, Keewenaw and Gem Copper Deposits on the Lobo Property | Research/Summarize - Pre-existing Data | ||
095193 | 2008 | Drilling and Geophysical Assessment Report on the Whitehorse Copper Belt Project | Diamond - Drilling, Drill Core - Geochemistry, IP - Ground Geophysics | 21 | 2134.10 |
094024 | 1998 | [Geological Report on the Sue,Jim,Ace,Dennis,Gem and Lobo Claims] | Rock - Geochemistry, Soil - Geochemistry | ||
092025 | 1974 | [Proposed 1974 Exploration of the Cowley Park and War Eagle Properties] | Property Evaluation - Other | ||
061172 | 1974 | [Proposed 1974 Exploration of the Cowley Park and War Eagle Properties] | Property Evaluation - Other | ||
061173 | 1974 | Report on Exploratory Work on Whitehorse Copper Belt | Diamond - Drilling, Drill Core - Geochemistry, IP - Ground Geophysics | 10 | 2222.29 |
062018 | 1973 | Preliminary Report on Geological Control to Ore Distribution in the Whitehorse Copper Belt | Reverse Circulation - Drilling, Bedrock Mapping - Geology, Petrographic - Lab Work/Physical Studies | 665 | 5555 |
090945 | 1970 | [Drilling, Stripping and Road Construction on the Whitehorse Copper Belt Project] | All Weather Road - Development, Surface, Drifting/Raising - Development, Underground, Diamond - Drilling | 5 | 206.96 |
091116 | 1968 | [Diamond Drilling on the Gem 1 Claims] | Diamond - Drilling | 10 | 950.21 |
062227 | 1966 | An Evaluation of the New imperial Mines Ltd. | Feasibility - Studies |
Related References
Number | Title | Page(s) | Document Type |
---|---|---|---|
ARMC004841 | Geology and geophysics map - Chargeability milliseconds - Gem and Keewenaw | Geophysical Map | |
ARMC004840 | Map showing chargeability contours - 4 m/sec, 20 ppm contour - Gem and Keewenaw | Geophysical Map | |
ARMC004844 | Exploration composite map - Keewenaw and Cowley Park - Figure 7 | Geoscience Map (General) | |
ARMC004839 | Geology map - Gem-Keewenaw | Geoscience Map (Geological - Bedrock) | |
ARMC004834 | Exploration composite map - Keewenaw and Cowley Park | Geoscience Map (Geological - Bedrock) | |
ARMC004842 | Map showing Tavern Lake | Geoscience Map (General) | |
1984-1 | The Whitehorse Copper Belt - A Compilation | Open File (Geological - Bedrock) |
Citations |
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Carriere, J J, et al. “Copper Deposits and Occurrences in Yukon Territory.” Ottawa: Geological Survey of Canada, 1982., 1981, doi:10.4095/109350. |
Kindle, E.D., “Summary of Research: Field, 1962”; Geological Survey of Canada, Paper no. 63-1, 1963, https://doi.org/10.4095/121464 (Open Access) |
The mineral industry of Yukon Territory and southwestern District of Mackenzie 1964; Green, L H. Geological Survey of Canada, Paper 65-19, 1965, 94 pages, https://doi.org/10.4095/100981 (Open Access) |