Denali Copper

The Denali Copper is a copper mine located in Alaska.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

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Site Name

Primary: Denali Copper
Secondary: Pass Creek
Secondary: Caribou Dome

Commodity

Primary: Copper
Secondary: Silver
Secondary: Zinc

Location

State: Alaska
District: Valdez Creek

Land Status

Not available

Holdings

Not available

Workings

Not available

Ownership

Not available

Production

Not available

Deposit

Record Type: Site
Operation Category: Prospect
Operation Type: Unknown
Years of Production:
Organization:
Significant:

Physiography

Not available

Mineral Deposit Model

Model Name: Basaltic Cu (BC name is Volcanic redbed Cu)

Orebody

Not available

Structure

Not available

Alterations

Alteration Type: L
Alteration Text: There is no hydrothermal alteration associated with the sulfide mineralization.

Rocks

Name: Tuff
Role: Associated
Age Type: Host Rock
Age Young: Late Triassic

Name: Tuff
Role: Associated
Age Type: Associated Rock
Age Young: Late Triassic

Analytical Data

Not available

Materials

Ore: Copper
Ore: Sphalerite
Ore: Pyrite
Ore: Malachite
Ore: Chalcopyrite
Ore: Chalcocite
Ore: Bornite
Ore: Azurite
Gangue: Quartz
Gangue: Calcite

Comments

Comment (Workings): Workings / Exploration = The deposit was discovered by M. A. Kaufman in 1963 while mapping for the State of Alaska Division of Mines and Minerals. It was subsequently staked by prospectors working for Leo Mark Anthony. From 1964 through 1968, exploration consisted of trenching, geologic mapping, geochemical and geophysical surveys, and diamond core drilling. ? In 1969, a 1,400-foot-long adit was driven from a portal at an elevation of 4,630 feet. This adit was driven to intersect and follow the drill-indicated trend of the widest known part of the deposit, which was informally called the main horizon. A crosscut was driven into the hanging wall approximately orthogonal to the main ore horizon to provide drill stations to intersect the down-dip extent of the main horizon. Slightly inclined percussion drill holes from this adit tested the adjacent areas out to about 100 feet. Surface diamond drilling tested the other four or five known ore horizons.? In 1970, an 1,800 foot long, minus-15-degree spiral decline was driven to provide drill stations for deep intercepts of the mineralized horizon, and to obtain bulk samples of the deposit. The main horizon has been tested by drilling as deep as 1,000 feet below outcrop. Drill testing of the other ore horizons has rarely been deeper than 300 feet.? Bulk samples for metallurgical testing were collected in both 1969 "&" 1970 as part of each underground exploration program. Three diamond core holes were drilled during the summer of 1999.

Comment (Geology): Age = This stratiform deposit is Late Triassic in age.

Comment (Exploration): Status = Active

Comment (Production): Production Notes = There has been no production.

Comment (Deposit): Model Name = Basaltic Cu (Cox and Singer 1986; model 23)

Comment (Reference): Primary Reference = Seraphim, 1975

Comment (Geology): Geologic Description = The Denali Copper prospect is near the upper contact of the Nikolai Greenstone, a thick sequence of Upper Triassic marine andesite and basalt, and subordinate clastic and carbonate units (Stevens, 1971, Wilson, and others, 1998). At the prospect, the strata dip at up to 80 degrees northwest and strike northeast. About a mile northwest of the prospect, the strata are cut by a strongly fractionated pluton dated by K-Ar methods at 130 to 143 m.y. (Smith, 1981).? the deposit consists of delicately-bedded to massive chalcopyrite and pyrite beds in black argillaceous limestone and black calcareous argillite. The massive, dominantly chalcopyrite beds are up to 12 inches thick and assay up to 12% copper. Pyrite commonly occurs as framboids. Minor bornite, chalcocite, and native copper occur locally, as well as sparse sphalerite. Gossans overlie the sulfide bodies and contain malachite, azurite, chalcocite, and minor chalcopyrite. A unique gossan material consisting of a jet-black earthy residue with relic bedding overlies the highest-grade portions of the sulfide horizons (D. L. Stevens, personal observation). Several major northeast-trending, strike-slip faults traverse the area. The most important occurs in the footwall just south of the main sulfide horizon; it is marked by a zone of fault gouge 20 to 50 feet in width. Movement along this fault has induced drag-folding of the steeply-dipping sulfide horizon, producing fold amplitudes of up to 50 feet. Northwest dipping thrust faults were encountered underground on the 4630-level adit. These faults offset the main horizon about 30 feet (Stevens, 1971). Regional mapping also shows a major southeast-dipping thrust fault that strikes northeast.? the main sulfide horizon, on which most of the exploration effort has been made, is up to 400 feet long and 30 feet wide; it extends at least 1,000 feet below the surface outcrop as confirmed by drilling. The sulfide horizons are characterized by 'pinching and swelling' along strike as well as down dip. As one horizon 'pinches', other horizons may 'swell'. The deposit remains open at depth and along strike both to the northeast and southwest on at least four known horizons. Their steep dip makes additions to the reserves expensive.? the rocks in this region were regionally metamorphosed to prehnite-pumpellyite-quartz facies (Stevens, 1971), but the very fine-grained sulfide minerals in the deposit were not recrystallized, as shown by chalcopyrite grains as small as 1 micron.? This sulfide deposit is interpreted to have formed in a reducing or euxinic marine basin with abundant organic matter and sulfate reducing bacteria (Stevens, 1971). Sulfur isotope ratio analyses of the chalcopyrite and pyrite averaged -28.35 permil with a standard deviation range of only 1.01 permil (Stevens, 1971). These values strongly confirm the biogenic reduction of the seawater sulfate to produce the sulfide ion and suggest the possibility of a closed system. The copper was probably derived by weathering of the subaerial copper-rich volcanic rocks adjacent to the marine basin.

Comment (Reserve-Resource): Reserves = the drill-indicated reserves of the main horizon were calculated to be 550,000 tons containing 5.84% copper, 0.3 ounces of silver per ton, and just a trace of gold (unpublished report by R. H. Seraphim, 1970). The other ore horizons have not been explored sufficiently to be included in reserve and resource calculations. The fine-grained nature of the sulfide minerals causes metallurgical complications which have largely been resolved by technological progress since the work done in the early 1970's.

Comment (Commodity): Ore Material = Copper (native)

References

Reference (Deposit): Bundtzen, T.K., Eakins, G.R., and Conwell, C.N., 1983, Alaska mineral resources 1981-82: Alaska Division of Geological and Geophysical Surveys Annual Report 1981-82, 153 p., 4 sheets, scale 1:2,500,000.

Reference (Deposit): MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous and selected non-metalliferous mineral deposits in the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-A, 99 p., 1 sheet, scale 1:1,000,000.

Reference (Deposit): Wilson, F.H., Dover, J.H., Bradley, D.C., Weber, F.R., Bundtzen, T.K., and Haeussler, P.J., 1998, Geologic map of central (interior) Alaska: U.S. Geological Survey Open-File Report 98-133, 17 p., 2 sheetsm, scale 1:500,000.

Reference (Deposit): Kaufman, M.A., 1964, Two new occurrences of ore minerals in the Denali area (Healy A-1 and Mt. Hayes B-6): Alaska Territorial Department of Mines Prospect Evaluation 67-4, 5 p.

Reference (Deposit): Stevens, D.L, 1971, Geology and geochemistry of the Denali Prospect, Clearwater Mountains, Alaska: Fairbanks, University of Alaska, Ph. D. dissertation, 81 p.

Reference (Deposit): Seraphim, R.H., 1975, Denali-A nonmetamorphosed stratiform sulfide deposit: Economic Geology, vol. 70, p. 949-959.

Reference (Deposit): Smith, T.E., 1981, Geology of the Clearwater Mountains, south-central Alaska: Alaska Division of Geological "&" Geophysical Surveys Geologic Report 60, 72 p., 3 sheets, scale 1:63,360.

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