The Hyder Skookum 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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Hyder Skookum MRDS details
Site Name
Primary: Hyder Skookum
Commodity
Primary: Copper
Location
State: Alaska
District: Hyder
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Chalcopyrite
Gangue: Pyrrhotite
Comments
Comment (Deposit): BUT ARE MOSTLY BARREN OF SULFIDES.
Comment (Deposit): THE COUNTRY ROCKS IN THE AREA OF THIS PROSPECT ARE PELITIC METASEDIMENTARY AND SUBORDINATE ANDESITIC (GREENSTONE) METAVOLCANIC STRATA OF THE JURASSIC OR OLDER MESOZOIC HAZELTON GROUP, WHICH IS UNDERLAIN AND LOCALLY INTRUDED BY THE TRIASSIC TEXAS CREEK GRANODIORITE (SMITH, 1977; KOCH, 1996). BUDDINGTON (1929, P. 72) DESCRIBES TWO TYPES OF DEPOSITS AT THIS SITE. ONE DEPOSIT IS A SULFIDE REPLACEMENT MASS IN SOMEWHAT SCHISTOSE GREENSTONE NEAR THE CONTACT OF A QUARTZ PORPHYRY DIKE. THE MASS CONSISTS OF PYRRHOTITE AND A LITTLE CHALCOPYRITE AND ARSENOPYRITE. SOME SULFIDES ALSO ARE DISSEMINATED IN QUARTZ IN THE SAME ZONE. THE OTHER TYPE OF DEPOSIT COMPRISES TWO PARALLEL QUARTZ VEINS UP TO 7 FEET THICK THAT LOCALLY FORM BRECCIAS WITH THE QUARTZ PORPHYRY OR GREENSTONE COUNTRY ROCKS. SOME OF THE COUNTRY ROCK FRAGMENTS IN THE BRECCIAS ARE IMPREGNATED WITH PYRITE AND A STRINGER IN THE GREENSTONE CARRIES A LITTLE DISSEMINATED SULFIDE. SURFACE EXPOSURES OF THE VEINS CARRY A LITTLE CALCITE
Comment (Location): THE HYDER SKOOKUM PROSPECT, IN SECTION 36 NEAR ITS SOUTHERN BOUNDARY, IS AT AN ELEVATION OF ABOUT 3150 FEET ON THE SOUTHEAST WALL OF SKOOKUM CREEK, AND ABOUT HUNDRED OR SO FEET ABOVE THE CREEK (ELLIOTT AND KOCH, 1981, P. 18, LOC. 76). THE LOCATION IS ACCURATE WITHIN ABOUT 0.2 MILE.
Comment (Exploration): Status = Inactive
Comment (Workings): DEPOSIT WAS EXPLORED BY AN OPEN CUT, PROBABLY IN THE 1920'S.
References
Reference (Deposit): Buddington, A.F., 1929, Geology of Hyder and vicinity, southeastern Alaska, with a reconnaissance of Chickamin River: U.S. Geological Survey Bulletin 807, 124 p."
Reference (Deposit): Smith, J.G., 1977, Geology of the Ketchikan D1 and Bradfield Canal A-1 quadrangles, southeastern Alaska: U.S. Geological Survey Bulletin 1425, 49 p.
Reference (Deposit): Elliott, R.L., and Koch, R. D., 1981, Mines, prospects, and selected metalliferous mineral occurrences in the Bradfield Canal quadrangle, Alaska: U.S. Geological Survey Open-File Report 81-728-B, 23 p., 1 sheet, scales 1:250,000 and 1:63,360.
Reference (Deposit): Koch, R. D., 1996, Reconnaissance geologic map of the Bradfield Canal quadrangle, southeastern Alaska: U.S. Geological Survey Open-File Report 81-728A, 35 p.,1 sheet, scale 1:250,000.
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