The Alaska-Premier is a silver, gold, copper, lead, and zinc 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
Elevation:
Commodity: Silver, Gold, Copper, Lead, Zinc
Lat, Long: 56.02583, -130.04194
Map: View on Google Maps
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Alaska-Premier MRDS details
Site Name
Primary: Alaska-Premier
Commodity
Primary: Silver
Primary: Gold
Primary: Copper
Primary: Lead
Primary: Zinc
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: Sphalerite
Ore: Chalcopyrite
Ore: Galena
Gangue: Quartz
Gangue: Pyrite
Comments
Comment (Workings): PROPERTY WAS EXPLORED BY OPEN CUTS AND DEVELOPED BY MORE THAN 200 FEET OF UNDERGROUND WORKINGS, PROBABLY MOSTLY IN THE 1920'S. SELECTED SAMPLES OF SULFIDE-RICH QUARTZ VEINS REPORTEDLY ASSAYED AS HIGH AS 35 OZ AU PER TON. ASSAYS OF SOME OF THE SHEARED AND MINERALIZED FELSITE SHOWED ABOUT 0.097-0.145 OZ AU AND 1.0 OZ AG PER TON.
Comment (Geology): LEAD-ISOTOPE STUDIES OF GALENA FROM THE ALASKA-PREMIER PROSPECT (MAAS AND OTHERS, 1995, P. 254) INDICATE THAT THE DEPOSIT IS JURASSIC IN AGE, CONTEMPORANEOUS, AT LEAST IN PART, WITH ISLAND-ARC VOLCANISM IN HAZELTON TIME (ALLDRICK, 1993).
Comment (Location): THE ALASKA-PREMIER PROSPECT IS IN SECTION 25 AT AN ELEVATION OF ABOUT 1340 FEET, APPROXIMATELY 0.2 MILE SOUTHWEST OF DALY CREEK (ELLIOTT AND KOCH, 1981, P. 17, LOC. 67). THE LOCATION IS ACCURATE TO WITHIN ABOUT 0.1 MILE. ALSO SEE ADDITIONAL COMMENTS FIELD, BELOW.
Comment (Deposit): THE COUNTRY ROCKS IN THE AREA OF THE ALASKA-PREMIER PROSPECT ARE PELITIC METASEDIMENTARY AND SUBORDINATE ANDESITIC (GREENSTONE) METAVOLCANIC STRATA OF THE JURASSIC OR OLDER MESOZOIC HAZELTON GROUP; THE TRIASSIC TEXAS CREEK GRANODIORITE, WHICH UNDERLIES AND LOCALLY INTRUDES THE HAZELTON; THE EOCENE BOUNDARY GRANODIORITE, WHICH INTRUDES THE HAZELTON AND TEXAS CREEK ROCKS; AND STILL-YOUNGER TERTIARY LAMPROPHYRE DIKES, WHICH CUT ALL THE OTHER ROCKS (SMITH, 1973, 1977, KOCH, 1996). THE DEPOSIT (BUDDINGTON, 1925, P. 74, 78-79; 1929, P. 85-86) IS IN GREENSTONE, SLATE, AND GRAYWACKE COUNTRY ROCKS. IT CONSISTS OF SULFIDE-BEARING QUARTZ VEINLETS IN SHATTERED ZONES IN THREE SHEETS OF ALTERED 'FELSITE,' WHICH MAY BE EITHER QUARTZ PORPHYRY SILLS OR A FACIES OF THE GREENSTONE. THE VEINS CONTAIN PYRITE, SPHALERITE, GALENA, PYRRHOTITE, AND CHALCOPYRITE; SELECTED SAMPLES REPORTEDLY ASSAYED AS HIGH AS 35 OZ AU PER TON. A 3-FOOT THICK MINERALIZED SHEAR ZONE IN A FELSITE SHEET CONTAINS
Comment (Deposit): PROPERTY PROBABLY ORIGINALLY STAKED IN EARLY 1920'S. THE ALASKA-PREMIER SITE PROBABLY INCLUDES THE OLD READY MONEY AND ALASKA CLAIMS (COBB, 1978, P. 92-93).
Comment (Exploration): Status = Inactive
Comment (Deposit): DISSEMINATED(?) PYRITE, GALENA, SPHALERITE, CHALCOPYRITE, TETRAHEDRITE, PYRRHOTITE, AND ARSENOPYRITE. ASSAYS OF SOME OF THE MINERALIZED FELSITE SHOWED ABOUT 0.097-0.145 OZ AU AND ABOUT 1.0 OZ AG PER TON. LEAD-ISOTOPE STUDIES OF GALENA FROM THE ALASKA-PREMIER PROSPECT (MAAS AND OTHERS, 1995, P. 254) INDICATE THAT THE DEPOSIT IS JURASSIC IN AGE, CONTEMPORANEOUS, AT LEAST IN PART, WITH ISLAND-ARC VOLCANISM IN HAZELTON TIME (ALLDRICK, 1993).
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., 1973, A Tertiary lamprophyre dike province in southeastern Alaska: Canadian Journal of Earth Sciences, v. 10, p. 408-420.
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): 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.
Reference (Deposit): Maas, K. M., Bittenbender, P. E., and Still, J. C., 1995, Mineral investigations in the Ketchikan mining district, southeastern Alaska: U. S. Bureau of Mines Open-File Report 11-95, 606 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): Alldrick, D. J., 1993, Geology and metallogeny of the Stewart mining camp, northwestern British Columbia: British Columbia Department of Mines and Petroleum Resources Bulletin no. 85, 105 p., 2 plates."
Reference (Deposit): Buddington, A.F., 1925, Mineral investigations in southeastern Alasaka: U.S. Geological Survey Bulletin 773, p. 71-139."
Reference (Deposit): Cobb, E. H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Bradfield Canal quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-922, 98 p."
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