The Glacier is a silver, gold, molybdenum, lead, and 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
Elevation:
Commodity: Silver, Gold, Molybdenum, Lead, Copper
Lat, Long: 56.04, -130.39972
Map: View on Google Maps
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Glacier MRDS details
Site Name
Primary: Glacier
Secondary: Banded Mountain
Commodity
Primary: Silver
Primary: Gold
Primary: Molybdenum
Primary: Lead
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
Name: Lamprophyre
Role: Associated
Age Type: Host Rock
Age Young: Late Jurassic
Name: Lamprophyre
Role: Associated
Age Type: Host Rock Unit
Age Young: Late Jurassic
Analytical Data
Not available
Materials
Ore: Chalcopyrite
Ore: Galena
Ore: Molybdenite
Gangue: Quartz
Gangue: Pyrite
Comments
Comment (Workings): WORKINGS ON THE GLACIER PROSPECT INCLUDED SURFACE STRIPPING AND AN 8-FOOT ADIT (BUDDINGTON, 1929, P. 120-121). EARLY ASSAYS SHOWED 0.04 OZ AU AND 6 OZ AG PER TON AND 3% CU. ASSAYS OF CHIP SAMPLES OF AN IRON-STAINED ZONE TAKEN BY THE U.S. BUREAU OF MINES IN 1972-3 SHOWED 10-60 PPM CU, 10-15 PPM PB, 30-150 PPM ZN, AND UP TO 10 PPM MO.
Comment (Deposit): OF ABOUT 3000-4300 FEET ON THE NORTHWEST SIDE OF BANDED MOUNTAIN ABOUT ONE MILE DUE WEST OF THE SUMMIT. HAZELTON GROUP GNEISS AND SCHIST IN THE IRON-STAINED ZONE CONTAIN UP TO 2% PYRITE AND PYRRHOTITE. ASSAYS OF CHIP SAMPLES OF THE ZONE SHOWED 10-60 PPM CU, 10-15 PPM PB, 30-150 PPM ZN, AND UP TO 10 PPM MO.
Comment (Deposit): SITE IS IN MISTY FIORDS NATIONAL MONUMENT. SOME OF THE EARLY PUBLICATIONS DESCRIBING THIS SITE ARE VAGUE OR AMBIGUOUS [SMITH, 1932 (B824, P 17); 1933 (B836, P.15; B844-A, P. 17); 1934 (B857-A, P. 16; B864-A, P. 16)]. ELLIOTT AND KOCH (1981, P. 9) DESCRIBE GLACIER (BANDED MOUNTAIN?) (LOC. 17A) AND BANDED MOUNTAIN (GLACIER?) (LOC. 17B) SEPARATELY, BUT ASSIGN BOTH PROSPECTS IDENTICAL MAP COORDINATES. THIS RECORD ASSIGNS THEM THE SAME ARDF NUMBER, BUT OTHERWISE FOLLOWS ELLIOTT AND KOCH. EARLY PUBLICATIONS (SMITH, 1932, 1933, 1934) THAT INCLUDE VAGUE REFERENCES TO LODE PROSPECTS ON THE NORTHWEST SIDE OF BANDED MOUNTAIN PROBABLY REFER TO THE GLACIER PROSPECT. THESE PROSPECTS ALSO WERE REFERRED TO AS THE METCALF AND FIN(D)LEY CLAIMS.
Comment (Deposit): THE COUNTRY ROCKS IN THE GENERAL AREA OF THIS SITE ARE GRAYWACKE AND ANDESITIC TUFF AND BRECCIA OF THE JURASSIC OR OLDER MESOZOIC HAZELTON GROUP (BERG AND OTHERS, 1977, P. 15, 40, 41, AND PLATE 1). THE DEPOSIT AT THE GLACIER PROSPECT (BUDDINGTON, 1929, P. 120-121) CONSISTS OF QUARTZ FISSURE VEINS AS MUCH AS ONE FOOT THICK IN GRAYWACKE AND SUBORDINATE ANDESITE TUFF AND BRECCIA THAT IS CUT BY A TERTIARY LAMPROPHYRE DIKE 3 FEET THICK. THE VEINS CONTAIN PYRITE, SMALL AMOUNTS OF PYRRHOTITE AND CHALCOPYRITE, AND RARELY, GALENA. ASSAYS SHOWED 0.04 OZ AU AND 6 OZ AG PER TON AND 3% CU. QUARTZ FLOAT NEAR THE GLACIER PROSPECT THAT MAY HAVE COME FROM THE GLACIER OR SIMILAR VEINS CONTAIN PYRITE, CHALCOPYRITE, AND MOLYBDENITE. IN 1972-73, A U.S. BUREAU OF MINES FIELD TEAM SEARCHED FOR, BUT COULD NOT LOCATE, THIS PROSPECT (BERG AND OTHERS, 1977, P. 41). IN 1972-73, A U. S, BUREAU OF MINES FIELD TEAM (BERG, 1977, P. 132-133) INVESTIGATED A VIVID IRON-STAINED ZONE IN THE CLIFFS AT AN ELEVATION
Comment (Exploration): Status = Inactive
Comment (Location): THE SITE IS IN SECTION 27 ON THE NORTHWEST FLANK OF BANDED MOUNTAIN AT AN ELEVATION OF ABOUT 2700 FEET (ELLIOTT AND KOCH, 1981, P. 9, LOCS. 17A AND 17B) THIS LOCATION IS PROBABLY ACCURATE TO WITHIN ABOUT A HALF MILE. ALSO SEE ADDITIONAL COMMENTS FIELD, BELOW.
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, P.S., 1932, Mineral industry of Alaska in 1929: U.S. Geological Survey Bulletin 824, p. 1-81.
Reference (Deposit): Smith, P.S., 1933, Mineral industry of Alaska in 1930: U.S. Geological Survey Bulletin 836, p. 1-83.
Reference (Deposit): Smith, P.S., 1934, Mineral industry of Alaska in 1932: U.S. Geological Survey Bulletin 857-A, p. 1-91.
Reference (Deposit): Smith, P.S., 1933, Mineral industry of Alaska in 1931, U.S. Geological Survey Bulletin 844-A, p. 1-82.
Reference (Deposit): Smith, P.S., 1934, Mineral industry of Alaska in 1933: U.S. Geological Survey Bulletin 864-A, p. 1-94.
Reference (Deposit): Berg, H. C., Elliott, R.L., Smith, J.G., Pittman, T.L., and Kimball, A. L., 1977, Mineral resources of the Granite Fiords wilderness study area, Alaska, with a section on aeromagnetic data by Andrew Griscom: U.S. Geological Survey Bulletin 1403, 151 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.
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