Glacier

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

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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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