Deposit ID | 10002938 |
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MRDS ID | A015431 |
Record type | Site |
Current site name | Cleary Hill Mine |
Alternate or previous names | Rhoads-Hall Mine |
Related records | 10111975 |
Geographic coordinates: | -147.43768, 65.0669 (WGS84) |
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Relative position | 25 MILES NE OF FAIRBANKS BY ROAD. |
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Country | State |
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United States | Alaska |
Commodity | Importance |
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Gold | Primary |
Antimony | Primary |
Silver | Secondary |
Copper | Tertiary |
Lead | Tertiary |
Tin | Tertiary |
Tungsten | Tertiary |
Zinc | Tertiary |
Materials | Type of material |
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Cassiterite | Ore |
Chalcopyrite | Ore |
Galena | Ore |
Gold | Ore |
Jamesonite | Ore |
Scheelite | Ore |
Sphalerite | Ore |
Stibnite | Ore |
Pyrite | Gangue |
Result | AVERAGE FINENESS 818 PARTS AU AND 169 PARTS AG PER THOUSAND. |
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Host or associated | Host |
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Rock type | Metamorphic Rock > Schist |
(1) | -147.43768, 65.0669 |
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Strike | N 75 W |
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Dip | 45 TO 63 S |
Development status | Past Producer |
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Commodity type | Metallic |
Deposit size | Small |
Significant | No |
Discoverer | Rhodes And Hall |
Year of first production | 1909 |
District name | Fairbanks |
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Ownership category | State |
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Type | Owner |
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Owner | Alaska Gold Mines Co. |
Agency | Database name | Acronym | Record ID | Notes |
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USGS | Mineral Resources Data System | MRDS | A015431 |
USGS MF-413 (A-1), LOC. 39
USGS BULL 525, P. 177-180
USGS BULL. 849-B, P. 93-96
Subject category | Comment text |
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Deposit | LODE IS GOLD, STIBNITE, ARSENOPYRITE, PYRITE, SPHALERITE, GALENA, CHALCOPYRITE, JAMESONITE, COVELLITE, AND SCHEELITE BEARING VEINS CUTTING SCHIST IN FAULT ZONE. GOLD INTRODUCED AT TWO DIFFERENT STAGES; FIRST WITH QUARTZ AND SECOND WITH SULFIDES. GOLD IRREGULARLY DISTRIBUTED THROUGH VEIN MATERIAL IN VISIBLE PARTICLES UNCOMBINED WITH OTHER ELEMENTS. IN SOME PLACES THE VEIN IS RICHEST ADJACENT TO WALLS; IN OTHER PLACES IT IS RICHEST IN CENTER. SULPHIDE RICH PORTIONS OF VEINS ALSO CONTAIN GOLD. PRINCIPAL VEIN AVERAGES ABOUT 1 FT. IN THICKNESS; MAXIMUM THICKNESS 3 FT. SMALLER PARALLEL VEINS IN BOTH HANGING AND FOOTWALLS. AT LEAST ONE INTERSECTING VEIN IS LARGELY STIBNITE. THIN LIMESTONE BEDS IN SCHIST CONTAIN SCHEELITE. CASSITERITE IN WEATHERED VEIN MATERIAL. |
Type | Date | Name | Affiliation | Comment |
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Reporter | 01-JUN-1987 | Powers, M.T. (Huber, D.F.) | U.S. Geological Survey |