| Deposit ID | 10000839 |
|---|---|
| MRDS ID | A011492 |
| Record type | Site |
| Current site name | Bernard Mountain Prospect |
| Alternate or previous names | Red Mountain |
| Related records | 10258792 |
| Geographic coordinates: | -145.14423, 61.57796 (WGS84) |
|---|---|
| Location accuracy | 2000(meters) |
| Relative position | N SLOPE OF BERNARD MOUNTAIN |
Political divisions (FIPS codes)
Valdez-Cordova(Census area)
Alaska(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Valdez C-4(quadrangle 1:63,360 scale)
Valdez NE(quadrangle 1:100,000 scale)
Valdez C(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Middle Copper River(hydrologic unit)
Copper River(hydrologic accounting unit)
South Central Alaska(hydrologic subregion)
Alaska(hydrologic region)
| Country | State |
|---|---|
| United States | Alaska |
| Commodity | Importance |
|---|---|
| Chromium Critical | Primary |
| Nickel Critical | Tertiary |
| Platinum Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Chromite | Ore |
| Result | RANGE: 1500 PPM TO MORE THAN 5000 PPM CR, 1500 PPM TO 5000 PPM NI, MEAN: 5000 PPM CR, 2000 PPM NI, MAXIMUM PT CONCENTRATION .200 PPM, AVERAGE PT CONCENTRATION .023 PPM, HOFFMANN, BARRY, 1974, UNIV. OF ALASKA M. S. THESIS, P. 46, 50 |
|---|---|
| Result | TABLE CONCENTRATES FROM COMPOSITE OF CUT SAMPLES CONTAINED 48% CHROMITE WITH CR: FE RATIO OF 2.7, USBM IC 8626, P. 18 |
| Host or associated | Associated |
|---|---|
| Rock type | Metamorphic Rock > Gneiss |
| Rock unit name | Streina Formation;Streina Formation;Streina Formation;Streina Formation;Streina Formation;Streina Formation;;; |
| Rock description | Streina Formation;Streina Formation;Streina Formation;Streina Formation;Streina Formation;Streina Formation;;; |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Ultramafic Intrusive Rock > Hornblendite |
| Rock unit name | Bernard Mountain Ultramafic Body;Bernard Mountain Ultramafic Body;Bernard Mountain Ultramafic Body;Bernard Mountain Ultramafic Body |
| Rock description | Bernard Mountain Ultramafic Body;Bernard Mountain Ultramafic Body;Bernard Mountain Ultramafic Body;Bernard Mountain Ultramafic Body |
| (1) | -145.14423, 61.57796 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Area Cut By Three Major Faults; Bernard Mt. Fault, Kimball Pass Fault And One Cross Fault |
| General form | LENSE |
|---|---|
| Thickness | 0.15M |
| Development status | Prospect |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Tonsina |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | A011492 |
USGS BULL 1246, P. 49, 52
ADGGS GC 15, P. 2, 4
USBM IC 8626, P. 18
HOFFMANN, BARRY, 1974, GEOLOGY OF THE BERNARD MOUNTAIN AREA, TONSINA, ALASKA: COLLEGE, ALASKA, UNIVERSITY OF ALASKA M. S. THESIS, 68 P.
USGS OFR 78-1-E, P. 19
USGS MF-438, LOC. 51
USGS OFR 80-892B, LOC. 42
BAG-OFR-80-892B-42
| Subject category | Comment text |
|---|---|
| Deposit | LAYERS, LENSES AND DISSEMINATIONS OF CHROMITE IN DUNITE AND ASSOCIATED ULTRAMAFICS; CHROMITE OCCURS AS DISSEMINATED GRAINS THAT FORM 0.5 TO 1% OF DUNITE, OR AS CONCENTRATIONS OF FROM 2 TO 40% CHROMITE IN TRAINS SEVERAL GRAINS WIDE, MASSIVE LENSES, OR LAYERS UP TO 6 IN THICK |
| Deposit | DESPITE PROXIMITY TO RICHARDSON HIGHWAY, SUFFICIENT QUANTITIES OF ORE GRADE CHROMITE HAVE NOT BEEN PROVEN AND AREA REMAINS UNECONOMIC; MIGHT BE MINED UNDER VERY UNUSUAL ECONOMIC CONDITIONS; SEE ALSO: DUST MOUNTAIN, SHEEP MOUNTAIN ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1985 | Leonard, Kenneth R. (Elliott, R. L.) | U.S. Geological Survey | PARSED DATA INTO WORKINGS AND ORE BODY MULTIVALUED FIELDS |
| Editor | 14-APR-1994 | Mosier, Dan | U.S. Geological Survey | |
| Editor | 30-MAY-1995 | Waller, Nichelle (Mosier, Dan) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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