| Deposit ID | 10110609 |
|---|---|
| MRDS ID | W022867 |
| Record type | Site |
| Current site name | East Tennessee Mine |
| Related records | 10178252 |
| Geographic coordinates: | -84.35074, 35.04455 (WGS84) |
|---|---|
| Elevation | 549 |
| Relative position | 8600 FT. NORTH 48 DEG. EAST OF THE U.S. RT. 64 - TN. RT. 68 INTERCHANGE |
Political divisions (FIPS codes)
Polk(county)
Tennessee(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Isabella(quadrangle 1:24,000 scale)
Cleveland(quadrangle 1:100,000 scale)
Chattanooga(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Ocoee(hydrologic unit)
Middle Tennessee-Hiwassee(hydrologic accounting unit)
Middle Tennessee-Hiwassee(hydrologic subregion)
Tennessee(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Tennessee | Polk |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Iron | Primary |
| Sulfur | Primary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Magnetite | Ore |
| Pyrite | Ore |
| Pyrrhotite | Ore |
| Sphalerite | Ore |
| Calcite | Gangue |
| Diopside | Gangue |
| Tremolite | Gangue |
| (1) | -84.35074, 35.04455 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Nw Limb Of The Burra Anticline |
| General form | LENTICULAR, TABULAR |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Both |
| Significant | No |
| District name | Ducktown Copper District |
|---|
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | Cities Service Co.{Copperhill, Tenn., 37317 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W022867 |
MAGEE, MAURICE, 1968, GEOLOGY AND ORE DEPOSITS OF THE DUCKTOWN DISTRICT, TENNESSEE: IN RIDGE, J.D., ED., ORE DEPOSITS OF THE UNITED STATES, 1933-1967 (GRATON-SALES VOLUME), V. 1, AM. INST. MINING, METALL., AND PETROLEUM ENGINEERS, P. 207-241
1968 DIREXPL MAGEE, IN GRATON-SALES VOLUM
MAGEE, 1968, P. 228, 231.
| Subject category | Comment text |
|---|---|
| Deposit | THE SULFIDES CONTAINED MORE CHALCOPYRITE THAN WAS TYPICAL OF THE DISTRICT, AND WERE DISSEMINATED IN A MATRIX OF SILICATE MINERALS AND SCHISTS. THE SUPERGENE ZONE EXTENDED DEEPER THAN 200 FEET. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1975 | U.S. Bureau Of Mines | U.S. Bureau of Mines | |
| Updater | 01-SEP-1978 | Geraci, Philip J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.