| Deposit ID | 10025565 |
|---|---|
| MRDS ID | K001462 |
| Record type | Site |
| Current site name | Fortner Prospect, Southern |
| Related records | 10251244 |
| Geographic coordinates: | -83.71128, 36.45202 (WGS84) |
|---|
Political divisions (FIPS codes)
Claiborne(county)
Tennessee(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Clouds(quadrangle 1:24,000 scale)
Morristown(quadrangle 1:100,000 scale)
Johnson City(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Powell(hydrologic unit)
Upper Tennessee(hydrologic accounting unit)
Upper Tennessee(hydrologic subregion)
Tennessee(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Tennessee | Claiborne |
| Commodity | Importance |
|---|---|
| Lead | Tertiary |
| Materials | Type of material |
|---|---|
| Galena | Ore |
| Result | GALENA REPORTEDLY SPARSE IN WALLS OF ADIT. |
|---|
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Dolomite | ||||
| Rock unit name | Copper Ridge Dolomite; Massive, Knotty, Light-Gray Dolomite | ||||
| Rock description | Copper Ridge Dolomite; Massive, Knotty, Light-Gray Dolomite | ||||
| |||||
| (1) | -83.71128, 36.45202 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Northeast-Trending Powell River Anticline |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discovery year | 1918 |
| Discoverer | American Zinc Co. |
| Type of workings | Underground |
|---|---|
| Length | 3.05M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | K001462 |
BROKAW, A. L., RODGERS, JOHN, KENT, D. F., LAURENCE, R. A., AND BEHRE, C. H. JR., 1966, GEOLOGY AND MINERAL DEPOSITS OF THE POWELL RIVER AREA, CLAIBORNE AND UNION COUNTIES, TENNESSEE: USGS BULL. 1222-C, 55 P
1966 GEOLMAP BROKAW, A.L., ET AL; REPOR
BROKAW, A.L., ET AL, 1966, USGS BULL. 1222-C
| Subject category | Comment text |
|---|---|
| Deposit | 190 FT. BELOW BASE OF CHEPULTEPEC DOLOMITE. GALENA IS MORE EVIDENT IN WEATHERED ROCK ON EITHER SIDE OF ADIT THAN IN FRESH ROCK EXPOSED ALONG ADIT WALLS. SPHALERITE APPARENTLY ABSENT, NONE OBSERVED. BROKAW (1966) CONSIDERS MINERALIZED BED AT THIS LOCALITY THE SAME AS THAT AT F. M. DAY AND W. P. DAY PROSPECTS ELSEWHERE IN THE DISTRICT. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1973 | Hale, Robin C. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.