| Deposit ID | 10025702 |
|---|---|
| MRDS ID | K001627 |
| Record type | Site |
| Current site name | Washburn Station Occurrence |
| Related records | 10178464 |
| Geographic coordinates: | -83.59517, 36.30148 (WGS84) |
|---|---|
| Relative position | RAILROAD CUT, 0.8 MI. N. OF WASHBURN, TENN. |
Political divisions (FIPS codes)
Grainger(county)
Tennessee(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Dutch Valley(quadrangle 1:24,000 scale)
Morristown(quadrangle 1:100,000 scale)
Johnson City(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Clinch, Tennessee, Virginia(hydrologic unit)
Upper Tennessee(hydrologic accounting unit)
Upper Tennessee(hydrologic subregion)
Tennessee(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Tennessee | Grainger |
| Commodity | Importance |
|---|---|
| Zinc Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Sphalerite | Ore |
| Chert | Gangue |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Dolomite | ||
| Rock unit name | Knox Group, Dolomite | ||
| Rock description | Knox Group, Dolomite | ||
| |||
| (1) | -83.59517, 36.30148 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Northeast-Trending Strike Belt |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| District name | Copper Ridge Zinc District |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | K001627 |
SECRIST, M.H., 1924, ZINC DEPOSITS OF EAST TENNESSEE: TENN. DIV. GEOL., BULL. 31, 165 P.
MAHER, S.W., 1958, THE ZINC INDUSTRY OF TENNESSEE: TENN. DIV. GEOL., INF. CIR. NO. 6, 28 P.
1924 GEOLMAP SECRIST, M.H., TENN. DIV. GEOL., REPORT
1958 COMPILE MAHER, S.W., TENN. DIV. GEOL., REPORT
SECRIST, M.H., 1924, TENN. DIV. GEOL. BULL. 31.
| Subject category | Comment text |
|---|---|
| Deposit | SECRIST (1924) NOTES THAT TWO SMALL OUTCROPS OF SPHALERITE WERE OBSERVED, STRATIGRAPHICALLY 35 FEET APART. "THE ORE CONSISTS OF SMALL MASSES AND VEINLETS OF SPHALERITE ASSOCIATED WITH GANGUE DOLOMITE AND CHERT IN A TIGHT, UNBRECCIATED COUNTRY ROCK. UPPER EXPOSURE IS 700 FEET STRATIGRAPHICALLY BELOW THE TOP OF THE KNOX. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-OCT-1973 | Hale, Robin C. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.