| Deposit ID | 10091865 |
|---|---|
| MRDS ID | K001625 |
| Record type | Site |
| Current site name | W.H. Green Prospect |
| Related records | 10299037 |
| Point of reference | Centroid |
|---|---|
| Geographic coordinates: | -83.22524, 36.52195 (WGS84) |
| Relative position | Original record had no coordinates, so this was plotted to the middle of the state/county area. |
Political divisions (FIPS codes)
Hancock(county)
Tennessee(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Sneedville(quadrangle 1:24,000 scale)
Middlesboro(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 | Hancock |
| Commodity | Importance |
|---|---|
| Zinc Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Sphalerite | Ore |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Dolomite | ||||
| Rock unit name | Rome Formation, Dolomite | ||||
| Rock description | Rome Formation, Dolomite | ||||
| |||||
| Centroid (1) | -83.22524, 36.52195 |
|---|
| Thickness | 0.91M |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discovery year | 1919 |
| Type of workings | Surface |
|---|---|
| Overall length | 4.57M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | K001625 |
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
| Subject category | Comment text |
|---|---|
| Deposit | FINELY DISSEMINATED SPHALERITE OCCURS IN TIGHT, UNBRECCIATED COUNTRY ROCK. MINERALIZED ZONE IS PARALLEL TO BEDDING AND RANGES FROM 1 TO 3 FEET IN THICKNESS. TWO PROMINENT SETS OF JOINTS STRIKE N 45 DEG W AND N 60 DEG W, BUT ARE APPARENTLY UNRELATED TO MINERALIZATION. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-OCT-73 | Hale, Robin C. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.