| Deposit ID | 10025807 |
|---|---|
| MRDS ID | K001763 |
| Record type | Site |
| Current site name | Holt Mine |
| Related records | 10251425 |
| Geographic coordinates: | -86.7061, 35.95149 (WGS84) |
|---|---|
| Relative position | 2.25 MILES WEST OF NOLENSVILLE |
Political divisions (FIPS codes)
Williamson(county)
Tennessee(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Nolensville(quadrangle 1:24,000 scale)
Murfreesboro(quadrangle 1:100,000 scale)
Columbia(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Lower Cumberland-Sycamore(hydrologic unit)
Lower Cumberland(hydrologic accounting unit)
Cumberland(hydrologic subregion)
Ohio(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Tennessee | Williamson |
| Commodity | Importance |
|---|---|
| Lead | Primary |
| Zinc Critical | Tertiary |
| Fluorine-Fluorite Critical | Tertiary |
| Barium-Barite Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Barite | Ore |
| Fluorite | Ore |
| Galena | Ore |
| Sphalerite | Ore |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||||
| Rock unit name | Carters Limestone | ||||
| Rock description | Carters Limestone | ||||
| |||||
| (1) | -86.7061, 35.95149 |
|---|
| Strike | N 40 E |
|---|---|
| Dip | VERT. |
| Length | 792.48M |
| Width | 0.55M |
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Significant | No |
| Discoverer | Indians |
| Production years | 1914 |
| District name | Central Tennessee Ba-F-Pb-Zn District |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | K001763 |
JEWELL, W.B., 1947, BARITE, FLUORITE, GALENA, SPHALERITE VEINS OF MIDDLE TENNESSEE: TENNESSEE DIV. GEOLOGY BULL. 51, 114 P
1947 RECON TENNESSEE DIV. GEOLOGY, REPOR
JEWELL, W.B., 1947, TENN. DIV. GEOLOGY, BULL. 51
| Subject category | Comment text |
|---|---|
| Deposit | SOME OF VEIN MATERIAL IS RYTHMICALLY BANDED, EITHER PARALLEL TO WALLS OF VEIN, CONCENTRICALLY IN FILLED CAVITIES OR AROUND LIMESTONE FRAGMENTS. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1974 | Fagan, James M. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.