| Deposit ID | 10025839 |
|---|---|
| MRDS ID | K001804 |
| Record type | Site |
| Current site name | Dixon Mine |
| Related records | 10202648 |
| Geographic coordinates: | -84.40409, 35.51732 (WGS84) |
|---|---|
| Relative position | 0.8 MILE SSW OF BM LHT 1615. |
Political divisions (FIPS codes)
Monroe(county)
Tennessee(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Sweetwater(quadrangle 1:24,000 scale)
Watts Bar Lake(quadrangle 1:100,000 scale)
Chattanooga(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Hiwassee(hydrologic unit)
Middle Tennessee-Hiwassee(hydrologic accounting unit)
Middle Tennessee-Hiwassee(hydrologic subregion)
Tennessee(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Tennessee | Monroe |
| Commodity | Importance |
|---|---|
| Barium-Barite Critical | Primary |
| Materials | Type of material |
|---|---|
| Barite | Ore |
| Chert | Gangue |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Dolomite |
| Rock unit name | Kingsport Formation, Dolomite & Limestone;Mascot Dolomite, Dolomite & Limestone;Clay Residuum |
| Rock description | Kingsport Formation, Dolomite & Limestone;Mascot Dolomite, Dolomite & Limestone;Clay Residuum |
| (1) | -84.40409, 35.51732 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Northeast-Trending Strike Belts |
| General form | IRREGULAR |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | K001804 |
MAHER, S.W., 1970, BARITE RESOURCES OF TENNESSEE: TENN. DIVISION OF GEOLOGY, REPORT OF INVESTIGATIONS NO. 28, 40 P
1970 COMPILE MAHER, S.W., TENN. DIV. GEOL., REPOR
| Subject category | Comment text |
|---|---|
| Deposit | ECONOMICALLY MINABLE BARITE DEPOSITS OCCUR IN THE CLAY RESIDUUM OVERLYING THE KNOX GROUP. MINERALIZED BRECCIATED ZONES IN THE UNDERLYING BEDROCK HAVE NOT BEEN MINED FOR BARITE BECAUSE OF INSUFFICIENT GRADE OF MATERIAL. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1974 | Hale, Robin C. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.