| Deposit ID | 10063144 |
|---|---|
| MRDS ID | TC36785 |
| Record type | Site |
| Current site name | Bowie Hill Deposit |
| Related records | 10251677 |
| Geographic coordinates: | -94.17799, 33.22376 (WGS84) |
|---|---|
| Elevation | 134 |
| Relative position | 7 MI N OF ATLANTA. |
Political divisions (FIPS codes)
Cass(county)
Texas(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Atlanta North(quadrangle 1:24,000 scale)
Texarkana(quadrangle 1:100,000 scale)
Texarkana(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Cross Bayou(hydrologic unit)
Big Cypress-Sulphur(hydrologic accounting unit)
Red-Sulphur(hydrologic subregion)
Arkansas-White-Red(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Texas | Cass |
| Commodity | Importance |
|---|---|
| Iron | Primary |
| Materials | Type of material |
|---|---|
| Goethite | Ore |
| Hematite | Ore |
| Siderite | Ore |
| Clay | Gangue |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone | ||||
| Rock unit name | Weches Member, Mount Selman Formation | ||||
| Rock description | Weches Mbr, Mount Selman Formation | ||||
| |||||
| (1) | -94.17799, 33.22376 |
|---|
| General form | BLANKET |
|---|---|
| Thickness | 10.67M |
| Length | 2011.63M |
| Width | 1206.98M |
| Depth to top | 0M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discovery year | 1864 |
| Production years | 1864-65; 1910'S |
| District name | North Basin East Texas |
|---|
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | Texas Iron Assoc. ; Sulphur Fork Iron Co. |
| First year | 1863 |
| Last year | 1865 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC36785 |
USGS B 902, P. 78-84
CIMRI
(1) USGS B 902, P. 83.
| Subject category | Comment text |
|---|---|
| Deposit | LENSES, BEDS AND CONCRETIONARY MASSES OF LIMONITE WITHIN OOLITIC GLAUCONITE SANDSTONE. COMMERCIAL ORE AVERAGES 3 FT THICK AT AN AVERAGE DEPTH OF 8 FT. TWO OUTLYING DEPOSITS, 0.5 MI S OF BOWIE HILL, CONSIST OF ABOUT 10 AC WITH ABOUT 1 FT THICKNESS ORE NEAR SURFACE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1993 | Long, Keith R. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.