| Deposit ID | 10085820 |
|---|---|
| MRDS ID | W701477 |
| Record type | Site |
| Current site name | Mammoth Prospect |
| Geographic coordinates: | -104.80495, 30.44713 (WGS84) |
|---|---|
| Relative position | 40 MI (65 KM) S OF VAN HORN |
Political divisions (FIPS codes)
Presidio(county)
Texas(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Quinn Creek(quadrangle 1:24,000 scale)
Marfa(quadrangle 1:100,000 scale)
Marfa(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Cibolo-Red Light(hydrologic unit)
Rio Grande-Amistad(hydrologic accounting unit)
Rio Grande-Amistad(hydrologic subregion)
Rio Grande(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Texas | Presidio |
| Commodity | Importance |
|---|---|
| Uranium | Primary |
| Materials | Type of material |
|---|---|
| Carnotite | Ore |
| Calcite | Gangue |
| Chalcedony | Gangue |
| Feldspar | Gangue |
| Opal | Gangue |
| Quartz | Gangue |
| Model code | 155 |
|---|---|
| USGS model code | 25f |
| Deposit model name | Volcanogenic U |
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||||
| Rock unit name | Buckshot Ignimbrite | ||||||
| Rock description | Buckshot Ignimbrite | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| (1) | -104.80495, 30.44713 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Ownership category | Private |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W701477 |
PRICE, J. G., HENRY, C. D., AND STANDEN, A. R., 1983, ANNOTATED BIBLIOGRAPHY OF MINERAL DEPOSITS IN TRANS-PECOS TEXAS: BUREAU OF ECONOMIC GEOLOGY (TEXAS), MINERAL RESOURCE CIRCULAR NO. 73, 108 P
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | HENRY AND OTHERS (1980) NOTED THAT BETA-URANOPHANE OCCURS IN CAVITIES IN DEVITRIFICATION SPHERES, IN FRACTURES IN ROCK FRAGMENTS, AND IN FRACTURES IN THE BUCKSHOT IGNIMBRITE. NYE (1957) PROPOSED THREE MODES OF ORIGIN: (1) CONCENTRATION OF URANIUM IN VESICLES BY LATE-STAGE VOLATILE COMPONENTS OF THE MAGMA, (2) GROUNDWATER LEACHING FROM THE IGNIMBRITE AND OVERLYING TUFFACEOUS SEDIMENTS AND RECONCENTRATION IN THE IGNIMBRITE, AND (3) HYDROTHERMAL MINERALIZATION. HENRY AND OTHERS (1980) AND HENRY AND DUEX (1981) SUGGESTED THAT HYDROGEN SULFIDE-RICH WATERS FROM DEPTH ENTERED THE BUCKSHOT IGNIMBRITE AND PRECIPITATED PYRITE BEFORE URANIUM DEPOSITION BY AN OXIDATION-REDUCTION MECHANISM. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAR-1991 | Paidakovich, Matthew E. | U.S. Geological Survey | |
| Updater | 01-MAR-1993 | Long, Keith R. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.