| Deposit ID | 10014254 |
|---|---|
| MRDS ID | D010948 |
| Record type | Site |
| Current site name | White Spar Mine |
| Alternate or previous names | Patented Claims: White Spar, MS 4819, New Discovery, MS 4819 |
| Geographic coordinates: | -108.04621, 38.01861 (WGS84) |
|---|---|
| Elevation | 2377 |
| Relative position | 13.7 MILES N 67 W FROM TELLURIDE |
Political divisions (FIPS codes)
San Miguel(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Placerville(quadrangle 1:24,000 scale)
Nucla(quadrangle 1:100,000 scale)
Moab(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
San Miguel(hydrologic unit)
Upper Colorado-Dolores(hydrologic accounting unit)
Upper Colorado-Dolores(hydrologic subregion)
Upper Colorado(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Colorado | San Miguel |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| New Mexico | 044N | 011W | 35 | S2 OF S2 | Colorado |
| Commodity | Importance |
|---|---|
| Uranium | Primary |
| Copper | Primary |
| Vanadium Critical | Secondary |
| Materials | Type of material |
|---|---|
| Chalcocite | Ore |
| Chalcopyrite | Ore |
| Barite | Gangue |
| Calcite | Gangue |
| Result | MOREHOUSE (1951) REPORTED ANALYSES OF CHANNEL SAMPLES OF VEIN MATERIAL: SAMPLE 12052, 0.05% U308 (RADIOMETRIC), 0.04% U308 (CHEMICAL) |
|---|---|
| Result | SAMPLE 12051, 0.13% U308 (RADIOMETRIC), 0.15% U308 (CHEMICAL) |
| Result | SAMPLE 12068, 0.06% U308 (RADIOMETRIC), 0.06% U308 (CHEMICAL), 0.15% V205. |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Siltstone | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone |
| Rock unit name | Cutler Formation;Dolores Formation |
| Rock description | Cutler Formation;Dolores Formation |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Conglomerate |
| (1) | -108.04621, 38.01861 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Paradox Basin, Uncompahgre Uplift, San Juan Volcanic Field, San Miguel Mtns |
| Type of structure | Local |
| Structure description | Black King Fault |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1887 |
| Discoverer | Ephraim Flangher And Others (Claimants) |
| District name | Lower San Miguel District |
|---|
| Ownership category | Private |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D010948 | |
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0081130337 |
FISCHER, R.P., AND OTHERS, 1947, VANADIUM DEPOSITS NEAR PLACERVILLE, SAN MIGUEL COUNTY, COLORADO: COLORADO SCI. SOC. PROC., V. 15, NO. 3, P. 117-146.
BUSH, A.L., AND OTHERS, 1959, AREAL GEOLOGY OF THE PLACERVILLE QUADRANGLE, SAN MIGUEL COUNTY, COLORADO: USGS BULL 1072-E.
MOREHOUSE, G.E., 1951, INVESTIGATION OF THUCHOLITE DEPOSITS NEAR PLACERVILLE, COLORADO: AEC RMO-910, P. 9, 13.
WILMARTH, V.R., 1953, PLACERVILLE HYDROCARBONS, COLORADO, IN SEARCH FOR AND GEOLOGY OF RADIOACTIVE DEPOSITS: AEC TEI-330, P. 107-108.
BLM MINERAL SURVEY MS 4819
| Subject category | Comment text |
|---|---|
| Deposit | MINE DEVELOPED ON SE EXTENSION OF BLACK KING FAULT, ONE OF PRINCIPAL FAULTS IN NW-TRENDING SYSTEM CHARACTERISTIC OF DISTRICT. THREE SEGMENTS OF FAULT TREND ABOUT N 20 W AND N 50 W, JOINING TO FORM CONTINUATION OF MAIN FAULT AT ABOUT N 80 W. MAIN FAULT AND SEGMENTS ALL DOWNTHROWN ON NE AND CUT CUTLER AND DOLORES FM RED BEDS. ON RIDGE NORTH OF MINE, CLASTIC DIKE TRENDS GENERALLY N 80 TO 90 W. WHITE SPAR SHOWS FEWER SULFIDES AND LESS WALLROCK ALTERATION THAN BLACK KING, BUT BOTH ARE PROBABLY GENETICALLY RELATED. URANIUM OCCURS AS SCATTERED GRAINS OF URANINITE AND COFFINITE AND POSSIBLY AS ORGANIC COMPLEX DISSEMINATED THROUGH HARDENED PETROLIFEROUS HYDROCARBON OR ASPHALTIC MATERIAL (TERMED THUCHOLITE). ASPHALT OCCURS IN FAULT ZONE, AS FRACTURE FILLINGS, AND DISSEMINATION IN SEDIMENTARY ROCK. RADIOACTIVITY SEEMS MORE CONCENTRATED IN SHINY LUSTROUS HYDROCARBON THAN IN SOOTY VARIETY. GENERAL PARAGENESIS: CALCITE, BARITE, PYRITE, HYDROCARBONS, SULFIDES (PYRITE, CHALCOPYRITE, BORNITE, |
| Deposit | ARGENTIFEROUS TETRAHEDRITE, GALENA, SPHALERITE) (GENERAL SEQUENCE FORAREA AS DETERMINED BY WILMARTH, 1953). |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-NOV-1983 | Schwochow, Stephen D. | Colorado Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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