| Lat / long: | 38.59529, -105.5253 |
| Primary: | Uranium |
| Ore: | Coffinite, Uraninite |
| Gangue: | Hematite, Limonite |
| Orebody form: | TABULAR, PODS |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Calcareous Tufa;Echo Park Formation Is Source Of Mineral Water |
| Host type: | Carbonate,Limestone |
| Associated rock: | Wall Mountain Tuff Was Probable Principal Source Of Uranium |
| Associated type: | Rhyolite |
| Structure: | Thirtynine Mile Volcanic Field, Currant Creek Basin, Echo Park Graben, Paleovalleys |
| Tectonic: | Central Cordillera (Southern Rocky Mountains) |
| Alteration processes: | Oxidation; Alteration Of Feldspar To Clay; |
| MRDS | D009357 |
| DEP | 10013203 |
| Reference | {Deposit:: NELSON-MOORE, J.L., COLLINS, D.B. AND HORNBAKER, A.L., 1978, RADIOACTIVE MINERAL OCCURRENCES OF COLORADO AND BIBLIOGRAPHY: CGS BULLETIN 40, P. 144.}{Deposit:: EPIS, R.C., WOBUS, R.A. AND SCOTT, G.R., 1979, GEOLOGIC MAP OF THE BLACK MOUNTAIN QUADRANGLE, FREMONT AND PARK COUNTIES, COLORADO: USGS MAP I-1195, 1:62,500.}{Deposit:: DICKINSON, K.A., 1981, GEOLOGIC CONTROLS OF URANIUM MINERALIZATION IN THE TALLAHASSEE CREEK URANIUM DISTRICT, FREMONT COUNTY, COLORADO: THE MOUNTAIN GEOLOGIST, V. 18, NO. 4, P. 88-94.} |
| Reporter | Collins, Donna B. |