| Deposit ID | 10013203 |
|---|---|
| MRDS ID | D009357 |
| Record type | Site |
| Current site name | A.E. Jones Claim |
| Alternate or previous names | Taylor Soda Springs |
| Related records | 10288378 |
| Geographic coordinates: | -105.5253, 38.59529 (WGS84) |
|---|---|
| Elevation | 2475 |
| Relative position | 11 MILES N 45 W OF PARKDALE |
Political divisions (FIPS codes)
Fremont(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Hall Gulch(quadrangle 1:24,000 scale)
Pikes Peak(quadrangle 1:100,000 scale)
Pueblo(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Arkansas Headwaters(hydrologic unit)
Upper Arkansas(hydrologic accounting unit)
Upper Arkansas(hydrologic subregion)
Arkansas-White-Red(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Colorado | Fremont |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 017S | 073W | 03 | SW OF NW OF NW | Colorado |
| Commodity | Importance |
|---|---|
| Uranium | Primary |
| Materials | Type of material |
|---|---|
| Coffinite | Ore |
| Uraninite | Ore |
| Hematite | Gangue |
| Limonite | Gangue |
| Result | CHIP AND GRAB SAMPLES RANGE FROM 33 TO 100 TIMES BACKGROUND RADIOACTIVITY. RADIOACTIVITY IS MORE CONCENTRATED IN "RED STREAKS" NEAR SPRINGS. WATER ANALYSES SHOW 960 PPB URANIUM, 460 PC/L RADIUM AND 13,000 PC/L RADON |
|---|
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||||
| Rock unit name | Wall Mountain Tuff Was Probable Principal Source Of Uranium | ||||||
| Rock description | Wall Mountain Tuff Was Probable Principal Source Of Uranium | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Rock unit name | Calcareous Tufa;Echo Park Formation Is Source Of Mineral Water |
| Rock description | Calcareous Tufa;Echo Park Formation Is Source Of Mineral Water |
| (1) | -105.5253, 38.59529 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Thirtynine Mile Volcanic Field, Currant Creek Basin |
| Type of structure | Local |
| Structure description | Echo Park Graben, Paleovalleys |
| General form | TABULAR, PODS |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Tallahassee Creek |
|---|
| Ownership category | Private |
|---|
| Type of workings | Unknown |
|---|---|
| Overall depth | 1.22M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D009357 | |
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0080430022 |
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.
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1982 | Collins, Donna B. | Colorado Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.