| Deposit ID | 10013507 |
|---|---|
| MRDS ID | D009851 |
| Record type | Site |
| Current site name | Four Corners Mine |
| Alternate or previous names | Pallaoro Lease, Morrison Mine |
| Geographic coordinates: | -105.17058, 39.63582 (WGS84) |
|---|---|
| Elevation | 1780 |
| Relative position | 1.7 MILES S 40 E FROM MORRISON |
Political divisions (FIPS codes)
Jefferson(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Morrison(quadrangle 1:24,000 scale)
Denver West(quadrangle 1:100,000 scale)
Denver(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper South Platte(hydrologic unit)
South Platte(hydrologic accounting unit)
South Platte(hydrologic subregion)
Missouri(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Colorado | Jefferson |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 005S | 070W | 12 | SW OF NE OF NE | Colorado |
| Commodity | Importance |
|---|---|
| Uranium | Primary |
| Vanadium Critical | Secondary |
| Molybdenum | Tertiary |
| Materials | Type of material |
|---|---|
| Uraninite | Ore |
| Ilsemannite | Gangue |
| Pyrite | Gangue |
| Result | PRINCIPAL ORE GRADES RANGED FROM 0.19 TO 0.23% U308, OVERALL 0.19% U308 |
|---|
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone | ||||
| Rock unit name | South Platte Formation | ||||
| Rock description | South Platte Formation | ||||
| |||||
| (1) | -105.17058, 39.63582 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Denver Basin, Front Range Uplift |
| Type of structure | Local |
| Structure description | Golden Fault, Damming Fault |
| General form | WEDGE, LENTICULAR |
|---|---|
| Thickness | 6.1M |
| Length | 18.29M |
| Depth to bottom | 25.91M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1954 |
| Discoverer | S.N. Strauss And R.W. Strauss |
| Year of first production | 1955 |
| Year of last production | 1960 |
| District name | Foothill District |
|---|
| Ownership category | Private |
|---|
| Year | 1955 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^0.19% U308 | ||||||||||||||
| |||||||||||||||
| Year | 1956 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^0.23% U308 | ||||||||||||||
| |||||||||||||||
| Year | 1960 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1955-1960 | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^0.19% U308 | ||||||||||||||
| |||||||||||||||
| Type of workings | Unknown |
|---|---|
| Length | 114.3M |
| Overall depth | 22.86M |
| Overall length | 91.44M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D009851 |
SCOTT, G.R., 1972, GEOLOGIC MAP OF THE MORRISON QUADRANGLE, JEFFERSON COUNTY, COLORADO: USGS MAP I-790-A
RICHTER, D.H., 1964, FOUR CORNERS URANIUM MINE, IN SIMS, P.K., AND SHERIDAN, D.M., GEOLOGY OF URANIUM DEPOSITS IN FRONT RANGE, COLORADO: USGS BULL. 1159, P. 102-103, PL. 5.
RICHTER, 1964, P. 102-103; NELSON-MOORE AND OTHERS (1978), P. 194
| Subject category | Comment text |
|---|---|
| Deposit | URANINITE AND URANIFEROUS ASPHALT (PROBABLY RELATED TO OIL SEEPS IN AREA) COAT SAND GRAINS AND FILL INTERSTICES IN SANDSTONE AND TO SMALL EXTENT FILL FRACTURES IN DAMMING FAULT ZONE. SOME ORE IS SPHEROIDAL AND COMPOSED OF CONCENTRIC BANDS OF URANINITE AROUND PYRITE GRAIN. ORE BODIES ARE ELONGATED, THIN, DISCONTINUOUS WEDGES AND LENSES PARALLEL TO INTERSECTION OF DAMMING FAULT AND BEDDING. MOST MINED ORE CAME FROM HANGING WALL OF FAULT ALTHO SOME FOUND IN FOOTWALL. GOLDSTEIN (1957) BELIEVED URANIUM TO BE OF PRIMARY ORIGIN AND WAS PRECIPITATED FROM ASCENDING HYDROTHERMAL SOLUTIONS ALONG DAMMING FAULT AT ZONES OF FAVORABLE SANDSTONE PERMEABILITY. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1983 | Schwochow, Stephen D. | Colorado Geological Survey | |
| Updater | 01-MAY-1993 | Spanski, Gregory T. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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