Unnamed Uranium Occurrence

Occurrence in Crowley county in Colorado, United States with commodity Uranium
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Public Land Survey System information
  6. Commodities
  7. Materials information
  8. Alteration
  9. Host and associated rocks
  10. Nearby scientific data
  11. Geologic structures
  12. Ore body information
  13. Controls for ore emplacement
  14. Economic information about the deposit and operations
  15. Mining district
  16. Land status
  17. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10013982
MRDS ID D010564
Record type Site
Current site name Unnamed Uranium Occurrence

Geographic coordinates

Geographic coordinates: -103.67691, 38.30669 (WGS84)
Elevation 1337
Location accuracy 1000(meters)
Relative position 24.2 MILES N17W FROM LA JUNTA

Site location context

Political divisions (FIPS codes)

Crowley(county)

Colorado(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Lake Henry(quadrangle 1:24,000 scale)

Las Animas(quadrangle 1:100,000 scale)

Lamar(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Horse(hydrologic unit)

Upper Arkansas(hydrologic accounting unit)

Upper Arkansas(hydrologic subregion)

Arkansas-White-Red(hydrologic region)

Federal lands

ST(Federal land areas administered by ST)

Geographic areas

Country State County
United States Colorado Crowley

Public Land Survey System information

Meridian Township Range Section Fraction State
6th Principal 020S 056W 16 Colorado

Comments on the location information

  • ALONG BRECKENRIDGE OR HORSE CREEK 4 MILES NE OF LAKE HENRY AND 8 M ILES NE OF ORDWAY. ELEV AND LAT-LONG GIVEN ARE FOR CENTER SEC. 16. ; INFO FROM LAND.ST :1981

Commodities

Commodity Importance
Uranium Primary

Materials information

Materials Type of material
Hematite Gangue
Iron Gangue
Limonite Gangue
Selenite Gangue

Alteration

  • (Local) Fe Oxidation

Analytical data

Result 4-IN. BENTONITIC CLAY BED CONTAINS 0.002% EQUIV U AND 0.001% U
Result WE ATHERED MIXTURE OF CLAY, LIMONITE OR HEMATITE, AND SELENITE UNDERLYING BENTONITIC CLAY CONTAINS 0.007% EQUIV U AND 0.006% U
Result WEATHERED MIXTU RE ABOVE CLAY CONTAINS 0.018% EQUIV U AND 0.020% U.

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Shale
    Rock unit name Pierre Shale (Sharon Springs Member)
    Rock description Pierre Shale (Sharon Springs Mbr)
    Stratigraphic age (youngest) Late Cretaceous
    Stratigraphic age (youngest) Late Cretaceous

Nearby scientific data

(1) -103.67691, 38.30669

Economic information

Geologic structures

Type of structure Regional
Structure description Denver Basin, Las Animas Arch
Type of structure Local
Structure description Denver Basin, Las Animas Arch

Ore body information

  • Thickness 1.37M
    Length 8851.15M

Controls for ore emplacement

  • Impermeable Bentonitic Clay And Fe-Rich Layers

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Ordway Area

Land status

Ownership category State

Reference information

Bibliographic references

  • Deposit

    SHARPS, J.A., 1976, GEOLOGIC MAP OF THE LAMAR QUADRANGLE, COLORADO AND KANSAS: USGS MAP I-944.

  • Deposit

    NELSON-MOORE, J.L., AND OTHERS, 1978, RADIOACTIVE MINERAL OCCURRENC ES OF COLORADO AND BIBLIOGRAPHY: CGS BULL. 40, P. 115-117.

  • Deposit

    LANDIS, E.R., 1959, RADIOACTIVITY AND URANIUM CONTENT, SHARON SPRIN GS MEMBER OF THE PIERRE SHALE, KANSAS AND COLORADO: USGS BULL. 1046-L9

General comments

Subject category Comment text
Deposit CONCENTRATION OF U BELIEVED TO BE EPIGENETIC IN ORIGIN AND ASSOCI ATED WITH BENTONITIC CLAYS IN CARBONACEOUS SHALE SEQUENCE CONTAINING F E CARBONATE CONCRETIONS. SECTION CONTAINING MOST U IMMEDIATELY OVERLIE S SANDY SHALE AND CLAY, APPARENTLY THE LATERAL EQUIVALENT OF NEARBY 4- IN. BENTONITIC CLAY. CONCENTRATION COULD BE DUE TO PERCHING OF WATER T ABLE ABOVE IMPERMEABLE CLAY AND TO LOCALIZATION BY FE.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1983 Schwochow, Stephen D. Colorado Geological Survey

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

Authoritative Colorado resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.