Old Man Spring Prospect

Occurrence in Humboldt county in Nevada, 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. Mineral occurrence model information
  10. Host and associated rocks
  11. Nearby scientific data
  12. Geologic structures
  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 10047384
MRDS ID M242674
Record type Site
Current site name Old Man Spring Prospect
Alternate or previous names Chevron Oil Prospect?

Geographic coordinates

Geographic coordinates: -118.15266, 41.90432 (WGS84)
Elevation 1897

Site location context

Political divisions (FIPS codes)

Humboldt(county)

Nevada(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Disaster Peak(quadrangle 1:24,000 scale)

Denio(quadrangle 1:100,000 scale)

Vya(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Upper Quinn(hydrologic unit)

Black Rock Desert(hydrologic accounting unit)

Black Rock Desert-Humboldt(hydrologic subregion)

Great Basin(hydrologic region)

Federal lands

Bureau of Land Management(Bureau of Land Management NV)

Bureau of Land Management NV BLM(Type of land area)

BLM(Federal land areas administered by BLM)

Geographic areas

Country State County
United States Nevada Humboldt

Public Land Survey System information

Meridian Township Range Section Fraction State
Mount Diablo 047N 034E 33,34 SE (33); SW (34) Nevada

Comments on the location information

  • ALONG THE WESTERN EDGE OF BULL BASIN ABOUT 1 MILE ENE OF OLD MAN SPRING . INFO FROM LAND.ST :(1972)

Commodities

Commodity Importance
Uranium Primary

Materials information

Materials Type of material
Clay Gangue
Iron Gangue
Opal Gangue
Quartz Gangue
Barite Unknown

Alteration

  • (Local) Argillized, Limonite-Stained; Silicification

Analytical data

Result U3O8 UP TO 0.13% WITH HIGH K (TO 10.9%) AND TH (0.5'%), AND ANOMALOUS AS, BA, F, HG, MO, SB, Y, ZR. LIMEY BEDS TO THE NORTH OF THE TRENCHES HAVE UP TO 41 PPM U3O8 AND HIGH AG. RADIOACTIVITY IS 2-3 X BG IN A AREA AS LARGE AS 20 YD SQUARE, AS A RESULT OF CAT WORK
Result 3 SEPARATE ANOMALIES WERE NOTED ALONG THE N-S ROAD HERE. BEST RADIOACTIVITY IS NOT IN SOLID ROCK, BUT ONE BOULDER FROM THE PROSPECT ASSAYED 200 PPM U3O8 AND 207 PPM TH.

Mineral occurrence model information

Model code 155
USGS model code 25f
Deposit model name Volcanogenic U

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Mudstone
    Stratigraphic age (youngest) Miocene
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Argillite

Economic information

Geologic structures

Type of structure Regional
Structure description Mcdermitt Caldera, A Miocene Volcanic Collapse Feature About 40km Across
Type of structure Local
Structure description This Occurrence Is Near The Edge Of The Intracaldera Moat Where They Lap Up Against The W. Wall Of The Caldera

Controls for ore emplacement

  • Fault Gouge Zone?

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Disaster District; Kings River; Thacker Pass Area

Land status

Ownership category BLM Administrative Area

Comments on the workings information

  • BULL-DOZED TRENCHES

Reference information

Bibliographic references

  • Deposit

    GREENE, R.C., 1976, USGS OFR 76-753.

  • Deposit

    MITCHELL, T.P., 1980, FIELD EXAMINATION OF URANIUM OCCURRENCE

  • Deposit

    WILLDEN, R., 1964, NBMG BULL 59, PL. I.

General comments

Subject category Comment text
Deposit THE HIGHEST RADIOACTIVITY IS ASSOCIATED WITH REDDISH-BROWN CLAY, POSSIBLY FAULT GOUGE. THIS OCCURRENCE IS AT THE EDGE OF THE SEDIMENTARY BASIN AND IN THE AREA OF THE CALDERA RING FRACTURE. AT THE EDGE OF THE SEDIMENTS, A SYSTEMATIC INCREASE IN PERMEABILITY CAN BE PREDICTED, WHICH WOULD FACILITATE THE MIGRATION OF SOLUTIONS INTO THE SEDIMENT HOSTS.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-DEC-1985 La Pointe, D.D. (Tingley, J.V.) Nevada Bureau of Mines and Geology
Updater 01-SEP-1994 Li, Zhiping (Peters, S.) U.S. Geological Survey

Beyond USGS

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

Authoritative Nevada resources

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