Quinseck Claims

Occurrence in Esmeralda county in Nevada, United States with commodities Manganese, 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. Alteration
  8. Host and associated rocks
  9. Nearby scientific data
  10. Geologic structures
  11. Ore body information
  12. Controls for ore emplacement
  13. Economic information about the deposit and operations
  14. Mining district
  15. Land status
  16. Links to other databases
  17. Bibliographic references
  18. General comments
  19. Reporter information

Geologic information

Identification information

Deposit ID 10047194
MRDS ID M242455
Record type Site
Current site name Quinseck Claims
Alternate or previous names NBMG Sample Site 460

Geographic coordinates

Geographic coordinates: -117.86871, 37.98438 (WGS84)

Site location context

Political divisions (FIPS codes)

Esmeralda(county)

Nevada(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Rhyolite Ridge NE(quadrangle 1:24,000 scale)

Goldfield(quadrangle 1:100,000 scale)

Goldfield(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Southern Big Smoky Valley(hydrologic unit)

Central Nevada Desert Basins(hydrologic accounting unit)

Central Nevada Desert Basins(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 Esmeralda

Public Land Survey System information

Meridian Township Range Section Fraction State
Mount Diablo 002N 037E 33 NE OF SW Nevada

Comments on the location information

  • INFO FROM LAND.ST :(1972)

Commodities

Commodity Importance
Manganese Critical Primary
Uranium Tertiary

Alteration

  • (Local) Strong Hyprothermal Alteration To Clays

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Pliocene
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite

Nearby scientific data

(1) Alluvium, undifferentiated

Economic information

Geologic structures

Type of structure Local
Structure description Faults,Slickensides

Ore body information

  • General form BLANKET
    Strike HORIZONTAL
    Dip HORIZONTAL
    Thickness 1M
    Length 10M

Controls for ore emplacement

  • Ne-Trending Fault Zone?

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Coaldale District

Land status

Ownership category BLM Administrative Area

Comments on the workings information

  • BULLDOZING, DRILLHOLE

Comments on development

  • BULLDOZER ROAD, RECENT DRILLHOLE PROBABLY FOR URANIUM

Reference information

Bibliographic references

  • Deposit

    GARSIDE, L.J. , 1982, FIELD EXAMINATION 13 JULY 1982.

  • Deposit

    ALBERS, J.P. AND STEWART, J.H., 1972, NBMG BULL 78, P. 59-60

General comments

Subject category Comment text
Deposit PRESUMABLY ACROSS THE PROPOSED FAULT) HIT WELDED TUFF, BUT SHOWS NO INDICATIONS (IN THE CUTTINGS) OF SINTER. IF THERE IS A FAULT HERE, IT WOULD BE NE-TRENDING. THE SINTER IS NEARLY HORIZONTAL, SUGGESTI
Deposit PROSPECT CONSISTS OF AN OUTCROP OF BROWN TO BLACK IRON- AND MANGANESE- OXIDE- BEARING SILICEOUS SINTER ONLY 1 M THICK AND 10 M LONG. IT APPEARS TO BE A SPRING SINTER DEPOSIT, FINELY LAMINATED, OVERLYING A 15-20 CM ZONE OF CEMENTED WELDED TUFF FRAGMENTS THAT APPEARS TO BE A REGOLITH ON A SOLID OUTCROP OF RHYOLITIC WELDED TUFF. THE TUFF UNIT IS PROBABLY THE SAME ONE PRESENT ABOUT 0.5 KM EAST AT THE COALDALE URANIUM PROPERTY. HOWEVER, THE SINTER AND SURROUNDING ROCKS ARE NOT ANOMALOUSLY RADIOACTIVE HERE. THE SINTER IS DOWNSLOPE FROM A 6-7 CM LAYER OF CLAY-RICH MATERIAL THAT IS HYDROTHERMALLY ALTERED RHYOLITIC WELDED TUFF (SMECTITE CLAY S?) THE SINTER IS CUT BY SMALL VEINLETS OF MN OXIDES. THE SINTER MAY BE ASSOCIATED WITH A FAULT ZONE HERE; THERE IS A LARGE FAULT BRECCIA ZONE TO THE WEST AND A SLICKENSIDED SURFACE (NEARLY HORIZONTAL SLICKENSIDES) OCCURS JUST BELOW THE SINTER. ALSO A FAULT MAY FORM THE MOUNTAIN FRONT HERE. HOWEVER, A DRILL HOLE TO THE SOUTH OF THE SINTER (AND

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1985 La Pointe, D.D. (Tingley, J.V.) Nevada Bureau of Mines and Geology

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.