Yellow Scheelite Prospect

Past Producer in Pershing county in Nevada, United States with commodity Tungsten
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. Mineral occurrence model information
  9. Host and associated rocks
  10. Nearby scientific data
  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 10103947
MRDS ID M231454
Record type Site
Current site name Yellow Scheelite Prospect
Alternate or previous names Wayne Lode

Geographic coordinates

Geographic coordinates: -118.14404, 40.77878 (WGS84)
Elevation 1676

Site location context

Political divisions (FIPS codes)

Pershing(county)

Nevada(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Woody Canyon(quadrangle 1:24,000 scale)

Eugene Mountains(quadrangle 1:100,000 scale)

Lovelock(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Lower Humboldt(hydrologic unit)

Humboldt(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 Pershing

Public Land Survey System information

Meridian Township Range Section Fraction State
Mount Diablo 304N 034E 34 Nevada

Comments on the location information

  • WEST OF THE STANK MINE ON THE EAST SIDE OF STANK HILL.

Commodities

Commodity Importance
Tungsten Critical Primary

Materials information

Materials Type of material
Scheelite Ore
Epidote Gangue
Garnet Gangue
Quartz Gangue

Analytical data

Result THE YELLOW SCHEELITE BED CONTAINED 0.5-0.75 % W03.

Mineral occurrence model information

Model code 42
USGS model code 14a
Deposit model name W skarn

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Stratigraphic age (youngest) Late Triassic
  • Host or associated Associated
    Rock type Metamorphic Rock > Hornfels
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone

Economic information

Ore body information

  • Thickness 0.61M

Controls for ore emplacement

  • Limestone Bed Near Granodiorite Stock.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Medium
Significant No

Mining district

District name Mill City District

Land status

Ownership category Private

Comments on the workings information

  • IN 1945 CROSSCUTS WERE EXTENDED FROM THE STANK MINE TO THE YELLOW SCHEELITE BED ON THE 300 FT AND 400 FT LEVELS.

Reference information

Bibliographic references

  • Deposit

    LEMMON, D.M., 1977, IN GEOLOGY AND MINERAL DEPOSITS OF PERSHING COUNTY, NEVADA: NBMG BULL. 89

  • Deposit

    KERR, 1934, GEOLOGY OF THE TUNGSTEN DEPOSITS NEAR MILL CITY, NEVADA:NBMG BULL. 21

  • Deposit

    KERR, 1946, TUNGSTEN MINERALIZATION IN THE UNITED STATES: GSA MEMOIR 15

  • Deposit

    TINGLEY, J.V., UNPUBLISHED REPORT, 1973.

  • Deposit

    STAGER, H. K., IN PREP., NBMG BULL ON TUNGSTEN DEPOSITS OF NEVADA.

General comments

Subject category Comment text
Deposit IN 1945 CROSSCUTS WERE EXTENDED FROM THE STANK MINE TO THE YELLOW SCHEELITE BED ON THE 300 AND 400 LEVELS. THE YELLOW SCHEELITE BED IS PART OF THE STANK-HUMBOLDT BELT ALONG WITH THE CODD, STANK, KEYES, GEORGE, SPRINGER AND HUMBOLDT WORKINGS. THE DEPOSIT'S NAME WAS APPLIED BECAUSE THE SCHEELITE FOUND IN THE DEPOSIT WAS THOUGHT TO FLUORESCE A MORE YELLOW -COLOR THAN THAT FROM THE NEARBY MINES ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT
Deposit THE YELLOW SCHEELITE BED IS PART OF THE STANK-HUMBOLDT BELT.THE YELLOW SCHEELITE TACTITE-LIMESTONE BED IS ABOUT 200 FT WEST OF THE STANK BED AND OCCUPIES THE SAME RELATIVE PO-SITION TO THE STANK BED AS DOES THE GEORGE BED. THE YELLOW SCH-EELITE AND GEORGE BEDS ARE PROBABLY FAULTED SEGMENTS OF THE SA-ME BED. ACCORDING TO KLEPPER (1943), THE BED WAS PRESENT IN TH-E YELLOW SCHEELITE MINE ONLY BETWEEN THE SURFACE AND THE 200 F-T LEVEL, AND IT EXTENDED FROM THE SPRINGER STOCK TO THE PRE-GR-ANODIORITE FAULT AT THE NORTH END OF THE STANK MINE

Reporter information

Type Date Name Affiliation Comment
Reporter 01-NOV-1980 Royse, Sue E. Nevada Bureau of Mines and Geology
Updater 01-AUG-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.