Wells Canyon Nickel and Clay Pits

Past Producer in Utah county in Utah, United States with commodities Clay, Nickel, Zinc
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. Ownership information
  18. Workings at the site
  19. Links to other databases
  20. Bibliographic references
  21. General comments
  22. Reporter information

Geologic information

Identification information

Deposit ID 10012715
MRDS ID D008557
Record type Site
Current site name Wells Canyon Nickel and Clay Pits

Geographic coordinates

Geographic coordinates: -112.16608, 40.263 (WGS84)
Elevation 1667
Relative position 12,800 FT SOUTH OF MANNING TOWNSITE

Site location context

Political divisions (FIPS codes)

Utah(county)

Utah(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Mercur(quadrangle 1:24,000 scale)

Rush Valley(quadrangle 1:100,000 scale)

Tooele(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Utah Lake(hydrologic unit)

Jordan(hydrologic accounting unit)

Great Salt Lake(hydrologic subregion)

Great Basin(hydrologic region)

Federal lands

Bureau of Land Management(Bureau of Land Management UT)

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

BLM(Federal land areas administered by BLM)

Geographic areas

Country State County
United States Utah Utah

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 006S 003W 27 SE OF SW OF SE Utah

Comments on the location information

  • INFO FROM LAND.ST :(1977)

Commodities

Commodity Importance
Clay Primary
Nickel Critical Primary
Zinc Critical Primary

Materials information

Materials Type of material
Kaolinite Ore
Montmorillonite Ore
Sericite Ore
Smithsonite Ore
Calcite Gangue
Chlorite Gangue
Quartz Gangue

Alteration

  • (Local) Sericitization, Limonitization And Silicification

Host and associated rocks

  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
    Stratigraphic age (youngest) Pennsylvanian
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Shale
    Rock unit name Manning Canyon Shale
    Rock description Manning Canyon Shale

Nearby scientific data

(1) -112.16608, 40.263

Economic information

Geologic structures

Type of structure Regional
Structure description Basin And Range
Type of structure Local
Structure description Fractures And Fissures

Ore body information

  • General form BLANKET
    Dip 30N
  • General form BLANKET
    Dip 30N
  • General form BLANKET
    Dip 30N

Controls for ore emplacement

  • Sedimentary Basin; And Fractures And Fissures

Comments on the geologic information

  • THE SHALES ARE HIGHLY SQUEEZED. LIMESTONES ARE BRECCIATED AND ALTERED. SECONDARY SILICA AND CALCITE OCCUR ALONG WITH SMITHSONITE IN VUGS, CAVITIES AND VEINS.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Both
Deposit size Small
Significant No

Mining district

District name Mercur District

Land status

Ownership category Private

Ownership information

  • Type Owner
    Owner Charles Mercer

Comments on the production information

  • PRODUCTION FIGURES ARE NOT KNOWN

Workings at the site

  • Type of workings Surface
    Area 0.066HA
    Overall length 45.72M
    Overall width 15.24M

Comments on the workings information

  • IN ADDITION TO CLAY PIT, SEVERAL OTHER SMALL PROSPECTING PITS AND TRENCHES ARE FOUND.

Reference information

Bibliographic references

  • Deposit

    HYATT, E.R., 1956, CLAYS OF UTAH COUNTY, UTAH: U.G.M.S. BULL. 55.

  • Deposit

    BISSELL, H.J., ET. AL., 1958, GUIDEBOOK TO THE GEOLOGY OF UTAH, NO 14, UT GEOL. SOC.: U.G.M. BULL. 14, 262 P.

  • Deposit

    ANDERSON, B.J., 1959, NICKEL-ZINC MINERALIZATION IN THE SOUTHERN OQUIRRH MOUNTAINS, UTAH: M.S. THESIS, UNIV. OF UTAH

  • Deposit

    VAN SANT, JOEL, N., 1964, REFRACTORY CLAY DEPOSITS OF UTAH: U.S. BUR. OF MINES INF.CIRC. 8213

  • Production

    MOHAMMAD, H., 1981, ON SITE INVESTIGATION: U.G.M.S.

General comments

Subject category Comment text
Deposit NICKEL MINERALS OCCURE AS VEINLETS OF BRIGHT GREEN MATERIAL IN A LIMONITIC MATRIX, AND ALSO AS A MASSIVE GREYISH GREEN SMITHSONITE IN LIMESTONES, EXPOSED IN A ROAD CUT OF 300 SQ FT AREA, NEAR THE CLAY PIT MINERLIZATION IS LOCALIZED TO FRACTURES
Deposit AVERAGE NICKEL CONTENT OF SHALES AND LIMESTONES OF THIS AREA IS SLIGHTLY LESS THAN 0.1%, WHICH IS HIGHER THAN THE KNOWN AVERAGE VALUES (0.001% AND 0.0089%, RESPECTIVELY). ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT; 3 FIELD OBSERV

Reporter information

Type Date Name Affiliation Comment
Reporter 01-APR-1981 Mohammad, Hasan Utah Geological and Mineral Survey

Beyond USGS

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