Bingham West Dip Tunnel

Occurrence in Tooele county in Utah, United States with commodities Lead, Copper, Silver, Zinc, Iron
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. Links to other databases
  17. Bibliographic references
  18. General comments
  19. Reporter information

Geologic information

Identification information

Deposit ID 10087669
MRDS ID D008521
Record type Site
Current site name Bingham West Dip Tunnel

Geographic coordinates

Geographic coordinates: -112.19941, 40.55244 (WGS84)
Elevation 1870
Relative position ABOUT 6000 FT. N68W FROM MARKHAM PEAK IN POLE CANYON

Site location context

Political divisions (FIPS codes)

Tooele(county)

Utah(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Bingham Canyon(quadrangle 1:24,000 scale)

Tooele(quadrangle 1:100,000 scale)

Tooele(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Rush-Tooele Valleys(hydrologic unit)

Great Salt Lake(hydrologic accounting unit)

Great Salt Lake(hydrologic subregion)

Great Basin(hydrologic region)

Geographic areas

Country State County
United States Utah Tooele

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 003S 003W 17 SW OF SE OF SE Utah

Commodities

Commodity Importance
Lead Primary
Copper Primary
Silver Primary
Zinc Critical Primary
Iron Secondary

Materials information

Materials Type of material
Galena Ore
Pyrite Ore
Sphalerite Ore
Calcite Gangue
Chlorite Gangue
Quartz Gangue
Sericite Gangue

Alteration

  • (Local) Dolomitization And Silicification

Host and associated rocks

  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
    Rock unit name Upper Bingham Mine
    Rock description Upper Bingham Mine
    Stratigraphic age (youngest) Pennsylvanian
    Stratigraphic age (youngest) Pennsylvanian

Economic information

Geologic structures

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

Ore body information

  • General form IRREGULAR
  • General form IRREGULAR

Controls for ore emplacement

  • Fissures And Fractures

Comments on the geologic information

  • QUARTZ AND CALCITE VEINS ARE VERY COMMON IN WALLROCKS. ORE MINERALS ARE INTIMATELY ASSOCIATED WITH QUARTZ VEINS.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Bingham Canyon

Comments on the workings information

  • TUNNEL USED FOR HAULAGE PURPOSES; CAVED; INACCESSIBLE.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit DEPOSIT LIES CLOSE TO THE AXIAL REGION OF BINGHAM SYNCLINE. HOSTROCKS ARE SHEARED AND ALTERED. MINERALIZATION IS CONTROLLED BY FRACTURES.

Reporter information

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

Beyond USGS

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

External references