Argentine Shaft

Occurrence in Salt Lake county in Utah, United States with commodities Copper, Gold, Lead, 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. Land status
  17. Ownership information
  18. Links to other databases
  19. Bibliographic references
  20. General comments
  21. Reporter information

Geologic information

Identification information

Deposit ID 10020884
MRDS ID DC14212
Record type Site
Current site name Argentine Shaft
Alternate or previous names Argentine Tunnel

Geographic coordinates

Geographic coordinates: -112.18191, 40.51105 (WGS84)
Elevation 2560
Relative position 1,800 FT S62E OF CLIPPER PEAK

Site location context

Political divisions (FIPS codes)

Salt Lake(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 Salt Lake

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 003S 003W 33 NE OF SW OF SE Utah

Comments on the location information

  • INFO FROM LAND.ST :(1977)

Commodities

Commodity Importance
Copper Primary
Gold Primary
Lead Primary
Iron Tertiary

Materials information

Materials Type of material
Chalcopyrite Ore
Galena Ore
Limonite Ore
Pyrite Ore
Actinolite Gangue
Biotite Gangue
Chlorite Gangue
Clay Gangue
Diopside Gangue
Epidote Gangue
Garnet Gangue
Talc Gangue

Alteration

  • (Local) Dolomitization, Biotitization, Chloritization, Diopsitization, Actinolitization And Silicification

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Trachyte
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Pennsylvanian
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Pennsylvanian
  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite
    Rock unit name Latite Porphyry And Volcanic Flows
    Rock description Latite Porphyry And Volcanic Flows
  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
    Rock unit name Upper Bingham Mine
    Rock description Upper Bingham Mine

Nearby scientific data

(1) -112.18191, 40.51105

Economic information

Geologic structures

Type of structure Regional
Structure description Basin And Range
Type of structure Local
Structure description Breccia Zones (N-S And N30e, Dip Steeply Ne)

Ore body information

  • General form IRREGULAR
    Strike W TO NW
    Dip 40N TO 30NE

Controls for ore emplacement

  • Contact Zones; Fissures And Fractures

Comments on the geologic information

  • MINERALIZATION IS INTIMATELY ASSOCIATED WITH QUARTZ VEINS IN ALTERED HOSTROCKS. QUARTZITES ARE CALCAREOUS NEAR ORE ZONES. LIMESTONES ARE DARK GRAY TO BLACK, BUT ARE OF LIGHTER COLORS IN AND AROUND ALTERED WALLROCKS. CALCITE AND JASPEROID VEINS ARE COMMON.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Bingham District

Land status

Ownership category Private

Ownership information

  • Type Owner
    Owner Kennecott Minerals Co.

Comments on the workings information

  • THE INCLINE FOLLOWS THE CONTACT OF QUARTZITE AND LIMESTONE BEDS. A 200 FT. TUNNEL ENDS AT THE CONTACT OF HOSTROCKS WITH PORPHYRY.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit DEPOSIT LIES IN A ZONE OF CROSS FAULTING, SW OF OCCIDENTAL FAULT. WALLROCKS ARE HIGHLY SHEARED AND ALTERED. ORE ZONES ARE LOCALIZED IN FISSURES AND 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.