Three Metals Mine

Past Producer in Tooele county in Utah, United States with commodities Silver, Lead, Gold, Copper
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 10088433
MRDS ID DC12212
Record type Site
Current site name Three Metals Mine

Geographic coordinates

Geographic coordinates: -112.24191, 40.36411 (WGS84)
Elevation 2225
Relative position ABOUT 2400 FT N.54E. FROM LION HILL

Site location context

Political divisions (FIPS codes)

Tooele(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)

Rush-Tooele Valleys(hydrologic unit)

Great Salt Lake(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 Tooele

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 005S 004W 24 SE OF SE OF SW Utah

Comments on the location information

  • INFO FROM LAND.ST :(1977)

Commodities

Commodity Importance
Silver Primary
Lead Primary
Gold Secondary
Copper Secondary

Materials information

Materials Type of material
Cerargyrite Ore
Gold Ore
Malachite Ore
Plumbojarosite Ore
Calcite Gangue
Chlorite Gangue
Dolomite Gangue
Sericite Gangue
Talc Gangue

Alteration

  • (Local) Dolomitization And Silicification

Analytical data

Result AG 90 OZ/TON
Result AU $3/TON
Result CU TRACES
Result PB 11 PERCENT

Host and associated rocks

  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
    Stratigraphic age (youngest) Mississippian
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
    Rock unit name Great Blue Limestone;Humbug Formation
    Rock description Great Blue Limestone;Humbug Formation

Nearby scientific data

(1) -112.24191, 40.36411

Economic information

Geologic structures

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

Ore body information

  • General form IRREGULAR
    Strike N15W TO N50W
    Dip 12E TO 40E

Controls for ore emplacement

  • Fissures

Comments on the geologic information

  • WALLROCKS ARE DEFORMED AND ALTERED. LIMESTONES ARE DARK GRAY, DOLOMITIZED AND SILICIFIED. SHALES ARE GREENISH GRAY TO BLACK, CARBONACEOUS, CALCAREOUS, KAOLINITIC, SERICITIC, AND PILICEOUS. EFFECTS OF LIMONITIZATION ARE VERY SIGNIFICANT ON HOSTROCKS. VEINS OF JASPEROID, QUARTZ AND CALCITE HAVE IMPREGNATED THE WALLROCKS.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Year of first production 1923
Year of last production 1925

Mining district

District name Ophir District; Lion Hill Area

Land status

Ownership category Private

Ownership information

  • Type Owner
    Owner Ophir Metal Co.

Comments on the production information

  • PRODUCTION FIGURES NOT AVAILABLE.

Workings at the site

  • Type of workings Underground
    Length 609.6M

Comments on the workings information

  • ONE TUNNEL, WHICH RUNS FOR 2,000 FT.; THE COURSE OF TUNNEL AS A WHOLE IS ABOUT S40W; CAVED AND INACCESSIBLE

Reference information

Bibliographic references

  • Deposit

    BISSELL, H.J., ET. AL., 1959, GUIDEBOOK TO THE GEOLOGY OF UTAH, NO. 14, UT. GEOL. SOC.: U.G.M.S. BULL. 14, 262P.

  • Deposit

    GILLULY, J., 1932, GEOLOGY AND ORE DEPOSITS OF THE STOCKTON AND FAIRFIELD QUADRANGLES: U.S.G.S. PROF. PA. 173, 167P.

  • Deposit

    BUTLER, B.S., ET. AL., 1920, THE ORE DEPOSITS OF UTAH: U.S.G.S. PROF. PA. 111, 672P.

  • Deposit

    SPURR, J.E., 1895, ECONOMIC GEOLOGY OF THE MERCUR MINING DISTRICT, UTAH: U.S.G.S. 16TH. ANN. REPT., PT. 2, 454P.

  • Production

    GILLULY, J., 1932, P. 141-142.

General comments

Subject category Comment text
Deposit ORE ZONES ARE LOCALIZED IN FISSURES WITH QUARTZ FILLINGS, IN DEFORMED AND HIGHLY ALTERED WALLROCKS; ORE IS COMPLETELY OXIDIZED; ORE BODY DIPS S40W
Deposit THE TUNNEL BEING A CROSSCUT, PENETRATING THE LOWER PART OF THE 'GREAT BLUE' LIMESTONE AND THE UPPER PART OF THE HUMBUG FORMATION. THE FISSURES INTERSECTED IN THE TUNNEL ALL STRIKE NORTHEAST. MOST OF THEM DIP WEST, BUT ONE SHEETED ZONE ALONG WHICH THE TUNNEL IS DRIVEN FOR ABOUT 300 FEET NEAR THE PORTAL, HAS A SOUTHWARD DIP. ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV

Reporter information

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

Beyond USGS

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