Mercur Quarry

Past Producer in Tooele county in Utah, United States with commodities Gold, Silver, Arsenic, Mercury, Antimony, 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 10087663
MRDS ID D008506
Record type Site
Current site name Mercur Quarry

Geographic coordinates

Geographic coordinates: -112.21913, 40.33272 (WGS84)
Elevation 2219
Relative position ABOUT 5200 FT. N. 30 W. FROM MERCUR

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)

Geographic areas

Country State County
United States Utah Tooele

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 006S 003W 06 NW OF NW OF NE Utah

Comments on the location information

  • INFO FROM LAND.ST :(1977)

Commodities

Commodity Importance
Gold Primary
Silver Primary
Arsenic Critical Secondary
Mercury Secondary
Antimony Critical Secondary
Iron Tertiary

Materials information

Materials Type of material
Cerargyrite Ore
Cinnabar Ore
Limonite Ore
Orpiment Ore
Pyrite Ore
Realgar Ore
Stibnite Ore
Barite Gangue
Calcite Gangue
Chlorite Gangue
Quartz Gangue
Sericite Gangue
Talc Gangue

Alteration

  • (Local) Dolomization, Sericitization, Limomitization, Kaolominzation And Silicification

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
    Rock unit name Great Blue Limestones;Long Trail Shale Member Of The Great Blue Limsestone
    Rock description Great Blue Limestones;Long Trail Shale Mbr. Of The Great Blue Limsestone
    Stratigraphic age (youngest) Mississippian

Nearby scientific data

(1) -112.21913, 40.33272

Economic information

Geologic structures

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

Ore body information

  • General form IRREGULAR
    Strike NW
    Dip 15NE
  • General form IRREGULAR
    Dip 15NE
  • General form IRREGULAR
    Dip 15NE

Controls for ore emplacement

  • Fissuers-Trending Ene-Wsw And N-S; Dipping Steeply Due West

Comments on the geologic information

  • WALLROCKS ARE HIGHLY SHATTERED, FOLDED AND CRUMPLED. SHALES ARE BROWN TO BUFF, FN'ABLE AND PULVERIZED, SERICITIC, CALCAREOUS, CARBONACEOUS, AND KAOLIMITIC. LIMESTONES ARE JOINTED, BRECCIATED, DARK GRAY TO BLACK, CHERTY, DOLOMITIC, SILICIFIED AND IMPREGNATED WITH VEINS OF CALCITE AND QUARTZ. ORE MINERALS ARE INTIMATELY ASSOCIATED WITH VEINS OF JASPEROID AND QUARTZ. EFFECTS ARE LIMONITIZATION ARE VERY SIGNIFICANT ON WALLROCKS

Economic information about the deposit and operations

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

Mining district

District name Mercur District

Land status

Ownership category Private

Ownership information

  • Type Operator
    Owner Consolidated Mercur Mines Co.
  • Type Owner
    Owner Getty Oil Co.

Comments on the production information

  • PRODUCTION FIGURES ARE NOT AVAILABLE

Comments on the workings information

  • ONE LARGE PIT OF 2000 X 1400 X 500 FT.; FIVE SMALL PITS OF 150 X 120 X 100 FT., 150 X120 X 20 FT., 120 X 60 X 30 FT., 150 X 50 X 40 FT., 300 X60 X60 FT.; TWO ADITS (35 DEG.) 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

    BISSELL, H.J., 19598 P. 214; SPURR, J.E., 1895, P.407

General comments

Subject category Comment text
Deposit THE ORE IS SOFT AND PULVERIZED, LIGHT YELLOWISH, OR GREYISH IN COLOUR. GOLD IS NOT VISIBLE IN THE ORES, AND IS CONCENTRATED ONLY IN THE CARBON RICH PORTIONS OF THE ALTERED ZONES. THE ORE IS FORMED BY THE IMPREGNATION AND REPLACEMENT OF THE WALLROCKS; AND THE FISSURE FILLINGS ARE NEGLIGIBLE. NEVERTHELESS THESE FISSURES WERE OF FUNDAMENTAL IMPORTANCE IN LOCALIZING THE DEPOSITS ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV
Deposit MINERALIZATION IS LOCALIZED IN ALTERED ZONES IN WALLROCKS. UNALTERED ROCKS ARE BARREN. THE OXIDIZED ORE IS LIGHT COLOURED AND MORE FN'ABLE THAN UNOXIDIZED ORE. IT LACKS SULFIDES AND CONTAINS SULFATES INCLUDING GYPSUM, SCORODITE AND MELANTERITE

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.