Violet Ray Mine

Past Producer in Tooele county in Utah, United States with commodities Gold, Silver, Mercury, Arsenic, 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. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10012737
MRDS ID D008587
Record type Site
Current site name Violet Ray Mine
Alternate or previous names Eagle Hill Mine

Geographic coordinates

Geographic coordinates: -112.21636, 40.30272 (WGS84)
Elevation 2377
Relative position 2100 FT. S36W FROM EAGLE 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 006S 003W 18 NE Utah

Comments on the location information

  • INFO FROM LAND.ST :(1977)

Commodities

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

Materials information

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

Alteration

  • (Local) Dolomitization And Silicification

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Rock unit name Eagle Hill Rhyolite
    Rock description Eagle Hill Rhyolite
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Mississippian
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
    Rock unit name Upper Great Blue Limestones;Long Trail Shale Member Of The Great Blue Formation
    Rock description Upper Great Blue Limestones;Long Trail Shale Mbr. Of The Great Blue Formation

Nearby scientific data

(1) -112.21636, 40.30272

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
  • General form IRREGULAR

Controls for ore emplacement

  • Fissures (N-S)

Comments on the geologic information

  • LIMESTONES ARE BLUE GRAY WITH SPORADIC CHERT LAYERS AND SOME SANDY LIMESTONES WITH THIN BLACK SHALES. WALLROCKS ARE DOLOMITIZED AND SILICIFIED. ORE MINERALS ARE INTIMATELY ASSOCIATED WITH QUARTZ VEINS. SHALES ARE PULBERIZED, KAOLIMITICS, LIMONITIC, AND CARBONACEOUS

Economic information about the deposit and operations

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

Mining district

District name Mercur District

Land status

Ownership category Private

Comments on the workings information

  • ON SHAFT(VERTICAL), TWO INCLINES (35 DEG.), ALL BADLY CAVED AND INACCESSIBLE. MORE THANT 12 PITS OF DIFFERENT SIZES, WITH LENGHTS VARYING FROM 150 TO 1500 FT., WIDTHS FROM 15 TO 150 FT., AND WITH DEPTHS FROM 15 TO 80 FT.

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 QUADRANGLE:U.S.G.S. PROF. PA.173,167P.

  • Deposit

    BUTTLER, 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.

General comments

Subject category Comment text
Deposit WALLROCKS ARE HIGHLY SHATTERED, CRUMPLED AND ALTERED. MINERALIZATION IS CONTROLLED BY FISSURES RUNNING IN A N-S DIRECTION.
Deposit THE ESTIMATED THICKNESS OF THE UPPER LIMESTONES IS 2,700 FT. THE SEDIMENTARIES ARE INTRUDED BY RHYOLITES OF HIGHLY VARIABLE NATURE. VARIATIONS IN THE APPEARANCE OF THE RHYOLITE ARE THE RESULT OF CHANGES IN TEXTURE, MINERAL CONTENT AND DEGREE OF ALTERATION. ; INFO.SRC : 1 PUB LIT; 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.

External references