Rover Hill Mine #4

The Rover Hill Mine #4 is a gold and silver mine located in Tooele county, Utah at an elevation of 8,281 feet.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Rover Hill Mine #4  

State:  Utah

County:  Tooele

Elevation: 8,281 Feet (2,524 Meters)

Primary Mineral: Gold, Silver

Lat, Long: 40.34139, -112.24444

Map: View on Google Maps


Satelite image of the Rover Hill Mine #4

Rover Hill Mine #4 MRDS details

Site Name

Primary: Rover Hill Mine #4


Commodity

Primary: Gold
Primary: Silver
Secondary: Antimony
Secondary: Mercury
Secondary: Arsenic
Tertiary: Iron


Location

State: Utah
County: Tooele
District: Mercur District


Land Status

Land ownership: Private


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Great Basin
Physiographic Detail: Uinta Extension


Mineral Deposit Model

Not available


Orebody

Form: IRREGULAR

Form: IRREGULAR


Structure

Type: R
Description: Basin And Range

Type: L
Description: Fissures And Fractures


Alterations

Alteration Type: L
Alteration Text: Dolomitization And Silicification


Rocks

Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene

Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Mississippian

Name: Diorite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Pliocene


Analytical Data

Not available


Materials

Ore: Realgar
Ore: Stibnite
Ore: Orpiment
Ore: Pyrite
Ore: Cinnabar
Gangue: Quartz
Gangue: Calcite
Gangue: Talc
Gangue: Chlorite


Comments

Comment (Location): INFO FROM LAND.ST :(1977)

Comment (Workings): ONE INCLINE (35 DEG.), CAVED AND INACCESSIBLE; SEVERAL SMALL PITS AND TRENCHES.

Comment (Deposit): MINERALIZED ZONE IS LOCATED IN ALTERED WALLROCKS, AND IS CONTROLLED BY FRACTURES. THE ORE IS SOFT AND PULVERIZED, LIGHT YELLOWISH OR GREYISH IN COLOR. ORE MINERALS ARE INTIMATELY ASSOCIATED WITH VEINS OF QUARTZ AND JASPEROID.

Comment (Production): PRODUCTION FIGURES ARE NOT AVAILABLE.

Comment (Geology): WALLROCKS ARE DEFORMED AND ALTERED. LIMESTONES ARE DARK GRAY, CLURTY, DOLOMITIZED AND SILICIFIED. SHALES ARE PULVERIZED, CALCAREOUS, SILICEOUS, SENCITIE, CARBONACEOUS, KAOLIMITIC AND CARBONACEOUS.


References

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

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

Reference (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.

Reference (Deposit): GILLULY,J.,1932,GEOLOGY AND ORE DEPOSITS OF THE STOCKTON AND FAIRFIELD QUADRANGELES: U.S.G.S. PROF. PA.173,167P.

Reference (Production): MOHAMMAD, H., 1981, ON SITE INVESTIGATION: U.G.M.S.