The Peace Mine is a gold and silver mine located in Washington county, Utah at an elevation of 5,279 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
Elevation: 5,279 Feet (1,609 Meters)
Commodity: Gold, Silver
Lat, Long: 37.38417, -113.87444
Map: View on Google Maps
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Peace Mine MRDS details
Site Name
Primary: Peace Mine
Commodity
Primary: Gold
Primary: Silver
Location
State: Utah
County: Washington
District: Goldstrike District
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Owner Name: Padre Mining Co., Bountiful, Utah
Owner Name: John Carroll And Associates
Home Office: New York City, Ny
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
Not available
Mineral Deposit Model
Not available
Orebody
Form: IREEGULAR
Structure
Type: R
Description: Sevier Overthrust Belt, Detachment And Denudation Faults.
Type: L
Description: Anticline, Upright And Tight With Axial Plane Striking N45e
Alterations
Alteration Type: L
Alteration Text: Oxidation
Rocks
Name: Limestone
Role: Host
Age Type: Host Rock
Age Young: Mississippian
Analytical Data
Analytical Data: A CHIP-CHANNEL SAMPLE WAS COLLECTED BY LEE PERRY OF THE UGMS IN 1979 WITH THE FOLLOWING RESULTS: .88 PPM AU, 1.0 PPM AG, 120 PPM AS, 3 PPM SB, 450 PPB HG, 12 PPM CU, 1 PPM MO, 30 PPM PB, 90 PPM ZN. A SECOND SAMPLE WAS COLLEDTED BY HARRY MESSENGER IN 1983 WITH THE FOLLOWING RESULTS: .1 PPM AU, .3 PPM AG, .7 PPM AS, 1 PPM SB, 220 PPB HG
Materials
Gangue: Limonite
Gangue: Hematite
Gangue: Calcite
Comments
Comment (Development): MANY ROTARY DRILL HOLES HAVE BEEN DRILLED IN THE DISTRICT IN RECENT YEARS
Comment (Deposit): DEPOSIT CONSISTS OF BRECCIATED ANDIRON STAINED LIMESTONE AND ARGILLITE IN A FAULT ZONE WITH LOCALLY ABUNDANT CALCITE VEINLETS. QUARTZ FRAGMENTS, POSSIBLY FROM QUARTZ VEINS, ARE PRESENT IN THE BRECCIA.
Comment (Workings): WORKINGS CONSIST OF TWO ADITS AND ONE SHAFT. ONE ADIT IS CAVED, AND THE OTHER IS BACKFILLED. SHAFT IS OPEN BUT SHALLOW. LOWER ADIT MAY BE 1000 FEET LONG, BUT IS CAVED. UPPER ADIT IS 60 FEET LONG. SHAFT IS 10 FEET DEEP
References
Reference (Deposit): ADAIR, D.H., AND MESSENGER, H.M., 1975, UNPUBLISHED GEOLOGIC MAP OF THE GOLDSTRIKE DISTRICT
Reference (Deposit): SHUBAT, M.A., 1985, ON-SITE INVESTIGATION, UGMS FILES
Reference (Deposit): MESSENGER, H.M., 1983, UNPUBLISHED REPORT ON THE GOLDSTRIKE DISTRICT, UGMS FILES
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