The Prospects North of the Johnny Mine is a mine located in Iron county, Utah at an elevation of 7,379 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: 7,379 Feet (2,249 Meters)
Commodity:
Lat, Long: 37.99722, -114.02528
Map: View on Google Maps
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Prospects North of the Johnny Mine MRDS details
Site Name
Primary: Prospects North of the Johnny Mine
Commodity
Secondary: Gold
Secondary: Silver
Location
State: Utah
County: Iron
District: Stateline District
Land Status
Land ownership: Private
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Deposit Type: Vein
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: TABULAR
Structure
Type: R
Description: Pioche Mineral Belt, Sevier Orogenic Belt
Type: L
Description: Fissure At N 10 W
Alterations
Alteration Type: L
Alteration Text: Silicification, Bleaching Of Host Rock
Rocks
Name: Rhyolite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Pliocene
Name: Rhyolite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene
Name: Rhyolite
Role: Associated
Age Type: Host Rock
Age Young: Pliocene
Analytical Data
Not available
Materials
Gangue: Quartz
Gangue: Calcite
Gangue: Pyrite
Comments
Comment (Location): 1:24000 QUADRANGLE MAP IS A 1972 EDITION
Comment (Commodity): COMMODITIES PROBABLY INCLUDE AU AND AG, BUT WERE NOT VISUALLY IDENTIFIED
Comment (Workings): WORKINGS CONSIST OF TWO INCLINED SHAFTS AND AN ADIT. SHAFTS ARE INCLINED TO FOLLOW THE VEIN. ADIT HAS AN INTERNAL SHAFT AT ENTRANCE. FLOOR OF ADIT IS FORMED OF WOODEN PLANKS, INDICATING THAT ENTIRE VEIN WASREMOVED BY MINING.
Comment (Geology): RHYOLITE IS EITHER A FLOW OR AN ASH-FLOW TUFF, DISTINCTION NOT MADE. RHYOLITE CONTAINS LARGE QUARTZ AND FELDSPAR PHENECRYSTS
Comment (Deposit): DEPOSIT CONSISTS OF A VUGGY, BANDED QUARTZ AND CALCITE VEIN. VEIN CONTAINS DISSEMINATED PYRITE, FE-OXIDES, AND ABUNDANT MANGANESE STAINING. ADJACENT HOST ROCK IS SILICIFIED, LOCALLY BRECCIATED, AND CUTY BY QUARTZ VEINLETS
Comment (Deposit): TYPICAL EPITHERMAL, VOLCANIC-HOSTED, QUARTZ-PYRITE-GOLD TYPE ENVIRONMENT ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV
References
Reference (Deposit): THOMPSON, K.C., AND PERRY, L.I., 1975, RECONNAISSANCE STUDY OF THE STATELINE MINING DISTRICT, IRON COUNTY, UTAH: UTAH GEOLOGY, VOL. 2, NO. 1, PP. 27-47
Reference (Deposit): SHUBAT, M.A., ON-SITE INVESTIGATION, UGMS FILES
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