The Judge Tunnel is a silver, lead, and zinc mine located in Summit county, Utah at an elevation of 7,799 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: 7,799 Feet (2,377 Meters)
Commodity: Silver, Lead, Zinc
Lat, Long: 40.62639, -111.50306
Map: View on Google Maps
Satelite View
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
Judge Tunnel MRDS details
Site Name
Primary: Judge Tunnel
Commodity
Primary: Silver
Primary: Lead
Primary: Zinc
Secondary: Gold
Secondary: Copper
Location
State: Utah
County: Summit
District: Park City 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
Owner Name: United Park City Mines Co.
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: L
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Middle Rocky Mountains
Physiographic Detail: Wasatch Mountains
Mineral Deposit Model
Not available
Orebody
Form: TABULAR TO IRREGULAR
Structure
Type: R
Description: Thrust Belt
Alterations
Not available
Rocks
Name: Quartzite
Role: Host
Age Type: Host Rock
Age Young: Late Permian
Analytical Data
Not available
Materials
Gangue: Quartz
Gangue: Calcite
Comments
Comment (Workings): TUNNEL TRENDS TOWARD THE ONTARIO GROUP
Comment (Location): SECTION SUBDIVISIONS NW 1/4 SE 1/4 SW 1/4
Comment (Production): PRODUCTION UNKNOWN
References
Reference (Deposit): CRITTENDEN, M.D., ET.AL., 1966, GEOL. MAP OF THE PARK CITY WEST QUAD: U.S.G.S. MAP GQ-535.
Reference (Deposit): BOUTWELL, J.M., 1912, GEOL. AND ORE DEPOSITS OF THE PARK CITY DISTRICT, UT.: U.S.G.S. PROF. PA. 77.
Reference (Deposit): ERICKSON, A.J., (ED.), 1966, PARK CITY DISTRICT, UT.: UTAH GEOL. SOCIETY GUIDEBOOK NO. 22.
Reference (Deposit): PERRY, L.I. 1976, LEAD AND ZINC IN UTAH: UTAH GEOL. AND MINERAL SURVEY OPEN FILE REPORT NO. 22.
Reference (Deposit): 1966 GEOLMAP CRITTENDEN, CALKINS AND SHARP GQ-53
Reference (Production): SALT LAKE MINING REVIEW, 1916, 1917, 1918, 1919, 1920, 1921, 1922, 1923
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These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.
