The Woodside Mine is a silver and lead mine located in Summit county, Utah at an elevation of 7,598 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.
Elevation: 7,598 Feet (2,316 Meters)
Primary Mineral: Silver, Lead
Lat, Long: 40.63306, -111.50000
Map: View on Google Maps
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.
Woodside Mine MRDS details
Primary: Woodside Mine
Secondary: Silver King Coalition Group
District: Park City Area; Park City District
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.
Owner Name: United Park City Mines Co.
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Discovery Year: 1873
Discovery Method: Ore-Mineral In Place
Years of Production:
Deposit Size: S
General Physiographic Area: Rocky Mountain System
Physiographic Province: Middle Rocky Mountains
Physiographic Detail: Wasatch Mountains
Mineral Deposit Model
Description: Thrust Belt
Description: Fractures Striking N 30-35 N; Faults And Brecciated Zones
Age Type: Host Rock
Age Young: Pliocene
Comment (Commodity): THE ORE IS MADE UP OF COPPER CARBONATES, AND LEAD CARBONATE, SULPHATE, AND SULPHIDE. FLUORITE OCCURS IN GANGUE.
Comment (Location): SECTION SUBDIVISIONS SE 1/4 SE 1/4 NW 1/4
Comment (Production): PRODUCED $700,000. WORTH OF ORE BY LATE 1880'S OR EARLY 1890'S, CONSIDERABLE PRODUCTION THEREAFTER.
Comment (Deposit): IT IS OBSERVED THAT WITHIN THE LOWEST PORTION ORE FORMED IN THESE LIMESTONE BEDS, EACH OF WHICH WAS UNDERLAIN BY A SANDY QUARTZITIC MEMBER AND THE MAIN OR HIGHESTONE BEING ALSO OVERLAIN BY QUARTZITE. THE CALCAREOUS MEMBER REPLACED WAS A FINE GRAINED DARK DENSE BED. THE ORE BEDS OR LENSES RANGED 2 TO 40 FT. IN THICKNESS.
Comment (Workings): ONE MAIN SHAFT AND ONE TUNNEL. TUNNEL IS 2,200 FT. LONG, SHAFT HAS 4,500 FT. OF DRIFTS. SHAFT IS 500 FT. DEEP.
Comment (Geology): FLUORITE IS FOUND AS A PIGMIFICANT GANGUE MINERAL. BOTH MASSIVE AND SEMICRYSTALLINE TYPES OCCUR IN LENSES. AN INCH THICK IN THE LIMESTONE AND IN THE ORE LYING ACCORDANT WITH THE BEDDING IN EACH BED.
Reference (Deposit): BOUTWELL, J.M., 1912, GEOLOGY AND ORE DEPOSITS OF PARK CITY DISTRICT, UTAH: USGS PROF PAPER, 77, 230 P.
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): ERICKSON, A.J., 1968, PARK CITY DISTRICT: UTAH GEOL. SOC. GUIDEBOOK NO. 22.
Reference (Deposit): 1966 GEOLMAP CRITTENDEN, CALKINS AND SHARP GQ-53
Reference (Production): ERICKSON, A.J.,(ED.) 1968, PARK CITY DISTRICT: UTAH GEOL. SOC. GUIDEBOOK NO. 22.
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