The Mazepah Shaft is a lead and silver mine located in Summit county, Utah at an elevation of 8,379 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.
Elevation: 8,379 Feet (2,554 Meters)
Primary Mineral: Lead, Silver
Lat, Long: 40.61472, -111.50722
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.
Mazepah Shaft MRDS details
Primary: Mazepah Shaft
Secondary: Daly Group
Secondary: United Park City Mines
Secondary: Park Utah Consolidated Mines
Secondary: Mazeppa Shaft
District: 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
Year First Production: 1886
Discovery Year: 1885
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: Uinta-Cottonwood Arch, Sevier Overthrust Belt, Park City Anticline
Description: Northeast Striking Fissures And Faults
Alteration Type: L
Alteration Text: Oxidation
Age Type: Associated Rock Unit
Age Young: Oligocene
Age Type: Associated Rock
Age Young: Oligocene
Comment (Deposit): RICH SILVER ORES REPORTEDLY STRUCK IN SHAFT. THE DIXIE VEIN IS LOCATED WITHIN THE GENERAL VICINITY OF THE SHAFT AND IS PROBABLY WHAT WAS EXPLORED BY THESE WORKINGS. SHAFT AND ASSOCIATED TUNNELS CONNECT WITH THE DALY MINE WORKINGS
Comment (Workings): MAZEPAH SHAFT CONNECTS WITH TUNNELS OF THE DALY MINE. DEPTH OF SHAFT PROBABLY LESS THAN 1200 FT
Comment (Geology): NORTH-SOUTH FAULT JUXTAPOSES THE PARK CITY FORMATION AND WEBER QUARTZITE NEAR THE SHAFT. MINERALIZATION, HOWEVER, IS RELATED TO NORTHEAST SET OF FISSURES AND FAULTS
Comment (Development): MAZEPAH SHAFT IS PART OF THE DALY MINE. MAZEPAH SHAFT WAS SUNK ABOUT 1911 TO EXPLORE WESTERN PART OF PROPERTY NOT ON THE DALY - ONTARIO FISSURE SYSTEM. THIS EXPLORATION WAS UNDERTAKEN AFTER MAIN DALY ORES HAD BEEN DEPLETED AND RICH ORES WERE FOUND ON THE ADJACENT ONTARIO PROPERTY
Comment (Location): INFO FROM LAND.ST :1983
Comment (Commodity): RICH SILVER ORE STRUCK BY SHAFT
Comment (Production): PRODUCTION FIGURES ARE REPORTED WITH FIGURES FOR DALY MINE, SEPARATE RECORDS NOT KEPT
Reference (Deposit): BOUTWELL, J.M., 1912, GEOLOGY AND ORE DEPOSITS OF THE PARK CITY DISTRICT, UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER, NO. 77, 231 PP.
Reference (Deposit): ERIKSON, A.J., (EDITOR), 1968, PARK CITY DISTRICT, UTAH: GUIDEBOOK TO THE GEOLOGY OF UTAH, NO. 22, UTAH GEOLOGICAL SOCIETY.
Reference (Deposit): BUTLER, B.S., LOUGHLIN, G.F., HEIKES, V.C., AND OTHERS, 1920, THE ORE DEPOSITS OF UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER, NO. 111, 672 PP.
Reference (Deposit): BAKER, A.A. CALKINS, F.C., CRITTENDEN, M.D., JR., AND BROMFIELD, C.S., 1956, GEOLOGIC MAP OF THE BRIGHTON QUADRANGLE, UTAH: U.S. GEOLOGICAL SURVEY GEOL. QUAD. MAP GQ-534
Reference (Deposit): BARNES, M.P., AND SIMOS, J.S., 1968, ORE DEPOSITS OF THE PARK CITY DISTRICT WITH A CONTRIBUTION ON THE MAYFLO ER LODE, IN ORE DEPOSITS OF THE UNITED STATES: AMER. INST. METALLO ENG., V. II, P. 1102
Reference (Production): BOUTWELL, 1912
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