The Thaynes Shaft is a lead and silver mine located in Summit county, Utah at an elevation of 8,619 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: 8,619 Feet (2,627 Meters)
Primary Mineral: Lead, Silver
Lat, Long: 40.625, -111.53833
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.
Thaynes Shaft MRDS details
Primary: Thaynes Shaft
Secondary: Silver King Coalition Group
Secondary: United Park City Mines
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
Deposit Type: Replacement
Operation Type: Unknown
Discovery Year: 1875
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, Iron Hollow Syncline
Description: Crescent Fissure
Alteration Type: L
Alteration Text: Oxidation
Age Type: Associated Rock
Age Young: Oligocene
Age Type: Associated Rock Unit
Age Young: Oligocene
Analytical Data: AVERAGE SILVER KING MINE ORE HAD GRADE OF .024 OZ/TON AU, 18.45 OZ/TON AG, 13.52% PB, .495% CU, 10.68% ZN
Comment (Location): LOCATED ON THE NORTHERN EDGE OF THE QUADRANGLE ; INFO FROM LAND.ST :1983
Comment (Development): SHAFT POST-DATES BOUTWELL'S 1912 PUBLICATION
Comment (Deposit): SHAFT ACCESSES THE TUNNELS WHICH DEVELOPED THE EXTENSIVE REPLACEMENT DEPOSITS IN THE SILVER KING MINE AREA. JENNY BED OF THE LOWER PARK CITY FORMATION WAS EXTENSIVELY REPLACED
Comment (Workings): SHAFT ACCESSES A TUNNEL WHICH CONNECTS THE SPIRO AND ALLIANCE TUNNELS. SHAFT POST-DATES 1912
Comment (Deposit): SHAFT ACCESSES A TUNNEL WHICH CONNECTS THE SPIRO AND ALLIANCE TUNNELS. SHAFT IS PART OF THE SILVER KING COALITION MINE CO. WORKINGS. ; INFO.SRC : 1 PUB LIT
Comment (Deposit): Discovery Year: LATE 1800'S
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.
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