The Lucky Bill Shaft is a lead and silver mine located in Summit county, Utah at an elevation of 8,934 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: 8,934 Feet (2,723 Meters)
Commodity: Lead, Silver
Lat, Long: 40.60667, -111.50472
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.
Lucky Bill Shaft MRDS details
Site Name
Primary: Lucky Bill Shaft
Secondary: Lucky Bill Group
Secondary: United Park City Mines
Commodity
Primary: Lead
Primary: Silver
Secondary: Zinc
Secondary: Copper
Secondary: Gold
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
Type: Underground
Ownership
Owner Name: United Park City Mines Co.
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year First Production: 1885
Year Last Production: 1895
Discovery Year: 1875
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Middle Rocky Mountains
Physiographic Detail: Wasatch Mountains
Mineral Deposit Model
Not available
Orebody
Form: TABULAR
Structure
Type: R
Description: Cottonwood - Uinta Arch, Park City Anticline, Sevier Overthrust Belt
Type: L
Description: Quartzite And Intrusive Show Considerable Fracturing And Fissuring
Alterations
Alteration Type: L
Alteration Text: Oxidation
Rocks
Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Pennsylvanian
Name: Diorite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Oligocene
Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Oligocene
Name: Diorite
Role: Associated
Age Type: Host Rock Unit
Age Young: Pennsylvanian
Analytical Data
Not available
Materials
Ore: Chalcopyrite
Ore: Galena
Ore: Sphalerite
Ore: Gold
Ore: Tetrahedrite
Gangue: Calcite
Gangue: Quartz
Comments
Comment (Location): INFO FROM LAND.ST :1983
Comment (Production): NO RECORDED PRODUCTION BUT THERE WAS PROBABLY A SMALL PRODUCTION
Comment (Development): ACTIVE EXPLORATION BEGAN IN THE 1880'S. BY 1888 THE TUNNEL WAS 775 FT LONG AND THE SHAFT 75 FT DEEP. IN 1892 A VEIN WAS STRUCK IN THE SHAFT AT A DEPTH OF 300 FT BUT NO ORE OF MUCH VALUE WAS FOUND. IN 1901 AND 1902 THERE WAS SPECULATION THAT THIS PROPERTY WAS THE APEX OF THE DALY WEST AND QUINCY ORE BODIES, BUT THIS WAS LATER SHOWN TO BE FALSE, PROPERTY INACTIVE SINCE 1902, PROPERTY NOW PART OF THE UNITED PARK CITY MINES CO. HOLDINGS
Comment (Deposit): ORE REPORTED HIT AT THE 300 FT LEVEL IN THE SHAFT. NO MAJOR ORE BODIES WERE EVER FOUND. ORE IS PRESUMABLY PB-AG TYPE LOCATED IN VEINS WITH NORTHEAST STRIKE
Comment (Workings): SHAFT IS AT LEAST 1000 FT BENEATH THE SURFACE WITH ADITS AT FOUR LEVELS. 200 FT LEVEL EXTENDS 250 FT NORTHEAST FROM THE SHAFT, 300 FT LEVEL EXTENDS 150 FT NORTHEAST OF THE SHAFT, 500 FT LEVEL EXTENDS 350 FT NORTHWEST OF THE SHAFT AND A 1000 FT LEVEL EXTENDS 500 FT SOUTH FROM THE SHAFT. ADITS TOTAL 1250 FT IN LENGTH. WORKINGS DO NOT CONNECT WITH THE MAIN PARK CITY NETWORK OF UNDERGROUND WORKINGS
Comment (Deposit): Discovery Year: 1870'S
References
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., 1966, GEOLOGIC MAP OF THE BRIGHTON QUADRANTGLE, UTAH: U.S. GEOLOGICAL SURVEY GEOL. QUAD. MAP GQ-534
Reference (Production): BOUTWELL, 1912
The Top Ten Gold Producing States
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.
