Winamuck Mine 1867

The Winamuck Mine 1867 is a gold, lead, silver, copper, and zinc mine located in Salt Lake county, Utah at an elevation of 6,250 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

Name: Winamuck Mine 1867

State:  Utah

County:  Salt Lake

Elevation: 6,250 Feet (1,905 Meters)

Commodity: Gold, Lead, Silver, Copper, Zinc

Lat, Long: 40.54306, -112.14500

Map: View on Google Maps

Satelite View

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Satelite image of the Winamuck Mine 1867

Winamuck Mine 1867 MRDS details

Site Name

Primary: Winamuck Mine 1867


Commodity

Primary: Gold
Primary: Lead
Primary: Silver
Primary: Copper
Primary: Zinc


Location

State: Utah
County: Salt Lake
District: Bingham District


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Years of Production:
Organization:
Significant: N


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Form: LENTICULAR


Structure

Type: L
Description: Fracture (N 40 - 60 W, 45 - 70 Ne), Fault Planes (N 6 - 10 W, 80 Ne)


Alterations

Not available


Rocks

Not available


Analytical Data

Analytical Data: 1872 : 34.98 % PB, 51.46 OZ AG. THREE ASSAYS FROM PIPES AVERAGE 5.9 % PB, 131.6 OZ AG, $.90 AU, 4.6 % CU, 13.9 % ZN.


Materials

Ore: Chalcocite
Ore: Sphalerite
Ore: Tetrahedrite
Ore: Chalcopyrite
Ore: Pyrite
Ore: Pyrargyrite
Ore: Cubanite
Gangue: Gypsum
Gangue: Clay


Comments

Comment (Location): INCLUDES NO. 112 , WINDLASS BUSHNELL, DAVIS, MOUNTAIN MAID, AND SAVAGE TUNNELS.

Comment (Production): TOTAL OUTPUT TO 1880 WAS $1,500,000

Comment (Deposit): ALONG CONTACT ZONE

Comment (Workings): SERIES OF ADITS AND A 400 FT INCLINE

Comment (Geology): GEOL.DESC: THE FOOTWALL OF THE ORE IS NORMAL QUARTZITE, THE HANGING WALL IS A MASSIVE GRAY-BLACK DRY FINE GRAINED SILICEOUS ROCK.


References

Reference (Deposit): USGS PROF. PAPER 38. P. 300

Reference (Deposit): USGS MIN. RES. 1920, PT. 1, P. 303.

Reference (Deposit): USBM MIN. RES. 1927, PT. 1, P. 665.

Reference (Deposit): CONSV. DIV. COMP. DATE, 02-18-1965


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