Rosa Tunnel

The Rosa Tunnel is a lead mine located in Salt Lake county, Utah at an elevation of 7,900 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: Rosa Tunnel  

State:  Utah

County:  Salt Lake

Elevation: 7,900 Feet (2,408 Meters)

Primary Mineral: Lead

Lat, Long: 40.53583, -112.17889

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.


Satelite image of the Rosa Tunnel

Rosa Tunnel MRDS details

Site Name

Primary: Rosa Tunnel


Commodity

Primary: Lead


Location

State: Utah
County: Salt Lake
District: Bingham 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: Kennecott Minerals Co.


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Colorado Plateaus
Physiographic Section: High Plateaus Of Utah
Physiographic Detail: Uinta Extension


Mineral Deposit Model

Not available


Orebody

Form: IRREGULAR


Structure

Type: R
Description: Basin And Range

Type: L
Description: Fractures, Fissures And Faults


Alterations

Alteration Type: L
Alteration Text: Dolomitization And Silicification


Rocks

Name: Quartzite
Role: Host
Age Type: Host Rock Unit
Age Young: Pennsylvanian

Name: Quartzite
Role: Host
Age Type: Host Rock
Age Young: Pennsylvanian


Analytical Data

Not available


Materials

Gangue: Quartz
Gangue: Chlorite
Gangue: Calcite
Gangue: Sericite
Gangue: Talc


Comments

Comment (Location): INFO FROM LAND.ST :(1977)

Comment (Deposit): DEPOSIT LIES ON THE SOUTHWESTERN FLANK OF BINGHAM SYNCLINE. HOST ROCKS ARE HIGHLY DEFORMED AND ALTERED. ORE IS COMPLETELY OXIDIZED.

Comment (Workings): 1,000 FT TUNNEL; COLLAPSED; INACESSIBLE

Comment (Geology): THE FRACTURE ZONE CARRIES A RED-BROWN, GRAY AND BLACK OCHEROUS GOUGE.


References

Reference (Deposit): BOUTWELL, J.M., 1905, ECONOMIC GEOLOGY OF THE BINGHAM MINING DISTRICT, UTAH: USGS P.P. 38, 410P.

Reference (Deposit): BRAY, E.R., WILSON, J.C., 1975, GUIDE BOOK TO THE BINGHAM MINING DISTRICT: SOCIETY OF ECONOMIC GEOLOGISTS

Reference (Deposit): COOK, D.R., 1961, GEOLOGY OF THE BINGHAM MINING DISTRICT AND NORTHERN OQUIRRH MOUNTAIN, GUIDE BOOK TO THE GEOLOGY OF UTAH, NO. 16 UTAH GEOLOGICAL SOCIETY, 145P.

Reference (Deposit): BUTLER, B.S., ET. AL., 1920, THE ORE DEPOSITS OF UTAH: USGS P.P. 111, 672P.