Shaft North of Chloride Canyon

The Shaft North of Chloride Canyon is a copper mine located in Iron county, Utah at an elevation of 5,459 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: Shaft North of Chloride Canyon

State:  Utah

County:  Iron

Elevation: 5,459 Feet (1,664 Meters)

Commodity: Copper

Lat, Long: 37.76056, -113.47389

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 Shaft North of Chloride Canyon

Shaft North of Chloride Canyon MRDS details

Site Name

Primary: Shaft North of Chloride Canyon


Commodity

Primary: Copper


Location

State: Utah
County: Iron
District: Antelope Range District


Land Status

Land ownership: BLM Administrative Area
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

Not available


Production

Not available


Deposit

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


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Form: TABULAR


Structure

Type: R
Description: Basin And Range Faults

Type: L
Description: Northwest Striking Faults And Fracture Zones


Alterations

Alteration Type: L
Alteration Text: Propylitic Alteration


Rocks

Name: Ash-Flow Tuff
Role: Associated
Age Type: Associated Rock Unit
Age Young: Oligocene

Name: Ash-Flow Tuff
Role: Associated
Age Type: Associated Rock
Age Young: Oligocene

Name: Ash-Flow Tuff
Role: Associated
Age Type: Host Rock
Age Young: Oligocene


Analytical Data

Not available


Materials

Ore: Malachite
Gangue: Albite
Gangue: Chlorite


Comments

Comment (Location): INFO FROM LAND.ST :(1975)

Comment (Deposit): VERY MINOR VEIN IN FRACTURE ZONE STRIKING NORTHWEST

Comment (Workings): WORKINGS CONSIST OF ONE TIMBERED SHAFT ABOUT 20 FEET DEEP.

Comment (Geology): SHAFT IS IN PROPYLITICALLY ALTERED ISOM FORMATION


References

Reference (Deposit): SHUBAT, M.A., 1984, UTAH GEOLOGICAL AND MINERAL SURVEY: ON-SITE INVESTIGATION


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