The Salt Valley Anticline is a mine located in Grand county, Utah at an elevation of 4,701 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: 4,701 Feet (1,433 Meters)
Commodity:
Lat, Long: 38.92167, -109.83611
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.
Salt Valley Anticline MRDS details
Site Name
Primary: Salt Valley Anticline
Commodity
Tertiary: Magnesite
Tertiary: Potassium
Location
State: Utah
County: Grand
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
Not available
Ownership
Owner Name: W. J. Coleman, Sawyer Petrol.
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: L
Physiography
General Physiographic Area: Intermontane Plateaus
Physiographic Province: Colorado Plateaus
Physiographic Section: Canyon Lands
Physiographic Detail: Lisbon Prong - Salt Anticline Region
Mineral Deposit Model
Not available
Orebody
Form: TABULAR
Structure
Type: R
Description: Paradox Basin
Type: L
Description: Some Faulting And Folding
Alterations
Not available
Rocks
Name: Shale
Role: Host
Age Type: Host Rock
Age Young: Pennsylvanian
Name: Shale
Role: Host
Age Type: Host Rock Unit
Age Young: Pennsylvanian
Analytical Data
Not available
Materials
Ore: Sylvite
Ore: Carnalite
Gangue: Halite
Gangue: Anhydrite
Gangue: Dolomite
Comments
Comment (Reserve-Resource): DEPOSIT WOULD HAVE SOME COMPLEX STRUCTURE WHICH WOULD LIMIT OR PROHIBIT MINING; MG WOULD BE DERIVED FROM CARNALITE DEPOSITS.
Comment (Location): SEC. 1 T23S R19E; T23S R20E; T23S, R21E; T24S R21E
Comment (Deposit): DEPOSIT INFORMATION FROM DRILL HOLE DATA. THERE IS SOME FOLDING AND FLOWAGE OF THIS DEPOSIT WHICH MAY CAUSE PROBLEMS IN SOLUTION MINING. DEPTHS TO DEPOSIT VARY CONSIDERABLY THROUGHOUT DEPOSIT.
Comment (Workings): NO WORKINGS ON THIS DEPOSIT; WOULD HAVE TO BE MINED BY SOLUTION MINING OR IN PLACES BY CONVENTIONAL MINING
Comment (Geology): THE SALT VALLEY ANTICLINE IS THE NORTHERN MOST SEGMENT OF THE SALT VALLEY - CACHE VALLEY - FISHER VALLEY - SINBAD VALLEY SYSTEM.
References
Reference (Deposit): HITE, R. J., AND LOHMAN; 1973 , GEOLOGIC APPRAISAL OF PARADOX BASIN SALT DEPOSITS FOR WASTE EMPLACEMENT: USGS OPEN-FILE REPORT
Reference (Deposit): HITE, R. J., 1964 , SALINES, IN MINERAL AND WATER RESOURCES OF UTAH: UTAH GEOL. AND MINERAL SURVEY BULL 73 P. 206-215 .
Reference (Reserve-Resource): MCCARTHY, B. M., 1978 , AND HITE, R. J., 1964 , SALINES
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