Lisbon Valley Potash Area

The Lisbon Valley Potash Area is a mine located in San Juan county, Utah at an elevation of 6,801 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: Lisbon Valley Potash Area

State:  Utah

County:  San Juan

Elevation: 6,801 Feet (2,073 Meters)

Commodity:

Lat, Long: 38.19722, -109.20778

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 Lisbon Valley Potash Area

Lisbon Valley Potash Area MRDS details

Site Name

Primary: Lisbon Valley Potash Area


Commodity

Tertiary: Potassium
Tertiary: Magnesite


Location

State: Utah
County: San Juan


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: U.S. Bureau Of Land Management And State


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: Lisbon Valley Anticline, Also Area Has Several Faults And Some Flowage


Alterations

Not available


Rocks

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

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


Analytical Data

Not available


Materials

Ore: Sylvite
Ore: Carnallite
Gangue: Halite
Gangue: Dolomite
Gangue: Anhydrite


Comments

Comment (Location): ALSO PARTS OF T30S, R24E; T29 1/2 S, R24E

Comment (Reserve-Resource): SOME MG ORE IS COULD BE DERIVED FROM CARNALLITE BEDS.

Comment (Deposit): DEPOSIT THICKNESS IS ESTIMATE OF SYLVITE LAYERS 5 , 6 , 9 , AND LOWER LAYERS ALTHOUGH THERE MAY BE CONSIDERABLE VARIATION.


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): RITZMA, HOWARD R., 1969 , POTASH IN THE SAN JUAN PROJECT AREA, UTAH AND COLORADO: UTAH GEOL. AND MINERAL SURVEY SPECIAL STUDIES 24 ( PT. 1 )

Reference (Deposit): HITE, R. J., 1978 , THE GEOLOGY OF THE LISBON VALLEY POTASH DEPOSITS, SAN JUAN COUNTY, UTAH: USGS OPEN-FILE REPORT 78 - 148


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