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Lisbon Valley

halokinetic potash-bearing salt in United States of America

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Geologic information

CountryUnited States of America
Location:-109.2078, 38.1972
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Site typemineral occurrence
Deposit typehalokinetic potash-bearing salt
Evaporite basinParadox
Basin typeintracratonic basin
Geologic unitHermosa Fm-Paradox Mbr
Age
Paleozoic
Carboniferous-Pennsylvanian
Middle Pennsylvanian
Moscovian
Minimum:Paleozoic-Carboniferous-Pennsylvanian-Middle Pennsylvanian-Moscovian
Maximum:Paleozoic-Carboniferous-Pennsylvanian-Middle Pennsylvanian-Moscovian
Commodities
Minerals
Potassium minerals:
Other minerals:
Lithology
Notes:Lisbon Valley fault cuts the anticline.
Geologic map unit-109.2078, 38.1972
Nearby scientific dataFind additional scientific data near this location

Economic information

Production
StatusNone

Reference information

References

Hite, R.J., 1976, A potential target for potash solution mining in cycle 13, Paradox Member, near Moab, Utah: U.S. Geological Survey Open-File Report OF 76-755, 5 p.
Hite, R.J., 1978, Geology of the Lisbon Valley potash deposits, San Juan County, Utah: U.S. Geological Survey Open-File Report OF 78-148, 25 p.
Hite, R.J., and Lohman, S.W., 1973, Geologic appraisal of Paradox basin salt deposits for waste emplacement: U.S. Geological Survey Open-File Report OF 73-114, 75 p.
Ritzma, H.R., 1969, Potash in the San Juan project area, Utah and Colorado, in Mineral resources, San Juan County, Utah, and adjacent areas: Utah Geological and Mineral Survey Special Studies 24, pt. 1.