Phosphoria Formation Stratigraphic range: Early Permian |
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Type | Geological formation |
Underlies | Dinwoody Formation |
Overlies | Casper Formation, Park City Formation, Tensleep Sandstone |
Area | 350,000 sq. km (140,000 sq. mi) |
Thickness | Up to 420 metres (1,380 ft) |
Lithology | |
Primary | Limestone, dolostone, shale |
Other | Chert, phosphorite, sandstone |
Location | |
Region | Idaho, Montana, Utah, Wyoming |
Country | USA |
Type section | |
Named for | Phosphoria Gulch, Idaho |
Named by | Richards and Mansfield, 1912 |
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The Phosphoria Formation of the western United States is a geological formation of Early Permian age. It represents some 15 million years of sedimentation, reaches a thickness of 420 metres (1,380 ft) and covers an area of 350,000 square kilometres (140,000 sq mi).
The formation includes phosphorite beds that are an important source of phosphorus. They have been mined in southeastern Idaho, northern Utah, western Wyoming, and southwestern Montana. Low concentrations of uranium are present in the phosphorite beds, and a vanadium-enriched zone is present in western Wyoming and southeastern Idaho. Many of the Phosphoria shales are rich in organic matter and are petroleum source rocks, and petroleum has been produced from some of the dolostones in the formation.
The Phosphoria Formation was deposited under marine conditions in a foreland basin located between the Paleozoic continental margin and the North American cratonic shelf.
The formation is commonly subdivided, from the top downward, as follows:
The Phosphoria is underlain by the Pennsylvanian-Permian Casper Formation or, depending on the location, by the Park City Formation or the Tensleep Sandstone, and it is overlain by the Triassic Dinwoody Formation. The upper boundary is placed at the top of the uppermost phosphorite bed and below the tan calcareous siltstone of Dinwoody formation. The lower boundary is marked by a thin phosphorite that contains abundant fish scales and bones.