Bishop Cap Formation | |
---|---|
Stratigraphic range: | |
Type | Formation |
Underlies | Panther Seep Formation |
Overlies | Berino Formation |
Thickness | 180 m (590 ft) |
Lithology | |
Primary | Shale |
Other | Limestone |
Location | |
Coordinates | 31°58′0″N106°31′30″W / 31.96667°N 106.52500°W |
Region | New Mexico Texas |
Country | United States |
Type section | |
Named for | Bishop Cap (mountain) |
Named by | L.A. Nelson |
Year defined | 1937 |
The Bishop Cap Formation is a geologic formation in the Franklin Mountains of southern New Mexico and western Texas and the Hueco Mountains of western Texas. It preserves fossils dating back to the Moscovian to Kasimovian Ages of the early Pennsylvanian. [1] [2]
The formation consists of brown to gray shale alternating with thin ray ledges of limestone. Shale makes up 65 to 75 percent of the formation. The total thickness is up to 180 meters (590 ft). [3] The formation rests on the Berino Formation [4] and is overlain by the Panther Seep Formation. [3]
The formation is highly fossiliferous, with a fauna dominated by snails, brachiopods ( Neospirifer , Crurithyris , Mesolobus ), [5] and clams, but is less diverse than the underlying Berino Formation. [1] The lower beds contain the fusulinids Wedekindellina euthysepta and Fusulina distenta. [1] Opercula of cephalopods (possibly Liroceras ) have been found in the formation, as have shells of Bellerophon , Phestia , and Euphemites . [5]
The unit was designated the Bishop Cap Member of the Magdalena Group by L.A. Nelson in 1937. [6] In 2001, B. Kues recommended abandoning the Magdalena Group and raising its members, including the Bishop Cap, to formation rank. [3]
The Bone Spring Formation is a geologic formation found in the Delaware Basin in Texas and New Mexico. It preserves fossils dating back to the Leonardian Age of the Permian Period.
The Cutoff Formation is a geologic formation in Texas and New Mexico, US. It preserves fossils dating back to the Permian period.
The Hueco Formation is a geologic formation in west Texas and southern New Mexico. It preserves fossils dating back to the early Permian period.
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The Panther Seep Formation is a geologic formation found in the mountain ranges of south-central New Mexico. It preserves fossils dating back to the late Pennsylvanian to early Permian.
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The Berino Formation is a geologic formation in the Franklin Mountains of southern New Mexico and western Texas. It preserves fossils dating back to the middle Pennsylvanian.
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The Porvenir Formation is a geologic formation exposed in the southeastern Sangre de Cristo Mountains of New Mexico. It preserves fossils dating back to the middle Pennsylvanian period.
The La Tuna Formation is a geologic formation in the Franklin Mountains of southern New Mexico and western Texas and the Hueco Mountains of western Texas. It preserves fossils dating back to the Bashkirian Age of the early Pennsylvanian.
The Beeman Formation is a geologic formation in the Sacramento Mountains of New Mexico. It preserves fossils dating back to the Kasimovian Age of the Pennsylvanian Period.
The Bar B Formation is a geologic formation found the Caballo Mountains of New Mexico. It preserves fossils showing it was deposited in the middle to late Pennsylvanian.
The Lead Camp Limestone is a geologic formation in the San Andres Mountains of New Mexico. It preserves fossils dating back to the middle Pennsylvanian.
The Victorio Peak Formation is a geologic formation found in the Delaware Basin in Texas and New Mexico. It preserves fossils dating back to the Leonardian Age of the Permian Period.