Bishop Cap Formation

Last updated
Bishop Cap Formation
Stratigraphic range: Moscovian–Kasimovian
Type Formation
Underlies Panther Seep Formation
Overlies Berino Formation
Thickness180 m (590 ft)
Lithology
Primary Shale
Other Limestone
Location
Coordinates 31°58′0″N106°31′30″W / 31.96667°N 106.52500°W / 31.96667; -106.52500
Region New Mexico
Texas
Country United States
Type section
Named forBishop Cap (mountain)
Named byL.A. Nelson
Year defined1937
Usa edcp relief location map.png
Green pog.svg
Bishop Cap Formation (the United States)
La Tuna Map.jpg
Green pog.svg
Bishop Cap Formation (Texas)

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]

Contents

Description

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]

Fossils

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]

History of investigation

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]

See also

Related Research Articles

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.

<span class="mw-page-title-main">La Pasada Formation</span> Geologic formation in New Mexico, US

The La Pasada Formation is a geologic formation in the southern Sangre de Cristo Mountains of New Mexico. It preserves fossils dating back to the early to middle Pennsylvanian.

<span class="mw-page-title-main">Red House Formation</span> Geologic formation in New Mexico, US

The Red House Formation is a geologic formation found in the Caballo Mountains in New Mexico. It preserves fossils dating back to the middle to late Pennsylvanian.

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.

<span class="mw-page-title-main">Alamitos Formation</span> Geologic formation of New Mexico

The Alamitos Formation is a geologic formation exposed in the southern Sangre de Cristo Mountains of New Mexico. It preserves fossils dating back to the late Pennsylvanian to early Permian periods.

<span class="mw-page-title-main">Bursum Formation</span>

The Bursum Formation is a geologic formation in New Mexico. It preserves fossils dating back to the Early Permian period.

The Gray Mesa Formation is a geologic formation in New Mexico. Its fossil assemblage dates the formation to the Moscovian age of the Pennsylvanian.

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.

The Holder Formation is a geologic formation in the Sacramento Mountains of New Mexico. It preserves fossils dating back to the late Pennsylvanian.

The Onate Formation is a geologic formation that is exposed in most of the highlands of south-central New Mexico. It preserves fossils dating back to the middle Devonian period.

<span class="mw-page-title-main">Atrasado Formation</span> Geologic formation in New Mexico

The Atrasado Formation is a geologic formation in New Mexico. Its fossil assemblage dates the formation to the Kasimovian age of the Pennsylvanian. It was formerly known locally as the Wild Cow Formation or the Guadelupe Box Formation.

<span class="mw-page-title-main">Madera Group</span> Group of geologic formations in New Mexico, United States

The Madera Group is a group of geologic formations in northern New Mexico. Its fossil assemblage dates the formation to the middle to late Pennsylvanian period.

<span class="mw-page-title-main">Porvenir Formation</span> Geologic formation ion New Mexico, US

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.

References

  1. 1 2 3 Harbour, R.L. (1972). "Geology of the northern Franklin Mountains, Texas and New Mexico". U.S. Geological Survey Bulletin. 1298. doi: 10.3133/b1298 .
  2. Kues, B.S.; Giles, K.A. (2004). "The late Paleozoic Ancestral Rocky Mountain system in New Mexico". In Mack, G.H.; Giles, K.A. (eds.). The geology of New Mexico. A geologic history (Special Volume 11). New Mexico Geological Society. pp. 95–136.
  3. 1 2 3 Kues, B.S. (2001). "The Pennsylvanian System in New Mexico; Overview with suggestions for revisions of stratigraphic nomenclature" (PDF). New Mexico Geology. 23 (4): 103–122. Retrieved 18 September 2020.
  4. Nelson, L.A. (1940). "Paleozoic stratigraphy of the Franklin Mountains, West Texas". American Association of Petroleum Geologists Bulletin. 24 (1): 157–172. doi:10.1306/3D93319A-16B1-11D7-8645000102C1865D.
  5. 1 2 Thompson, E.; Yochelson, E.; Flower, R. (1980). "Aptychi from the Pennsylvanian of West Texas". Journal of Paleontology. 54 (5): 903–909. JSTOR   1304355.
  6. Nelson, L.A. (1937). "Gastropoda from the Pennsylvanian (Magdalena) of the Franklin Mountains of west Texas [abstract of thesis]". Colorado University Studies. 25 (1): 89–91.