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In the Permian geologic period, North-Central Texas was a part of the western coastal zone of equatorial Pangea, a super-continental land mass. [1] Nearby uplifts and mountainous regions, such as the Muenster Arch and Red River Uplift, the Wichita, Arbuckle, and Ouachita mountains developed by the end of the Pennsylvanian, [2] providing elevated topography to the north and east during the Permian.
The Wichita Group is the oldest of the three groups, having been deposited in the Sakmarian age. [12] The Wichita Group contains some of the richest fossil deposits in the red beds, including the Geraldine Bonebed in Archer County. [12] The Pease River Group is the most recent deposition, occurring during the Guadalupian epoch. [12]
The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. [1] It is the principal relief system in the Southern Oklahoma Aulacogen , being the result of a failed continental rift.
Shaded relief map of the Llano Estacado. Texas contains a wide variety of geologic settings. The state's stratigraphy has been largely influenced by marine transgressive-regressive cycles during the Phanerozoic, with a lesser but still significant contribution from late Cenozoic tectonic activity, as well as the remnants of a Paleozoic mountain range.
The Archer City Formation is a geological formation in north-central Texas, preserving fossils from the Asselian and early Sakmarian stages of the Permian period.It is the earliest component of the Texas red beds, introducing a tropical ecosystem which will persist in the area through the rest of the Early Permian.
Pages for logged out editors learn more. Contributions; Talk; Geology of Wichita Falls, Texas
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The Bend Arch–Fort Worth Basin Province is a major petroleum producing geological system which is primarily located in North Central Texas and southwestern Oklahoma.It is officially designated by the United States Geological Survey (USGS) as Province 045 and classified as the Barnett-Paleozoic Total Petroleum System (TPS).