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The most complex Natural Region, it includes Sand Hills, the Stockton Plateau, desert valleys, wooded mountain slopes and desert grasslands. The Basin and Range Province is in West Texas, west of the Pecos River, beginning with the Davis Mountains on the east and the Rio Grande to its west and south. The Trans-Pecos region is the only part of ...
Peaks in the state of Texas [1] [2] [3] Mountain Peak Elevation Prominence Isolation Location Mountain range County; Guadalupe Peak: 8,751 ft 2667 m: 3,031 ft 924 m: 72.6 mi 116.9 km Guadalupe Mountains: Culberson: Shumard Peak: 8,635 ft 2632 m: 899 ft
The Permian Basin covers more than 86,000 square miles (220,000 km 2), [1] and extends across an area approximately 250 miles (400 km) wide and 300 miles (480 km) long. [2] The Texas cities of Midland, Odessa and San Angelo serve as headquarters for some of the oil production activities in the basin.
The Edwards Plateau is a geographic region forming the crossroads of Central, South and West Texas, United States.It is named in honor of Haden Edwards. [2] It is bounded by the Balcones Fault to the south and east; the Llano Uplift and the Llano Estacado to the north; and the Pecos River and Chihuahuan Desert to the west. [3]
Big Bend area map Casa Grande is a prominent peak in the Chisos Mountains of the Big Bend area of west Texas. The view is from the Pinnacles Trail in Big Bend National Park . The Big Bend is part of the Trans-Pecos region in southwestern Texas , United States along the border with Mexico , north of the prominent bend in the Rio Grande for which ...
Location County Ownership Description Attwater Prairie Chicken Preserve: 1968: Colorado: federal/US Fish & Wildlife Service: Contains the only significant segment of gulf coastal prairie. Bayside Resaca Area: 1980
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.
This page was last edited on 24 February 2022, at 13:19 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
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