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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 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 ...
Map of the part of the region in Texas. Red is the core; pink represents the counties sometimes included in the region. Active Permian Basin pumpjack east of Andrews, TX Aerial view of oil fields of the Permian Basin in Ward County, TX. Due to its economic significance, the Permian Basin has also given its name to the geographic region in which ...
USGS map colored by paleogeological areas and demarcating the sections of the U.S. physiographic regions: Laurentian Upland (area 1), Atlantic Plain (2-3), Appalachian Highlands (4-10), Interior Plains (11-13), Interior Highlands (14-15), Rocky Mountain System (16-19), Intermontane Plateaus (20-22), & Pacific Mountain System (23-25) The legend ...
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
The term is considered synonymous with Far West Texas, a subdivision of West Texas. [2] The Trans-Pecos is part of the Chihuahuan Desert , the largest desert in North America . It is the most mountainous and arid portion of the state, and most of its vast area (outside the city of El Paso ) is sparsely populated.
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.
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