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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
Pages in category "Mountain ranges of Texas" The following 14 pages are in this category, out of 14 total. This list may not reflect recent changes. B. Beach ...
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 ...
It is located in Guadalupe Mountains National Park, and is part of the Guadalupe Mountains range in southeastern New Mexico and West Texas. The mountain is about 90 miles (140 km) east of El Paso and about 50 miles (80 km) southwest of Carlsbad, New Mexico. The peak rises more than 3,000 feet (910 m) above the arid floor of the Chihuahuan Desert.
Map all coordinates using OpenStreetMap. Download coordinates as: KML; ... Pages in category "Mountains of Texas" The following 59 pages are in this category, out of ...
The Guadalupe Mountains (Spanish: Sierra de Guadalupe) are a mountain range located in West Texas and southeastern New Mexico.The range includes the highest summit in Texas, Guadalupe Peak, 8,751 ft (2,667 m), and the "signature peak" of West Texas, El Capitan, both of which are located within Guadalupe Mountains National Park.
The mountains occupy a rough square about 50 km (31 mi) on each side. The mountains are of volcanic origin composed of strata associated with eruptions of the Trans-Pecos Volcanic Field 35 million years ago. [2] The highest peak in the Davis Mountains is Mount Livermore at 2,555 m (8,383 ft) the fifth-highest peak in Texas.
The Franklin Mountains of Texas (Spanish: Sierras de los Mansos [1]) are a small range 23 miles (37 km) long, 3 miles (5 km) wide that extend from El Paso, Texas, north into New Mexico. [2] The Franklins were formed due to crustal extension related to the Cenozoic Rio Grande rift .
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