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Guadalupe Mountains National Park is a national park of the United States in the Guadalupe Mountains, east of El Paso, Texas. The mountain range includes Guadalupe Peak , the highest point in Texas at 8,751 feet (2,667 m), and El Capitan used as a landmark by travelers on the route later followed by the Butterfield Overland Mail stagecoach line.
The Guadalupe Mountains reach their highest point at Guadalupe Peak, the highest point in Texas, [5] with an elevation of 8,751 feet (2,667 m). [6] The range lies southeast of the Sacramento Mountains and east of the Brokeoff Mountains. The mountain range extends north-northwest and northeast from Guadalupe Peak in Texas into New Mexico. [1]
Guadalupe Peak, also known as Signal Peak, [3] is the highest natural point in Texas, [4] with an elevation of 8,751 feet (2,667 m) above sea level. [1] It is located in Guadalupe Mountains National Park , and is part of the Guadalupe Mountains range in southeastern New Mexico and West Texas .
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 274 m
Bartlett Peak is located in Guadalupe Mountains National Park and it ranks as the fourth-highest peak in the Guadalupe Mountains, the park, the county, and in the state of Texas. [5] The mountain is composed of late Permian limestone like the other peaks in the Guadalupe Mountains. Topographic relief is significant as the summit rises over ...
Quitman Mountains: series of calderas from the Eocene period that includes volcanic rocks Mitre Peak: contains 35 million-year-old rhyolite lava from the Davis Mountains Show comments
El Capitan (Spanish: El Capitán) is a peak in Culberson County, Texas, located within Guadalupe Mountains National Park. [2] The 10th-highest peak in Texas at 8,085 ft (2,464 m), El Capitan is part of the Guadalupe Mountains, an exposed portion of a Permian period reef uplifted and exposed by tectonic activity during the late Cretaceous period. [3]
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