Bartlett Peak | |
---|---|
Highest point | |
Elevation | 8,519 ft (2,597 m) [1] |
Prominence | 450 ft (137 m) [1] |
Parent peak | Bush Mountain (8,631 ft) [2] |
Isolation | 0.82 mi (1.32 km) [2] |
Coordinates | 31°55′04″N104°52′55″W / 31.9178879°N 104.8818299°W [3] |
Naming | |
Etymology | John Russell Bartlett |
Geography | |
Country | United States |
State | Texas |
County | Culberson |
Protected area | Guadalupe Mountains National Park [1] |
Parent range | Guadalupe Mountains [1] |
Topo map | USGS P X Flat |
Geology | |
Rock age | Lopingian |
Rock type | Limestone [4] |
Climbing | |
Easiest route | class 2 hiking [2] |
Bartlett Peak is an 8,519-foot-elevation (2,597-meter) summit in Culberson County, Texas, United States.
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 4,500 feet (1,372 m) above Salt Basin in three miles (4.8 km). Precipitation runoff from the mountain's slopes drains west to Salt Basin, and east to the Delaware River which is part of the Pecos River watershed. [1] No trail reaches the summit, and the peak is best seen from U.S. Highway 62/180 to the west of the park. [6] The Salt Basin Dunes provides a good location to view the peak from a distance.
The mountain's toponym was officially adopted on November 4, 1938, by the United States Board on Geographic Names to commemorate John Russell Bartlett (1805–1886), one of the United States and Mexican Boundary Commissioners. [3] He passed through this region in the 1850s and wrote one of the best early descriptions of these mountains when in 1854 he published A Personal Narrative of Explorations and Incidents in Texas, New Mexico, California, Sonora and Chihuahua, in which he described the Guadalupe Mountains as "a dark, gloomy-looking range, with bold and forbidding sides, consisting of huge piles of rock, their debris heaped far above the surrounding hills." [6]
Based on the Köppen climate classification, Bartlett Peak is located in a cold semi-arid climate zone with relatively hot summers, calm, mild autumn weather, and cool to cold weather in winter and early spring. [7] Nights are cool, even in summer. Late summer monsoons bring thunderstorms.
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 ruins of a stagecoach station stand near the Pine Springs visitor center. The restored Frijole Ranch contains a small museum of local history and is the trailhead for Smith Spring. The park covers 86,367 acres in the same mountain range as Carlsbad Caverns National Park, about 25 miles (40 km) to the north in New Mexico. The Guadalupe Peak Trail winds through pinyon pine and Douglas-fir forests as it ascends over 3,000 feet (910 m) to the summit of Guadalupe Peak, with views of El Capitan and the Chihuahuan Desert.
Guadalupe Peak, also known as Signal Peak, is the highest natural point in Texas, with an elevation of 8,751 feet (2,667 m) above sea level. 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.
The Guadalupe Mountains 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 Guadalupe Mountains are bordered by the Pecos River valley and Llano Estacado to the east and north, Delaware Mountains to the south, and Sacramento Mountains to the west. One of the clearest exposures of a prehistoric reef is preserved in the mountain range's bedrock geology. Bedrock contains fossils of reef-dwelling organisms from the Permian period, and the geology is widely studied, mostly by stratigraphers, paleontologists, and Paleoecologists.
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Pyramid Peak is an 8,875-foot (2,705-meter) mountain summit located at the western edge of the Saint Elias Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, 22 mi (35 km) southeast of McCarthy, 7 mi (11 km) southeast of Williams Peak, and 6 mi (10 km) south-southeast of Joshua Green Peak. The peak's descriptive local name was reported in 1908 by the United States Geological Survey. Precipitation runoff from the mountain drains into tributaries of the Nizina River, which in turn is part of the Copper River drainage basin.
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