Shumard Peak | |
---|---|
Highest point | |
Elevation | 8,636 ft (2,632 m) [1] |
Prominence | 900 ft (274 m) [1] |
Parent peak | Guadalupe Peak (8,751 ft) [1] |
Isolation | 1.32 mi (2.12 km) [2] |
Coordinates | 31°54′27″N104°52′28″W / 31.9075511°N 104.8743940°W [3] |
Naming | |
Etymology | George Getz Shumard |
Geography | |
Country | United States |
State | Texas |
County | Culberson |
Protected area | Guadalupe Mountains National Park [1] |
Parent range | Guadalupe Mountains [1] |
Topo map | USGS Guadalupe Peak |
Geology | |
Rock age | Lopingian |
Rock type | Limestone [4] |
Climbing | |
Easiest route | class 2 hiking [2] |
Shumard Peak is an 8,636-foot-elevation (2,632-meter) summit in Culberson County, Texas, United States.
Shumard Peak is located in Guadalupe Mountains National Park and with more recent accurate Lidar measurements, it ranks as the second-highest peak in the Guadalupe Mountains and in the state of Texas, [1] moving up from previous third in outdated sources. The mountain is composed of late Permian limestone and Capitan Formation like the other peaks in the Guadalupe Mountains. [5] Topographic relief is significant as the summit rises over 4,600 feet (1,402 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] The mountain's toponym was officially adopted on November 4, 1938, by the United States Board on Geographic Names to commemorate George Getz Shumard (1823–1867), who made the first geologic exploration of the Guadalupe Mountains in the 1850s. [3] During an 1852 exploration, Shumard discovered the presence of Permian fossils in the area of the Guadalupe Mountains. [6]
Based on the Köppen climate classification, Shumard 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.
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.
Bannock Peak is a 10,329-foot (3,148-metre) mountain summit in the southern section of the Gallatin Range in Yellowstone National Park, in the U.S. state of Wyoming. The peak ranks as the sixth-highest peak in the Gallatin Range. Precipitation runoff from the mountain drains west into headwaters of the Gallatin River and east into Panther Creek which is a tributary of the Gardner River. Topographic relief is significant as the summit rises nearly 2,000 feet above Panther Creek in one mile (1.6 km). This mountain's toponym was officially adopted in 1897 by the United States Board on Geographic Names.
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Williams Peak is a 7,431-foot 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, 15 mi (24 km) east-southeast of McCarthy, and 4 mi (6 km) west-southwest of Joshua Green Peak in the Dan Creek area. Precipitation runoff from the mountain drains into tributaries of the Nizina River, which in turn is part of the Copper River drainage basin.
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.
Mount Emma is a 13,581-foot-elevation (4,139-meter) mountain summit located in San Miguel County of Colorado, United States. It is situated three miles north of the community of Telluride, on the south side of Yankee Boy Basin, in the Uncompahgre National Forest. It is part of the Sneffels Range which is a subset of the San Juan Mountains, which in turn is part of the Rocky Mountains. Mount Emma is situated west of the Continental Divide, two miles south of Mount Sneffels, and 0.8 mile south of Gilpin Peak, the nearest higher neighbor. Emma ranks as the 197th-highest peak in Colorado, and the 10th-highest in the Sneffels Range. Topographic relief is significant as the south aspect rises 4,830 feet above Telluride in approximately three miles. An ascent of Mt. Emma is a difficult climb with 2,180 feet of elevation gain covering three miles from Yankee Boy Basin, or 4,836 feet of elevation gain from Telluride. This mountain's name was officially adopted by the U.S. Board on Geographic Names.
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