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Casa Grande Peak
Casa Grande Peak is a mountain summit in Brewster County, Texas, United States. Description Casa Grande Peak is located in Big Bend National Park and the Chisos Mountains. It ranks as the fifth-highest peak in this park, mountain range, and county, but only the 26th-highest in Texas. The peak is an extra-caldera vent, or volcanic dome, of the Pine Canyon caldera which formed about 32–35 million years ago during a period of volcanic activity. United States Geological Survey, 2010. Although modest in elevation, is significant as the summit rises 2,000 feet (610 m) above Chisos Basin in less than . B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toll Mountain
Toll Mountain is a summit in Brewster County, Texas, United States. Description Toll Mountain is located in the Chisos Mountains. It ranks as the fourth-highest peak in Big Bend National Park, Brewster County, and the Chisos Mountains, but only the 25th-highest in Texas. The mountain is composed of extrusive volcanic rock which formed during the Oligocene period. Based on the Köppen climate classification, Toll Mountain is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains into Oak Creek, Blue Creek, and Juniper Draw which are all part of the Rio Grande The Rio Grande ( or ) in the United States or the Río Bravo (del Norte) in Mexico (), also known as Tó Ba'áadi in Navajo language, Navajo, is one of the principal rivers (along with the Colorado River) in the Southwestern United States a ... watershed. Topographic relief is significant as the summit rises 2,600 feet (792&nb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Grande
The Rio Grande ( or ) in the United States or the Río Bravo (del Norte) in Mexico (), also known as Tó Ba'áadi in Navajo language, Navajo, is one of the principal rivers (along with the Colorado River) in the Southwestern United States and in northern Mexico. The length of the Rio Grande is , making it the List of longest rivers of the United States (by main stem), 4th longest river in the United States and in North America by main stem. It originates in south-central Colorado, in the United States, and flows to the Gulf of Mexico. The Rio Grande drainage basin (watershed) has an area of ; however, the endorheic basins that are adjacent to and within the greater drainage basin of the Rio Grande increase the total drainage-basin area to . The Rio Grande with Rio Grande Valley (landform), its fertile valley, along with its tributaries, is a vital water source for seven U.S. and Mexican states, and flows primarily through arid and semi-arid lands. After traversing the length ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of The United States
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Texas
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ward Mountain (Texas)
Ward Mountain is a summit in Brewster County, Texas, United States. Description Ward Mountain is located on the west side of the Chisos Mountains in Big Bend National Park. The mountain is composed of rhyolite (volcanic rock) and Chisos Formation which formed during the Oligocene period. Topographic relief is significant as the summit rises 2,500 feet (762 m) above Cottonwood Creek near Ward Spring in . Based on the Köppen climate classification, Ward Mountain is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains into Cottonwood Creek which is part of the Rio Grande watershed. The lower slopes of the mountain are covered by juniper, oak, and piñon. The mountain's toponym was officially adopted on March 9, 1939, by the United States Board on Geographic Names. The namesake was Johnny Ward, a cowboy from the nearby G4 ranch. The G4 ranch manager Captain Jim Gillette trusted nineteen-yea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Emory Peak
Emory Peak, located in Big Bend National Park, is the highest peak in the Chisos Mountains and the highest in Brewster County. The peak is named for William H. Emory, the chief surveyor of the U.S. Boundary Survey team of 1852. From the Chisos Basin the peak appears to be a minor ridge, while the summit of Casa Grande, one mile closer, seems to be much taller. From the west, Emory Peak is clearly visible as a point slightly higher than most of the mountain range. The peak can be reached by a moderate hike on a well-marked path across steep rocky terrain with an elevation gain of approximately . The Emory Peak Trail is about long. The trail is reached by climbing the Pinnacles Trail from the Chisos Basin trailhead. Once at the base there is a semi-technical rock scramble to navigate before reaching the summit. No gear is needed for this climb although hikers should take great care. High-desert flora and fauna including alligator juniper ('' Juniperus deppeana''), pinyon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crown Mountain (Texas)
Crown Mountain is a summit in Brewster County, Texas, United States. Description Crown Mountain is located in Big Bend National Park and the Chisos Mountains. It ranks as the sixth-highest peak in this park, mountain range, and county, but only the 34th-highest in Texas. The mountain is composed of volcanic rock of the Chisos Formation which formed during the Paleogene period. Robert G. Bohannon, 2011, U.S. Geological Survey. Although modest in elevation, is significant as the summit rises nearly 2,000 feet (610 m) above Pine Canyon in , and 2,650 feet (808 m) a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lost Mine Peak
Lost Mine Peak is a summit in Brewster County, Texas, United States. Description Lost Mine Peak is located in Big Bend National Park and the Chisos Mountains. It ranks as the third-highest peak in the park, mountain range, and county, but only the 20th-highest in Texas. The mountain is composed of volcanic rock which formed during the Oligocene period. Although modest in elevation, topographic relief is significant as the summit rises 2,150 feet (655 m) above Pine Canyon in , and 2,550 feet (777 m) above Juniper Canyon in . Based on the Köppen climate classification, Lost Mine Peak is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains into the Rio Grande watershed. The lower slopes of the peak are covered by juniper, oak, and piñon. The mountain's toponym has been officially adopted by the United States Board on Geographic Names. The peak's name comes from a legend of Spanis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Huffman (Texas)
Mount Huffman is a summit in Brewster County, Texas, United States. Description Mount Huffman is located in the Chisos Mountains and it ranks as the 16th-highest peak in Big Bend National Park. The mountain is composed of intrusive rock which formed during the Oligocene period. Robert G. Bohannon, 2011, U.S. Geological Survey. is modest as the summit rises 1,375 feet (419 m) above The Basin in . Based on the |
Vernon Bailey Peak
Vernon Bailey Peak is a summit in Brewster County, Texas, United States. Description Vernon Bailey Peak is located in the Chisos Mountains. It ranks as the 12th-highest peak in Big Bend National Park and 77th-highest in Texas. The mountain is composed of intrusive rock which formed during the Oligocene period. Topographic relief is significant as the summit rises 2,070 feet (631 m) above Oak Canyon in . Based on the Köppen climate classification, Vernon Bailey Peak is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains into Oak Creek which is part of the Rio Grande watershed. The lower slopes of the peak are covered by juniper, oak, and piñon. The mountain's toponym was officially adopted in 1945 by the United States Board on Geographic Names to remember Vernon Orlando Bailey (1864–1942), American naturalist who specialized in mammalogy and is best known for his biological surveys of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Texas
The geography of Texas is diverse and large. Occupying about 7% of the total water and land area of the U.S., it is the second largest state after Alaska, and is the southernmost part of the Great Plains, which end in the south against the folded Sierra Madre Oriental of Mexico. Texas is in the South Central United States of America, and is considered to form part of the U.S. South and also part of the U.S. Southwest. By residents, the state is generally divided into North Texas, East Texas, Central Texas, South Texas, West Texas and, sometimes, the Panhandle and Upper Gulf Coast, but according to the '' Texas Almanac'', Texas has four major physical regions: Gulf Coastal Plains, Interior Lowlands, Great Plains, and Basin and Range Province. This has been cited as the difference between human geography and physical geography, although the fact that Texas was granted the prerogative to divide into as many as five U.S. states may be a historical motive for Texans definin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountain Peaks Of Texas ...
This is a list of mountains in the state of Texas greater than 2,000 feet. References {{DEFAULTSORT:Mountain peaks of Texas Texas Mountain peaks A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
