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The Mountain and Basin Region. Most of the basins lie between 2,500 and 4,000 feet. The mountains, which include the Chisos and Davis ranges, generally rise 2,000 to 3,000 feet above the basins with some peaks (notably Guadalupe Peak and El Capitan) exceeding 8,000 feet.
Elevations in the Mountains and Basins region vary widely. For instance, this region contains the highest point in Texas—Guadalupe Peak, which stands 8,751 feet tall. On the other hand, some parts of this region reach an elevation of only about 2,500 feet.
Causes of Basin and Range Topography In basins and ranges, the hanging wall of the fault is what creates the range as they are the blocks of the Earth’s crust that are pushed upward during crustal extension. This upward movement occurs as the crust spreads apart.
The Mountains and Basins region extends from the Rio Grande east to the Pecos River. Because most of the region lies west of the Pecos River, it is sometimes called the Trans-Pecos area. Trans means “across” or “beyond.” Interpreting Maps This region is characterized by little rainfall and a dramatic desert landscape.
The Basin and Range Province is a vast physiographic region covering much of the inland Western United States and northwestern Mexico. It is defined by unique basin and range topography, characterized by abrupt changes in elevation, alternating between narrow faulted mountain chains and flat arid valleys or basins.
Basin and range topography is an alternating landscape of parallel mountain ranges and valleys. It is a result of crustal extension/stretching (extensional tectonics) of the lithosphere (crust and upper mantle) due to mantle upwelling, gravitational collapse, crustal thickening, or relaxation of confining stresses.
Basin and Range Province. The Basin and Range Province is a vast physiographic region covering much of the inland Western United States and northwestern Mexico. It is defined by unique basin and range topography, characterized by abrupt changes in elevation, alternating between narrow faulted mountain chains and flat arid valleys or basins.
It has many different landforms, rivers, and vegetation. The climate in the Mountain and Basin region is hot and dry, but some of the mountains get rainfall because of there elevation.
The average crustal thickness of the Basin and Range Province is approximately 30 – 35 km and is comparable to extended continental crust around the world. The crust in conjunction with the upper mantle comprises the lithosphere.