Basin and Range

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Great Basin Ranges
Highest point
PeakWhite Mountain Peak
Elevation14,252 ft (4,344 m)
CountryUnited States
Parent rangeNorth American Cordillera
Coordinates: 33°N 112°W / 33°N 112°W / 33; -112
Basin and Range
physiographic region
One of various geographical definitions of the Province
Countries United States, Mexico
Location western United States
 - coordinates 33°N 112°W / 33°N 112°W / 33; -112
Area 170,000 sq mi (440,298 km²)
Biome North American Desert ecoregion

The Basin and Range Province is a vast geographic region in the west United States and northwest Mexico. Its topography has abrupt changes in height. It has narrow faulted mountain chains and flat arid valleys or basins. There are many ecoregions, but the lower part is mostly desert.

The physical geography (physiography) of the province was caused by extension and thinning of the lithosphere, which is composed of crust and upper mantle. What caused this thinning is still being investigated. The thinning began around 17 million years ago (mya) in early Miocene time.

The highest point fully within the Province is White Mountain Peak in California, while the lowest point is Badwater Basin in Death Valley. Other high points are at the boundary of the Basin and Range province.

The numerous ranges within the Province in the United States are collectively referred to as the Great Basin Ranges, although many are not actually in the Great Basin. The Basin and Range province should not be confused with the Great Basin, which is a sub-section of the greater Basin and Range region. The Great Basin is defined by its watershed (internal drainage).

Clarence Dutton compared the many narrow mountain ranges of the Basin and Range to an "army of caterpillars marching toward Mexico", which is a helpful way to visualize the overall appearance of the region.[1]

Volcanics[change | change source]

Before the Eocene epoch (55.8 ±0.2 to 33.9 ±0.1 mya) the Farallon and North American plates were converging. During the Eocene the many volcanos in the Basin and Range Province flared up. The Farallon plate continued to be underthrust until about 19 mya. By then it was consumed and volcanic activity ceased.[2][3][4][5]

References[change | change source]

  1. Reynolds D. & Christensen J. 2001. Nevada. Portland, Or: Graphic Arts Center.
  2. McKee, E. H. (1971). "Tertiary igneous chronology of the Great Basin of Western United States–-implications for tectonic models". Geological Society of America Bulletin. 82 (12): 3497–3502. Bibcode:1971GSAB...82.3497M. doi:10.1130/0016-7606(1971)82[3497:ticotg];2. Retrieved 2010-04-09.
  3. "Northwest origins, an introduction to the geologic history of Washington State, Catherine L. Townsend and John T. Figge". The Burke Museum of Natural History and Culture, University of Washington. Retrieved 2010-04-10.
  4. "Oregon: a geologic history". Oregon Department of Geology and Mineral Industries. Archived from the original on 2010-01-28. Retrieved 2010-03-26.
  5. "Digital geology of Idaho, Laura DeGrey and Paul Link". Idaho State University. Archived from the original on 2018-07-21. Retrieved 2010-04-10.