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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.
The rise of hot asthenosphere below New Mexico reversed the compression of the crust and put it into tension, resulting in the opening of the Rio Grande rift, [51] [52] beginning about 30 Mya, [53] and the development of Basin and Range geology across the southern part of the state.
The Albuquerque Basin (or Middle Rio Grande Basin [1]) is a structural basin and ecoregion within the Rio Grande rift in central New Mexico. It contains the city of Albuquerque . Geologically, the Albuquerque Basin is a half-graben that slopes down towards the east to terminate on the Sandia and Manzano mountains. [ 2 ]
New Mexico's other major center of population is in south-central area around Las Cruces, its second-largest city and the largest city in the southern region of the state. The Las Cruces metropolitan area includes roughly 214,000 residents, but with neighboring El Paso, Texas forms a combined statistical area numbering over 1 million.
Map of the Tularosa Basin (light blue) and its landmarks, in southern New Mexico and West Texas, U.S. White gypsum sand and Yucca (Yucca elata) plants, in Tularosa Basin at White Sands National Park. The Tularosa Basin is a graben basin in the Basin and Range Province and within the Chihuahuan Desert , east of the Rio Grande in southern New ...
The Ouachita Orogeny was the collision of South America with the current-day Gulf-region, and resulted in the Ancestral Rockies - a northwest trending intercontinental mountain belt mainly through Texas, New Mexico, and Colorado. The Ancestral Rockies gave way to the Uncompahgre Mountain Range, which bound the San Juan Basin on the northeast ...
The large Basin and Range Province is a basin and range topography resulting from crustal extension (extensional tectonics). It is located in all or parts of Oregon, Idaho, Nevada, California, Utah, New Mexico, Arizona in the Western United States; and Sonora, Chihuahua, Sinaloa, and other states southwards to the Trans-Mexican Volcanic Belt in ...
"Emory cauldron, Black Range, New Mexico, source of the Kneeling Nun Tuff". Field Conf Guide, New Mexico Geological Society. 26: 283– 292. Erb, E.E. Jr. (1979). Petrologic and structural evolution of ash-flow tuff cauldrons and noncauldron related volcanic rocks in the Animas and southern Peloncillo Mountains, Hidalgo County, New Mexico ...
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