Basin and Range faults
The Basin and Range province in the western US is a result of extensional faulting. This type of faulting occurs when the Earth's crust is being stretched, causing blocks of the crust to drop down in a series of mountain ranges and valleys.
Major cities in the Basin and Range Province include Las Vegas (Nevada), Reno (Nevada), Salt Lake City (Utah), and Phoenix (Arizona).
because it is a geological term for topography
The answer is a fault-block mountain
basin and range province
Some of the prominent mountains in the Basin and Range Province include the Sierra Nevada, Snake Range, Ruby Mountains, Wasatch Range, and Granite Mountains. These mountains are characterized by parallel ridges and valleys, which are a result of stretching and pulling apart of the Earth's crust.
The mountains of the Basin and Range province formed from extensional tectonic forces that caused the Earth's crust to stretch and thin out, resulting in horst and graben structures. This extensional tectonics created alternating blocks of uplifted mountains and down-dropped valleys, giving the region its characteristic basin-and-range topography.
The Basin and Range province is a type of mountain range formed by extensional forces, resulting in numerous normal faults that create alternating basin and range topography. This region is characterized by elongated valleys and mountain ridges running parallel to each other.
The Basin and Range Province of North America ,,
The Basin and Range Province is an example of a rift zone.
Basin and Range Province is a type of mountain range characterized by linear mountain ranges separated by elongated valleys or basins. They are formed by extensional tectonics where the Earth's crust stretches and thins, creating a series of parallel faults.
Thomas Brennan Nolan has written: 'The basin and range province in Utah, Nevada, and California'