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As a result of this extension, the average crustal thickness of the Basin and Range region is 30 - 35 kilometers (19 - 22 miles), compared with a worldwide average of around 40 kilometers (25 miles).asin and Range topography is characterized by alternating valleys and mountainous areas, oriented in a north-south, linear direction. The entire region, including all of Nevada, southeastern California, and southeastern Oregon, consists of high mountain ranges (mostly running north-south) alternating with low valleys.
Both fold mountains and ocean trenches result from plates moving together. If both landforms occur in the same area, they are found in association with subduction on a destru â¦ ctive plate boundary (e.g: The Andes Mountains, Western coast of South America). The Andes formed from the Nazca plate subducting under the South American plate. The continental plate crumples and folds. The result is a fold mountain range. The Andes is formed. If fold mountains occur by themselves, they are in areas where collision is taking place on a collisional plate boundary (e.g: The Himalayas). The Himalayas formed from two continental plates which collided into one another- The Indo-Australian plate collided into the Eurasian plate. They crumple and fold. The result is a fold mountain range. The Himalayas is formed.