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The Spring Mountains divide the Pahrump Valley and Amargosa River basins from the Las Vegas Valley watershed, which drains into the Colorado River watershed, by way of Las Vegas Wash into Lake Mead, thus the mountains define part of the boundary of the Great Basin.
Stuart Range from Cashmere Peak. There are at least 64 named mountain ranges in the U.S. state of Washington.Names, elevations and coordinates from the U.S. Geological Survey, Geographic Names Information System and trail guides published by The Mountaineers.
The southern portion of the Las Vegas Range has the linear ridgelines ending at the massif at the south, defining the northern Las Vegas Valley metropolitan area, including the city of North Las Vegas. Region. The range is on the southeast of the Sheep Range, which itself is a massive north–south range. Both ranges are Basin and Range block ...
The McCullough Range is surrounded by three valleys. First, the Las Vegas Valley lies to the north; next, the north region of the Ivanpah Valley, with two major dry lakes borders the west; and to the east lies the endorheic basin of the Eldorado Valley. The range specifically borders one mountain range at the south, being connected to the ...
Alvin R. McLane, Silent Cordilleras: The Mountain Ranges of Nevada. (Reno: Camp Nevada Monograph #4, 1978) (Reno: Camp Nevada Monograph #4, 1978) Geographic Names Information System (GNIS) , USGS
The day before its 1980 eruption, Mount St. Helens was the fifth highest major summit of Washington. Today, Mount St. Helens is the 35th highest major summit of the state. This article comprises three sortable tables of major mountain peaks [1] of the U.S. State of Washington. The summit of a mountain or hill may be measured in three principal ...
The Enchantments is a region within the Alpine Lakes Wilderness area of Washington state's Cascade Mountain Range. [2] At an elevation of 4,500 feet (1,372 m), it is home to over 700 alpine lakes and ponds surrounded by the vast peaks of Cashmere Crags, which rate among the best rock-climbing sites in the western United States. [3]
Like the Cascade Range, the Sierra Nevada Range formed from a chain of volcanoes along a subduction zone. However unlike the Cascade volcanoes, those that formed the Sierra Nevada Range are mostly extinct and buried deep within the earth forming a bed of solidified lava that is responsible for the gray granitic rocks of the Sierra.