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The Sandia Mountains (Southern Tiwa: Posu gai hoo-oo, Keres: Tsepe, Navajo: Dził Nááyisí; Tewa: O:ku:p’į, Northern Tiwa: Kep’íanenemą; Towa: Kiutawe, Zuni: Chibiya Yalanne) [1] are a mountain range located in Bernalillo and Sandoval counties, immediately to the east of the city of Albuquerque in New Mexico in the southwestern United States.
[2] [3] It is found in the Sandia, Jemez, [4] Sangre de Cristo, [3] and Manzano Mountains [1] as well as the Las Vegas Basin. [ 3 ] The formation rests on Precambrian basement rock in the Sandia Mountains, but is underlain by Osha Canyon Formation in the southern Jemez Mountains or by formations of the Arroyo Penasco Group in the Sangre de ...
Sandia Mountain Wilderness, part of Cibola National Forest, is located east of Albuquerque, New Mexico, and comprises much of Sandia Mountains. It became part of the National Wilderness Preservation System in 1978 by an act of the United States Congress and has a total of 37,877 acres (15,328 ha).
The pluton lies in the southern Sandia Mountains, with Sandia granite to the northwest and Seven Springs shear zone to the south. The pluton may include three compositionally distinct phases: a fine-grained, peraluminous, two-mica leucogranite with a radiometric age of 1632±45 Ma, a medium-grained equigranular monzogranite with a radiometric age of 1659±13 Ma, and a generally coarse-grained ...
Shaded relief map of the Llano Estacado. Texas contains a wide variety of geologic settings. The state's stratigraphy has been largely influenced by marine transgressive-regressive cycles during the Phanerozoic, with a lesser but still significant contribution from late Cenozoic tectonic activity, as well as the remnants of a Paleozoic mountain range.
Sandia Crest, also known locally as Sandia Peak or simply as the Crest, [2] is a mountain ridge that, at 10,679 feet (3,255 m), is the highpoint of the Sandia–Manzano Mountains, and is located in the Sandia Mountains of Bernalillo County, New Mexico, United States. Instead of a true summit or topographic peak, this range climbs to a long ...
Flanking mountains are generally taller along the east side of the rift (although some of this relief may be Laramide in origin). [1] The thickness of the crust increases to the north beneath the rift, where it may be as much as 5 kilometres (3.1 mi) thicker than it is in the south. The crustal thickness underneath the rift is on average 30 ...
The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11. pp. 95– 136. ISBN 9781585460106. Lindsey, D.A. (1995). "Geologic map of the McCarty Park quadrangle, Costilla and Huerfano Counties, Colorado". U.S. Geological Survey Miscellaneous Field Studies. Map MF-2282.