stepping, en echelon pattern similar to that of the Sierra Nevada frontal fault system. Jeffrey Unruh, James Humphrey, Andrew Barron; Transtensional model for the Sierra Nevada frontal fault system, eastern California. The most powerful earthquake recorded in the state was a 7.6 magnitude quake that occured near Winnemucca in 1915. The fault lies between the Calaveras Fault, the Greenville Fault, and the Concord… … Wikipedia, We are using cookies for the best presentation of our site. 3 Dec. 2015. Activity on this fault… It forms the eastern escarpment of the Sierra Nevada, extending roughly 600Â km (370Â mi) from just north of the Garlock Fault to the Cascade Range.. It parallels closely the marginal faults on the west4 and the Sierra Nevada fault on the east, and is, so far as the writer is aware, the largest fault within the southern Sierra Nevada that trends parallel to the marginal faults. Nature contributed its part, most spectacularly on March 26, 1872 when what may have been the greatest earthquake experienced by the contiguous United States in historic time shook the area.
Whitney, 14,495 ft. (4420 m). Geologists refer to these landforms as "fault-block mountains." (1996b) observed that a component of deformation along the eastern margin of the northern Sierra Nevada may step west-ward across the crest of the range. The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. "Geology of the Sierra Nevada Mountain Range." Web. The Sierra Nevada Fault is a normal (vertical motion) seismic fault along the eastern edge of the Sierra Nevada mountain block in California. It is… … Wikipedia, Chino Fault — The Chino Fault is a fault that extends along the eastern Chino Hills range region, from Corona in Riverside County to the Los Serranos, Chino Hills area of San Bernardino County in Southern California. As it began to cool, a large mass of igneous rock was created and is now visible as the granite domes of the Sierra Nevada Batholith.
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like. "Creation of the Sierra Nevada Batholith." the Sierra Nevada block (Fig. Strike-slip faults bordering the eastern Sierran microplate are subparallel to small circles about the Sierra Nevada–North American Euler pole. CS1 maint: multiple names: authors list (.  No large earthquake has been reported on this fault in recorded history. Crustal shortening occurs at the northern end of the Sierran microplate, where a component of northwest dextral shear steps westward in a left-restraining geometry across the Sierran crest to the Sacramento Valley. Around 200 million years ago, the ancient oceanic Farallon Plate began to subduct beneath the North American Plate. Seismotectonics of an evolving intracontinental plate boundary, southeastern California, Multiple constraints on divergent strike-slip deformation along the eastern margin of the Sierran microplate, SE California, Geodetic constraints on contemporary deformation in the northern Walker Lane: 2. N.p., n.d.
That's it. doi: https://doi.org/10.1130/0091-7613(2003)031<0327:TMFTSN>2.0.CO;2. By continuing to use our website, you are agreeing to our, https://doi.org/10.1130/0091-7613(2003)031<0327:TMFTSN>2.0.CO;2, Active transtensional boundary zone between the western Great Basin and Sierra Nevada block, western U.S. Cordillera, Seismogenic deformation between the Sierran microplate and Oregon Coast block, California, USA, Constraints on exhumation and extensional faulting in southwestern Nevada and eastern California, U.S.A., from zircon and apatite thermochronology, The Neogene–Recent Hatay Graben, South Central Turkey: graben formation in a setting of oblique extension (transtension) related to post-collisional tectonic escape, Neotectonics of the SW Marmara region, NW Anatolia, Turkey.
The largest earthquake in its vicinity was on the adjacent Owens Valley Fault in 1872, known as the Lone Pine Earthquake, which has been estimated as a 7.8 magnitude.
This movement, combined with the activity of the adjacent Owens Valley and Lone Pine faults, is responsible for the continuing rise of the Sierra Nevada Mountains. Highest peak, Mulhacén, 11,420 ft. (3480 m). i). Velocity and strain rate tensor analysis, Transtensional deformation of the western Caribbean–North America plate boundary zone, Seismotectonic framework of coastal central California, Neogene tectonic evolution of the Neuquén Andes western flank (37–39°S), Copyright © 2020 Geological Society of America. Geology of the Sierra Nevada Mountain Range. Normal faults of the Sierra Nevada frontal fault system strike ∼45° clockwise of the small circle trajectories and exhibit well-defined, left-stepping en echelon patterns, consistent with formation in dextral transcurrent regime. The Sierra Nevada Fault is an active seismic fault along the eastern edge of the Sierra Nevada mountain block in California.
You could also do it yourself at any point in time. Tusd.org. U.S. route 395 is a geologic master class disguised as a road. The kind of fault created by shearing is called a strike-slip fault. Kurbatova, Elena.
Kinematic inversions of earthquake focal mechanisms from the Walker Lane belt bordering the eastern Sierra Nevada indicate that seismogenic deformation primarily is characterized by horizontal shearing and oblique crustal thinning. âª California in 10 Million Years - Perspectives on Ocean Science, âª Plate Tectonics and California Geology, âª Geologic History of Southern California.mov. There are several contributors to the uplift of the Sierra Nevada Batholith. Would you like Wikipedia to always look as professional and up-to-date?