walker lane fault

Walker Lane rift system - currently accommodates 20-25% of the plate motion between the Pacific and the North American plates!! For context, I first review available observations describing strain accumulation and the history of slip on faults within the Eastern California Shear Zone and Walker Lane. The Walker Lane has historically not received the detail of attention given to the San Andreas fault system to the west. The pent-up stress that currently appears to be migrating from the San Andreas to the Walker Lane might instead be taken up by the Wasatch Fault, which passes through Salt Lake City.
The quake’s epicenter was 2.3 miles deep and about 14 … The Walker Lane is composed of discontinuous sets of right-slip faults that are located to the east and strike approximately parallel to the San Andreas fault system. along the Walker Lane, and reasons for similarities and differences in styles of faulting between the Walker Lane and San Andreas fault systems. The results of the field study Next came the present day fault system known as the Walker Lane Fault system. Walker Lane rift system - currently accommodates 20-25% of the plate motion between the Pacific and the North American plates!! Most of this fault lies beneath the alluvial fans of the valleys and under Walker Lake. The Walker Lane is a geologic trough roughly aligned with the California/Nevada border southward to where Death Valley intersects the Garlock Fault, a major left lateral, or … We apply recently acquired 0.5-1 m/pixel lidar data and terrestrial cosmogenic nuclide (TCN) surface exposure ages to characterize the geometry, Quaternary expression, and slip rates of active faults in these three valleys. It is considered an integral part of the Walker Lane..

In comparison, the San Andreas Fault contains one singular, mature, and well-mapped strand.

No obvious connection of the northern end of the zone with another plate boundary exits. Between Wadsworth and Pyramid Lake, the Truckee River follows the path of an important zone of faults called the Walker Lane, which began to develop approximately 13 million years ago. Collection Overview: PI: Steven G. Wesnousky, University of Nevada, Reno The requested survey area consisted of 1-km wide swaths centered along 335 km of fault centerlines. However, the Eastern California Shear Zone, sometimes called Walker Lane, does not act properly. BARSTOW (CBSLA) — A 4.6-magnitude earthquake jolted Southern California just after 7 p.m. Friday night. The fault zone extends to the southeast from Pyramid Lake roughly parallel to the course of the Truckee River between the Truckee Range to the northeast and the Pah Rah Range to the southwest. We have been using geologic, geomorphic, and paleoseismic studies to better understand how the fault system serves to accommodate plate motion. Provides a clear record of rift initiation… !!

The Walker Lane may represent an incipient major transform fault zone which could replace the San Andreas as the plate boundary in the future. There were a total of 44 fault segments for 12 fault lines, totaling a nominal 335 km 2 of map area. The Walker Lane may represent an incipient major transform fault zone which could replace the San Andreas as the plate boundary in the future. The first fault along this mountain range was called the Pine Nut Fault. The Walker Lane fault pattern within the area of Fig. The idea of migration of plate boundary migration of strain release to newer (relatively speaking) faults is interesting and I see similar possibilities/pattern in the NE corner of the South Island of New Zealand. The Walker Lane takes up 15 to 25 percent of the boundary motion between the Pacific Plate and the North American Plate, the other 75 percent being taken up by the San Andreas Fault system to the west. and a time-transgressive view of!! The faults are spread throughout an area of 15,600 km 2 of central western Nevada east of Lake Tahoe. 5 may be analogous to an earlier stage in the structural development of the San Andreas when the system was transtensional and before sufficient slip accumulated to yield the now throughgoing San Andreas fault.

This was the Walker Lane. The Walker Lane fault pattern within the area of Fig.
Provides a clear record of rift initiation… !! Modern Tectonic Context ! and a time-transgressive view of!! Antelope, Mason and Smith Valleys are half-grabens within the Northern Walker Lane, east and south of Carson City and Reno, Nevada.

5 may be analogous to an earlier stage in the structural development of the San Andreas when the system was transtensional and before sufficient slip accumulated to yield the now throughgoing San Andreas fault. processes involved in strain localization.!!!! The earthquake occurred in the Walker Lane seismic belt that extends along the eastern side of the Sierra Nevada and accommodates about 10–25% of the Pacific/North American plate boundary motion. processes involved in strain localization.!!!!


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