|Walker Lane Deformation Belt|
|Parts||Faults: Honey Lake, Pyramid Lake,
Benton Springs, Furnace Creek,
Death Valley, Petrified Springs
|Length||500 mi (805 km), NNW-SSE|
|Biome||Central Basin and Range ecoregion|
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 sinistral, strike-slip fault. The north-northwest end of the Walker Lane is between Pyramid Lake in Nevada and California's Lassen Peak where the Honey Lake Fault Zone meets the transverse tectonic zone forming the southern boundary of the Modoc Plateau and Columbia Plateau provinces. 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. 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 Walker Lane deformation belt accommodates nearly 12 mm/yr of dextral shear between the Sierra Nevada-Great Valley Block and North America. The belt is characterized by the northwest-striking trans-current faults and co-evolutionary dip-slip faults formed as result of a spatially segregated displacement field.
Eastern California shear zone
The eastern California shear zone is the portion of the Walker Lane that extends south from Owens Valley, and continues across and south of the Garlock Fault, across the Mojave Desert to the San Andreas Fault.
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- Bernard Guest et al. (2007). "Stateline fault system: A new component of the Miocene-Quaternary Eastern California shear zone". Geological Society of America Bulletin (Division of Geological and Planetary Sciences, California Institute of Technology) 119 (11–12): 1337. doi:10.1130/0016-7606(2007)119[1337:SFSANC]2.0.CO;2.
- Active Faulting in the Walker Lane
- Faulds, James E.; Christopher D. Henry, Nicholas H. Hinz (2005-6). "Kinematics of the northern Walker Lane: An incipient transform fault along the Pacific–North American plate boundary". Geology. The Geological Society of America, Inc. Retrieved 2009-12-19.
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- Unruh, Jeffrey; James Humphrey and Andrew Barron (April 2003). "Transtensional model for the Sierra Nevada frontal fault system, eastern California". Geology 31 (4): 327–330. doi:10.1130/0091-7613(2003)031<0327:TMFTSN>2.0.CO;2.
- Dokka, R.K., and Travis, C.J., 1990, Role of the eastern California shear zone in accommodating Pacific-North American plate motion: Geophysical Research Letters, v. 17, p. 1323-1326.
- Frankel, K. L.; Glazner, A. F.; Kirby, E.; Monastero, F. C.; Strane, M. D.; Oskin, M. E.; Unruh, J. R.; Walker, J. D.; Anandakrishnan, S.; Bartley, J. M.; Coleman, D. S.; Dolan, J. F.; Finkel, R. C.; Greene, D.; Kylander-Clark, A.; Morrero, S.; Owen, L.A.; Phillips, F. (2008). "Active tectonics of the eastern California shear zone". Field Guide to Plutons, Volcanoes, Faults, Reefs, Dinosaurs, and Possible Glaciation in Selected Areas of Arizona, California, and Nevada. Geological Society of America. pp. 43–82. ISBN 978-0-8137-0011-3.