Extension in the ESVS probably began in the middle Miocene in response to initial westward movement of the SN-GVm relative to the Colorado Plateau. Numerous geologic and geodetic studies have produced estimates of late Pleistocene to Holocene rates of horizontal extension and right-lateral movement across the ESVS, with particular emphasis on the Sierra Nevada Frontal Fault and the Owens Valley Fault south of latitude 37° N, e.g., [,In the south, dextral strike-slip displacement is presently occuring along the Owens Valley Fault, which cuts obliquely across the axis of the valley, e.g., [,Isostatic gravity data are especially useful for interpreting vertical fault displacements, basin shapes, and sediment thicknesses, e.g., [,A striking feature of the ESVS is the discontinuous nature of the deep basins that extend northward from Indian Wells Valley through Owens Valley to Chalfant and Long valleys (,In Owens and Chalfant valleys, the eastern margin of this deep basin system is sharply marked by the West Inyo and White Mountains faults except at an apparent divide between the Owens and Bishop basins near latitude 37° N, where Cenozoic deposits are very thin (,The western margin of the deep basin system coincides with the Owens Valley Fault east of the Alabama Hills, whereas to the south in Indian Wells Valley, the western boundary lies close to the Sierran front.


Please note that many of the page functionalities won't work as expected without javascript enabled.You can use * to search for partial matches.Department of Geology, San Jose State University, 1 Washington Square, San Jose, CA 95192, USA,Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA.Author to whom correspondence should be addressed.Received: 1 February 2013 / Revised: 30 March 2013 / Accepted: 30 March 2013 / Published: 22 April 2013,The tectonically active East Sierra Valley System (ESVS), which comprises the westernmost part of the Walker Lane-Eastern California Shear Zone, marks the boundary between the highly extended Basin and Range Province and the largely coherent Sierra Nevada-Great Valley microplate (SN-GVm), which is moving relatively NW. more than a few dozen miles away from the Pacific shores, except for their
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Extension in the ESVS probably began in the middle Miocene in response to initial westward movement of the SN-GVm relative to the Colorado Plateau. Numerous geologic and geodetic studies have produced estimates of late Pleistocene to Holocene rates of horizontal extension and right-lateral movement across the ESVS, with particular emphasis on the Sierra Nevada Frontal Fault and the Owens Valley Fault south of latitude 37° N, e.g., [,In the south, dextral strike-slip displacement is presently occuring along the Owens Valley Fault, which cuts obliquely across the axis of the valley, e.g., [,Isostatic gravity data are especially useful for interpreting vertical fault displacements, basin shapes, and sediment thicknesses, e.g., [,A striking feature of the ESVS is the discontinuous nature of the deep basins that extend northward from Indian Wells Valley through Owens Valley to Chalfant and Long valleys (,In Owens and Chalfant valleys, the eastern margin of this deep basin system is sharply marked by the West Inyo and White Mountains faults except at an apparent divide between the Owens and Bishop basins near latitude 37° N, where Cenozoic deposits are very thin (,The western margin of the deep basin system coincides with the Owens Valley Fault east of the Alabama Hills, whereas to the south in Indian Wells Valley, the western boundary lies close to the Sierran front.


Please note that many of the page functionalities won't work as expected without javascript enabled.You can use * to search for partial matches.Department of Geology, San Jose State University, 1 Washington Square, San Jose, CA 95192, USA,Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA.Author to whom correspondence should be addressed.Received: 1 February 2013 / Revised: 30 March 2013 / Accepted: 30 March 2013 / Published: 22 April 2013,The tectonically active East Sierra Valley System (ESVS), which comprises the westernmost part of the Walker Lane-Eastern California Shear Zone, marks the boundary between the highly extended Basin and Range Province and the largely coherent Sierra Nevada-Great Valley microplate (SN-GVm), which is moving relatively NW. more than a few dozen miles away from the Pacific shores, except for their
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Extension in the ESVS probably began in the middle Miocene in response to initial westward movement of the SN-GVm relative to the Colorado Plateau. Numerous geologic and geodetic studies have produced estimates of late Pleistocene to Holocene rates of horizontal extension and right-lateral movement across the ESVS, with particular emphasis on the Sierra Nevada Frontal Fault and the Owens Valley Fault south of latitude 37° N, e.g., [,In the south, dextral strike-slip displacement is presently occuring along the Owens Valley Fault, which cuts obliquely across the axis of the valley, e.g., [,Isostatic gravity data are especially useful for interpreting vertical fault displacements, basin shapes, and sediment thicknesses, e.g., [,A striking feature of the ESVS is the discontinuous nature of the deep basins that extend northward from Indian Wells Valley through Owens Valley to Chalfant and Long valleys (,In Owens and Chalfant valleys, the eastern margin of this deep basin system is sharply marked by the West Inyo and White Mountains faults except at an apparent divide between the Owens and Bishop basins near latitude 37° N, where Cenozoic deposits are very thin (,The western margin of the deep basin system coincides with the Owens Valley Fault east of the Alabama Hills, whereas to the south in Indian Wells Valley, the western boundary lies close to the Sierran front.


Please note that many of the page functionalities won't work as expected without javascript enabled.You can use * to search for partial matches.Department of Geology, San Jose State University, 1 Washington Square, San Jose, CA 95192, USA,Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA.Author to whom correspondence should be addressed.Received: 1 February 2013 / Revised: 30 March 2013 / Accepted: 30 March 2013 / Published: 22 April 2013,The tectonically active East Sierra Valley System (ESVS), which comprises the westernmost part of the Walker Lane-Eastern California Shear Zone, marks the boundary between the highly extended Basin and Range Province and the largely coherent Sierra Nevada-Great Valley microplate (SN-GVm), which is moving relatively NW. more than a few dozen miles away from the Pacific shores, except for their
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owens valley fault system

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Slemmons (cited in Hill, 1972 #1207) referred to the fault zone as both the mid-Owens Valley fault zone and mid-Valley fault zone. The presence of a thin cover of Pliocene to Pleistocene sedimentary and volcanic deposits in this block suggests a period of modest subsidence approximately coeval with downfaulting of the surrounding basins. The study also involved geomorphic analysis of stream deflections near site 51-7.Sites 51-6 and 51-7. and – as in 1872 –.Another factor is that the Owens Valley is the westernmost extent of a geologic Except for a few other mining settlements, the Owens Valley was only
Total vertical displacement across the Owens Valley fault zone is 2.5 km, based on gravity data (Hollett and others, 1991 #5617). Finally, we briefly discuss the possibility that the ESVS might be evolving into a rift system like the Gulf of California [,In addition to the types of recent investigations noted above, much research also has been concerned with the deep lithospheric processes inferred to have driven the structural and tectonic evolution of the Sierra Nevada and ESVS region, e.g., [,The structural and geomorphic features represented in the modern valley system are largely due to faults developed as a consequence of recent uplift and lateral displacement of the SN-GVm. This along the eastern flank of the Sierra Nevada. The Garlock fault extends from the San Andreas Fault in the west to Death Valley in the east, and hasn’t had a major earthquake in about 500 years. In 1997, Inyo County, Los Angeles, the Owens Valley Committee, the Sierra Club, and other concerned parties signed a,Los Angeles Department of Water and Power,"Los Angeles Mayor Seeks To Freeze Valley Growth","New dust-busting method ends L.A.'s longtime feud with Owens Valley",The Owens Valley Committee: The Owens Valley,Cenozoic/Mesozoic Volcanism of the Eastern Sierra Nevada,Groundwater Quality in the Owens Valley, California,Lower Owens River Project - 60-mile (97 km) restoration of the lower owens river,Eval.

Extension in the ESVS probably began in the middle Miocene in response to initial westward movement of the SN-GVm relative to the Colorado Plateau. Numerous geologic and geodetic studies have produced estimates of late Pleistocene to Holocene rates of horizontal extension and right-lateral movement across the ESVS, with particular emphasis on the Sierra Nevada Frontal Fault and the Owens Valley Fault south of latitude 37° N, e.g., [,In the south, dextral strike-slip displacement is presently occuring along the Owens Valley Fault, which cuts obliquely across the axis of the valley, e.g., [,Isostatic gravity data are especially useful for interpreting vertical fault displacements, basin shapes, and sediment thicknesses, e.g., [,A striking feature of the ESVS is the discontinuous nature of the deep basins that extend northward from Indian Wells Valley through Owens Valley to Chalfant and Long valleys (,In Owens and Chalfant valleys, the eastern margin of this deep basin system is sharply marked by the West Inyo and White Mountains faults except at an apparent divide between the Owens and Bishop basins near latitude 37° N, where Cenozoic deposits are very thin (,The western margin of the deep basin system coincides with the Owens Valley Fault east of the Alabama Hills, whereas to the south in Indian Wells Valley, the western boundary lies close to the Sierran front.


Please note that many of the page functionalities won't work as expected without javascript enabled.You can use * to search for partial matches.Department of Geology, San Jose State University, 1 Washington Square, San Jose, CA 95192, USA,Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA.Author to whom correspondence should be addressed.Received: 1 February 2013 / Revised: 30 March 2013 / Accepted: 30 March 2013 / Published: 22 April 2013,The tectonically active East Sierra Valley System (ESVS), which comprises the westernmost part of the Walker Lane-Eastern California Shear Zone, marks the boundary between the highly extended Basin and Range Province and the largely coherent Sierra Nevada-Great Valley microplate (SN-GVm), which is moving relatively NW. more than a few dozen miles away from the Pacific shores, except for their

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