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![Coso Range (after Lewis et al. [2007]). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001). The triangle with vertices at three of the GPS stations is cell 34 of Lewis et al. (2007), which includes Wild Horse Mesa. The letter X labels the locations in Petroglyph Canyon and Sheep Canyon where the fault-slickenline data were gathered. Stars show locations from which the paleomagnetic orientations were determined; curved arrows around the stars show the paleomagnetic rotation of lavas in the fault stepover relative to the same lavas outside the stepover, which averages 12.0°±2.6°. Solid diamonds and open squares show the epicenters of earthquakes at greater than and less than 5 km depth, respectively; the focal mechanisms from these events were inverted for a solution of the local deformation. (b) Stereogram showing the orientations of the axis of maximum rates of lengthening () and shortening () inferred from the inversion of fault-slickenline data and from the inversion of GPS velocity data from the triangular cell shown in part (a). The boundary of the shaded areas is the locus of zero instantaneous extension. Lower hemisphere equal area projection. (c) Values of the deformation rate parameter D and the relative vorticity parameter W inferred from two independent methods: first, from the inversion of fault-slickenline data; and second, from the inversion of GPS velocities for the vertices of the triangular cell in part (a), which defines the macrovorticity and the maximum macroshear rate, and from the paleomagnetically determined block-rotation rates, which define the microvorticity.]()
![Coso Range (after Lewis et al. [2007]). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001). The triangle with vertices at three of the GPS stations is cell 34 of Lewis et al. (2007), which includes Wild Horse Mesa. The letter X labels the locations in Petroglyph Canyon and Sheep Canyon where the fault-slickenline data were gathered. Stars show locations from which the paleomagnetic orientations were determined; curved arrows around the stars show the paleomagnetic rotation of lavas in the fault stepover relative to the same lavas outside the stepover, which averages 12.0°±2.6°. Solid diamonds and open squares show the epicenters of earthquakes at greater than and less than 5 km depth, respectively; the focal mechanisms from these events were inverted for a solution of the local deformation. (b) Stereogram showing the orientations of the axis of maximum rates of lengthening () and shortening () inferred from the inversion of fault-slickenline data and from the inversion of GPS velocity data from the triangular cell shown in part (a). The boundary of the shaded areas is the locus of zero instantaneous extension. Lower hemisphere equal area projection. (c) Values of the deformation rate parameter D and the relative vorticity parameter W inferred from two independent methods: first, from the inversion of fault-slickenline data; and second, from the inversion of GPS velocities for the vertices of the triangular cell in part (a), which defines the macrovorticity and the maximum macroshear rate, and from the paleomagnetically determined block-rotation rates, which define the microvorticity.]()
![Coso Range (after Lewis et al. [2007]). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001). The triangle with vertices at three of the GPS stations is cell 34 of Lewis et al. (2007), which includes Wild Horse Mesa. The letter X labels the locations in Petroglyph Canyon and Sheep Canyon where the fault-slickenline data were gathered. Stars show locations from which the paleomagnetic orientations were determined; curved arrows around the stars show the paleomagnetic rotation of lavas in the fault stepover relative to the same lavas outside the stepover, which averages 12.0°±2.6°. Solid diamonds and open squares show the epicenters of earthquakes at greater than and less than 5 km depth, respectively; the focal mechanisms from these events were inverted for a solution of the local deformation. (b) Stereogram showing the orientations of the axis of maximum rates of lengthening () and shortening () inferred from the inversion of fault-slickenline data and from the inversion of GPS velocity data from the triangular cell shown in part (a). The boundary of the shaded areas is the locus of zero instantaneous extension. Lower hemisphere equal area projection. (c) Values of the deformation rate parameter D and the relative vorticity parameter W inferred from two independent methods: first, from the inversion of fault-slickenline data; and second, from the inversion of GPS velocities for the vertices of the triangular cell in part (a), which defines the macrovorticity and the maximum macroshear rate, and from the paleomagnetically determined block-rotation rates, which define the microvorticity.]()
![Figure 2. Location map and major geographic and geologic features discussed in this paper. Coso Range, Little Lake fault zone (LLFZ), Airport Lake fault zone (ALFZ), Coso Wash fault (CWF), White Hills anticline (WHA), Wild Horse Mesa fault (WHMF), Lower Centennial Flat (LCF), Haiwee Spring (HS). Faults are designated as heavy black lines, dashed where approximate. Arrows indicate sense of offset on faults, and tick mark is on downthrown block of normal faults.]()
![Figure 5. Cross section through the Dooley and McClay (1997) 30° translational stepover model. Model depth to basement from the original surface is 8 km. Alternating dark and light bands represent prekinematic layers. Stippled layers are postkinematic layers that are added at various stages of model advancement. The “A” and “T” in the circles represent blocks moving away from and toward the viewer, respectively. Projected location of cross section A–A′ is shown on Figure 1. LLF—Little Lake fault, ALF-CWF—Airport Lake fault–Coso Wash fault, WHMF—Wild Horse Mesa fault. Little Lake fault designation is queried on this cross section because it is not clear whether it is actually that fault or the furthermost fault on the left of the figure.]()
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Book Chapter
Multiple constraints on divergent strike-slip deformation along the eastern margin of the Sierran microplate, SE California Available to Purchase
... We have examined the deformation associated with a right-releasing stepover along the dextral Walker Lane belt where it traverses Wild Horse Mesa in eastern California. We use a micropolar inversion of both seismic focal mechanism and fault-slickenline data and compare the results...
Image
![Coso Range (after Lewis et al. [2007]). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001). The triangle with vertices at three of the GPS stations is cell 34 of Lewis et al. (2007), which includes Wild Horse Mesa. The letter X labels the locations in Petroglyph Canyon and Sheep Canyon where the fault-slickenline data were gathered. Stars show locations from which the paleomagnetic orientations were determined; curved arrows around the stars show the paleomagnetic rotation of lavas in the fault stepover relative to the same lavas outside the stepover, which averages 12.0°±2.6°. Solid diamonds and open squares show the epicenters of earthquakes at greater than and less than 5 km depth, respectively; the focal mechanisms from these events were inverted for a solution of the local deformation. (b) Stereogram showing the orientations of the axis of maximum rates of lengthening () and shortening () inferred from the inversion of fault-slickenline data and from the inversion of GPS velocity data from the triangular cell shown in part (a). The boundary of the shaded areas is the locus of zero instantaneous extension. Lower hemisphere equal area projection. (c) Values of the deformation rate parameter D and the relative vorticity parameter W inferred from two independent methods: first, from the inversion of fault-slickenline data; and second, from the inversion of GPS velocities for the vertices of the triangular cell in part (a), which defines the macrovorticity and the maximum macroshear rate, and from the paleomagnetically determined block-rotation rates, which define the microvorticity.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/bssa/99/2B/10.1785_0120080084/2/s_1103eq143.jpeg?Expires=2147483647&Signature=gMtmKSJHvlIFISe7ydigTZUItU1xxcn31w04Fy9~X405cozLcJEIDbpyUcG7YNj7i8v16NSykHAOP2KOeZI5xEVrAW6ddxhVajl5-Fbm~RnrMwjxnPdBhFSs3sZcg2dPIfNzV01deTfwLY1elG2t5hMOPGKmwLc-nJMin1w-7~PjOI2ZCaG3PMt2OVD4B6ki7viNLNK9H-SEr7hiNk3QGL1zdCe-yPGKDbDU4PWT8zXq0EYt-vIztXLR38e9qjkuTGpyMZMMBljKDTe7eWQMbOU8XvZfdY8Je6CDq9H7w2RZytHkxSXMJHIxj5mdT~g0HQvRLbj5UzOxeh-qs068Mg__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of... Available to Purchase
in An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure
> Bulletin of the Seismological Society of America
Published: 01 May 2009
Figure 7. Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001) . The triangle with vertices at three of the GPS
Image
![Coso Range (after Lewis et al. [2007]). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001). The triangle with vertices at three of the GPS stations is cell 34 of Lewis et al. (2007), which includes Wild Horse Mesa. The letter X labels the locations in Petroglyph Canyon and Sheep Canyon where the fault-slickenline data were gathered. Stars show locations from which the paleomagnetic orientations were determined; curved arrows around the stars show the paleomagnetic rotation of lavas in the fault stepover relative to the same lavas outside the stepover, which averages 12.0°±2.6°. Solid diamonds and open squares show the epicenters of earthquakes at greater than and less than 5 km depth, respectively; the focal mechanisms from these events were inverted for a solution of the local deformation. (b) Stereogram showing the orientations of the axis of maximum rates of lengthening () and shortening () inferred from the inversion of fault-slickenline data and from the inversion of GPS velocity data from the triangular cell shown in part (a). The boundary of the shaded areas is the locus of zero instantaneous extension. Lower hemisphere equal area projection. (c) Values of the deformation rate parameter D and the relative vorticity parameter W inferred from two independent methods: first, from the inversion of fault-slickenline data; and second, from the inversion of GPS velocities for the vertices of the triangular cell in part (a), which defines the macrovorticity and the maximum macroshear rate, and from the paleomagnetically determined block-rotation rates, which define the microvorticity.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/bssa/99/2B/10.1785_0120080084/2/s_1103eq142.jpeg?Expires=2147483647&Signature=Opn4Ec35W8VL1aamvdObUd7b3SB6h1pLfy~aBqp3-CEDO9tonb3HHsvESPHjBfEw08YJ1PubWKpOKvQHZWA0Vb5kXPe64JMuDktB8cqtN3UFjQKheT1kS~~cNkitXdClJ2dyVxeS0DSLcZVzmswDqmuHmIkRF70I0fmA86ZVVupj7JUFIoIMTUgY8PU3bK5oKIpsymi0TGbTt1Q2ilKkhzGPBETPZg8OPS1LrbRuSt1i1sHJRxlt1BVFCbLeeO6hbE~gAjxL8P~lYfYFbBfyOPnT8TrV5y51UA2HhrtuoloIrv-dslfcBd~MudYqb-xdhgsWqMn5pX0B9Stc1OwpCw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of... Available to Purchase
in An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure
> Bulletin of the Seismological Society of America
Published: 01 May 2009
Figure 7. Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001) . The triangle with vertices at three of the GPS
Image
![Coso Range (after Lewis et al. [2007]). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001). The triangle with vertices at three of the GPS stations is cell 34 of Lewis et al. (2007), which includes Wild Horse Mesa. The letter X labels the locations in Petroglyph Canyon and Sheep Canyon where the fault-slickenline data were gathered. Stars show locations from which the paleomagnetic orientations were determined; curved arrows around the stars show the paleomagnetic rotation of lavas in the fault stepover relative to the same lavas outside the stepover, which averages 12.0°±2.6°. Solid diamonds and open squares show the epicenters of earthquakes at greater than and less than 5 km depth, respectively; the focal mechanisms from these events were inverted for a solution of the local deformation. (b) Stereogram showing the orientations of the axis of maximum rates of lengthening () and shortening () inferred from the inversion of fault-slickenline data and from the inversion of GPS velocity data from the triangular cell shown in part (a). The boundary of the shaded areas is the locus of zero instantaneous extension. Lower hemisphere equal area projection. (c) Values of the deformation rate parameter D and the relative vorticity parameter W inferred from two independent methods: first, from the inversion of fault-slickenline data; and second, from the inversion of GPS velocities for the vertices of the triangular cell in part (a), which defines the macrovorticity and the maximum macroshear rate, and from the paleomagnetically determined block-rotation rates, which define the microvorticity.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/bssa/99/2B/10.1785_0120080084/2/s_1103fig7.jpeg?Expires=2147483647&Signature=vE9Iw5ugMowWi2UV8tGQvKUZ7vQe1MqsepZ1If1jE2aykyae0rlxP-g3iDO6nq4omHlk3HRzJ5XTjBQzkzoGxi5h2Zr8uguRkAqQZ19dDALe0vnvbW-HdeLaqS8kVypz0s86uFVYgwFfCkM-LZY~Wk3e-1U8LRVHZBwvA0iKRd17Z-JLoZF6rtiDj7m6d38g6LAnhZAOdjZ7XV1OLdhXomaIv4Lnsgi3I1Z01giKACZeqoAMi-ShbHBOcmZnuvV6dBrApvrK7zTgycqlgqUeXsRp~ywaI69Itl~AEjeqQrxBe6MTOQoOWOG1NrYdksSdjwVkGExomJ~tCtpjVQgRFQ__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of... Available to Purchase
in An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure
> Bulletin of the Seismological Society of America
Published: 01 May 2009
Figure 7. Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001) . The triangle with vertices at three of the GPS
Image
Figure 2. Location map and major geographic and geologic features discussed... Available to Purchase
Published: 01 November 2005
Figure 2. Location map and major geographic and geologic features discussed in this paper. Coso Range, Little Lake fault zone (LLFZ), Airport Lake fault zone (ALFZ), Coso Wash fault (CWF), White Hills anticline (WHA), Wild Horse Mesa fault (WHMF), Lower Centennial Flat (LCF), Haiwee Spring (HS
Image
Figure 5. Cross section through the Dooley and McClay (1997) 30° translat... Available to Purchase
Published: 01 November 2005
of model advancement. The “A” and “T” in the circles represent blocks moving away from and toward the viewer, respectively. Projected location of cross section A–A′ is shown on Figure 1 . LLF—Little Lake fault, ALF-CWF—Airport Lake fault–Coso Wash fault, WHMF—Wild Horse Mesa fault. Little Lake fault
Image
Test of the Fault-Slickenline Inversion Solution with GPS and Paleomagnetic... Available to Purchase
in An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure
> Bulletin of the Seismological Society of America
Published: 01 May 2009
Table 2 Test of the Fault-Slickenline Inversion Solution with GPS and Paleomagnetic Data for the Wild Horse Mesa Area in the Coso Range, East-Central California (from Lewis et al. , 2007 ) Fault-Slickenline Inversion Solution * GPS /Paleomag Solution † [plunge, trend
Image
Test of the Fault-Slickenline Inversion Solution with GPS and Paleomagnetic... Available to Purchase
in An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure
> Bulletin of the Seismological Society of America
Published: 01 May 2009
Table 2 Test of the Fault-Slickenline Inversion Solution with GPS and Paleomagnetic Data for the Wild Horse Mesa Area in the Coso Range, East-Central California (from Lewis et al. , 2007 ) Fault-Slickenline Inversion Solution * GPS /Paleomag Solution † [plunge, trend
Image
Test of the Fault-Slickenline Inversion Solution with GPS and Paleomagnetic... Available to Purchase
in An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure
> Bulletin of the Seismological Society of America
Published: 01 May 2009
Table 2 Test of the Fault-Slickenline Inversion Solution with GPS and Paleomagnetic Data for the Wild Horse Mesa Area in the Coso Range, East-Central California (from Lewis et al. , 2007 ) Fault-Slickenline Inversion Solution * GPS /Paleomag Solution † [plunge, trend
Journal Article
The Coso geothermal field: A nascent metamorphic core complex Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 November 2005
GSA Bulletin (2005) 117 (11-12): 1534–1553.
...Figure 2. Location map and major geographic and geologic features discussed in this paper. Coso Range, Little Lake fault zone (LLFZ), Airport Lake fault zone (ALFZ), Coso Wash fault (CWF), White Hills anticline (WHA), Wild Horse Mesa fault (WHMF), Lower Centennial Flat (LCF), Haiwee Spring (HS...
FIGURES
Journal Article
An Asymmetric Micropolar Moment Tensor Derived from a Discrete-Block Model for a Rotating Granular Substructure Available to Purchase
Publisher: Seismological Society of America
Published: 01 May 2009
Bulletin of the Seismological Society of America (2009) 99 (2B): 1103–1131.
...Figure 7. Coso Range (after Lewis et al. [2007] ). (a) Map showing the location of the Coso Range in east central California and of Wild Horse Mesa within the Coso Range. Labeled open dots are the GPS stations of McClusky et al. (2001) . The triangle with vertices at three of the GPS...
FIGURES
Journal Article
Millennial-scale dynamics of valley fills over the past 12,000 14 C yr in northeastern New Mexico, USA Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 November 2007
GSA Bulletin (2007) 119 (11-12): 1433–1448.
... of incision was a series of unusually frequent and large floods following a series of severe droughts ( Hereford, 1986 , 1993 , 2002 ; Hereford et al., 1996 ). Wild Horse Arroyo was enlarged significantly by the flood of August 27–28, 1908, which was caused by a torrential thunderstorm over Johnson Mesa...
FIGURES
Journal Article
Geologic Road Log of Pan-american Highway, Laredo to Mexico City Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 April 1936
AAPG Bulletin (1936) 20 (4): 457–466.
... of northern Mexico. Here is located the large American Smelting and Refining Company and American Metal Company smelters; steel mills; cement plants; the large Guactemoc brewery—free beer from 12 to 2 P.M. in park. Pancho Villa stabled his horses in the lobby of the Ancira Hotel. The notable points...
FIGURES
Journal Article
HENRY FAIRFIELD OSBORN AND JURASSIC DINOSAUR RECONNAISSANCE IN THE SAN JUAN BASIN, ALONG THE COLORADO-UTAH BORDER, 1893–1900 Available to Purchase
Journal: Earth Sciences History
Publisher: History of Earth Sciences Society
Published: 01 October 2005
Earth Sciences History (2005) 24 (2): 159–174.
... and camping in the wilds, but the naturalist in Fellows allowed him to revel in the outdoors. Whether he was on a slow or a swift horse, he noticed everything and often jotted down every detail of the landscape.” 25 Fellows had information about a deposit of fossil vertebrates in his county in southwestern...
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Journal Article
Comparing the modern, Quaternary, and Neogene records of climate-controlled hillslope sedimentation in southeast Nevada Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 March 2001
GSA Bulletin (2001) 113 (3): 305–319.
... in the production and basinward delivery of hillslope detritus through Neogene, Quaternary, and modern time is readily seen at outcrop scale ( Fig. 2 ). In the Table Mesa basin ( Pederson, 1999 ), as well as neighboring basins ( Bohannon, 1984 ; Schmidt, 1994 ), the exposed Muddy Creek Formation lacks coarse...
FIGURES
Journal Article
EXPERIMENTAL TAPHONOMY OF KERATIN: A STRUCTURAL ANALYSIS OF EARLY TAPHONOMIC CHANGES Available to Purchase
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 10 October 2017
PALAIOS (2017) 32 (10): 647–657.
... with the epidermal outgrowth that supports the bristles, were dissected and placed in the freezer. However, the male bronze turkey provided was younger than expected—it only had very short bristles. To supplement this, dried beards of wild turkeys (same species as the domestic turkey) from older individuals...
FIGURES
Journal Article
Mid-Miocene rhyolite volcanism in northeastern Nevada: The Jarbidge Rhyolite and its relationship to the Cenozoic evolution of the northern Great Basin (USA) Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 July 2014
GSA Bulletin (2014) 126 (7-8): 1047–1067.
... after Coats (1987) . Abbreviations for mapped Jarbidge Rhyolite sampled in this study: M—Mahoganies; 7201—Peak 7201; WHR—Wild Horse Reservoir; MB—main body (includes the town of Jarbidge, the Jarbidge mining district, and exposures to the east and south). Black boxes with numbers give sample locations...
FIGURES
Journal Article
Seismicity, Stress State, and Style of Faulting of the Ridgecrest‐Coso Region from the 1930s to 2019: Seismotectonics of an Evolving Plate Boundary Segment Available to Purchase
Publisher: Seismological Society of America
Published: 02 June 2020
Bulletin of the Seismological Society of America (2020) 110 (4): 1457–1473.
... of ∼ 80 km . In contrast, the 2019 sequence only has an east–west extent of about 5–10 km (Fig. 8 ). Many previously seismically active tectonic features such as the Wild Horse Mesa, Cotton Wood fault region, central Indian Wells Valley faults, and western Little Lake fault zone remained...
FIGURES
Journal Article
EMIL BÖSE’S SEARCH FOR AN ANCIENT LANDMASS Available to Purchase
Journal: Earth Sciences History
Publisher: History of Earth Sciences Society
Published: 01 April 1994
Earth Sciences History (1994) 13 (1): 58–66.
... of cattle left, the furniture in the hacienda is entirely destroyed, the buildings are half ruined and extremely dirty, the gardens are abandoned, the irrigation ditches destroyed, the trails are lost mostly, of about one thousand horses are only 80 to 90 left, running wild in the desert. You can understand...
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Journal Article
THE ROLE OF GLACIERS AND GLACIER RESEARCH IN THE DEVELOPMENT OF U. S. NATIONAL PARKS Available to Purchase
Journal: Earth Sciences History
Publisher: History of Earth Sciences Society
Published: 01 October 2017
Earth Sciences History (2017) 36 (2): 337–358.
..., which purpose is to conserve the scenery and the natural and historic objects and the wild life therein and to provide for the enjoyment of the same in such manner and by such means as will leave them unimpaired for the enjoyment of future generations (Office of the Law Revision Counsel 2016). Note...
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