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    Tectonic geomorphology of the Toroweap Fault, western Grand Canyon, Arizona: Implications for transgression of faulting on the Colorado Plateau

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    Author
    Jackson, G.W.
    Issue Date
    1990
    Keywords
    Arizona Geological Survey Open File Reports
    Mohave County
    Colorado Plateau
    Grand Canyon
    Toroweap Fault
    Arizona
    faulting
    fault
    tectonic geomorphology
    geomorphology
    Geology
    Cenozoic
    Late Tertiary
    Quaternary
    Pleistocene
    Holocene
    Vulcan's Throne
    Toroweap Valley
    Prospect Valley
    North rim Grand Canyon
    Whitmore Wash
    alluvium
    alluvial fan
    Uinkaret Volcanic field
    Sevier Fault
    Aubrey Fault
    basalts
    cinder cones
    soil profile
    transgression
    magnitude
    slip rate
    recurrence rate
    geologic hazard
    escarpment
    fault scarp
    geochronology
    relative geochronology
    morphology
    carbonate
    climate
    Show allShow less
    
    Metadata
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    Citation
    Jackson, G.W., 1990, Tectonic geomorphology of the Toroweap Fault, western Grand Canyon, Arizona: Implications for transgression of faulting on the Colorado Plateau. Arizona Geological Survey Open File Report, OFR-90-04, 2 map sheets, map scale 1:24,000, 67 p.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    Tectonic geomorphology of the Toroweap Fault, western Grand Canyon, Arizona: implications for transgression of faulting on the Colorado Plateau. The Toroweap fault is a major normal fault in Northwestern Arizona. Along its southern end are four displaced Quaternary surfaces, three of which have measurable displacements that are multiples of about 2.2 m. Soil carbonate analysis was carried out to estimate ages for the three surfaces. An extrapolated carbonate accumulation was used to estimate an age for the oldest surface of between 26 and 54 ka; the youngest displaced surface is between 4 and 11 ka. Oldest undisplaced surface is 2 ± 1 ka. Diffusion modelling determined the most recent surface rupture to be 3 ± 1 ka. An aid in determining degree of tectonic activity where displaced materials are not present is the escarpment sinuosity index (Es). Escarpment length was divided by fault length. Because cliff height varies from one area to another, the index was normalized by dividing by total cliff height. The index is inversely proportional to total displacement. Segments of the fault were distinguished using Es, presence and style of Quaternary displacements, and changes in fault orientation. There are five segments in the study area, the most active segment spanning the Grand Canyon. Report and two map sheets, map scale 1:24,000.
    URI
    http://hdl.handle.net/10150/630851
    Additional Links
    https://library.azgs.arizona.edu/
    Language
    en
    Series/Report no.
    OFR-90-04
    Rights
    Arizona Geological Survey. All rights reserved.
    Collection Information
    Documents in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
    North Bounding Coordinate
    38.2882
    South Bounding Coordinate
    35.709
    West Bounding Coordinate
    -114.033
    East Bounding Coordinate
    -112.165
    Collections
    AZGS Document Repository

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