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    Geological Map of the Redington 7.5’ Quadrangle, Cochise, Graham, and Pima Counties, Arizona v 3.0

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    Author
    Cook, J.P.
    Spencer, J.E.
    Affiliation
    Arizona Geological Survey
    Issue Date
    2018-09
    Keywords
    Arizona Geological Survey Digital Geologic Map
    Bisbee Group
    geologic hazard
    Galiuro Volcanics
    Quiburis Formation
    Cochise County
    Pima County
    Pinal County
    Redington
    Rincon Mountains
    Quaternary
    Miocene
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    Citation
    Cook, J.P. and Spencer, J.E., 2018, Geological Map of the Redington 7.5’ Quadrangle, Cochise, Graham, and Pima Counties, Arizona: Arizona Geological Survey Digital Geologic Map DGM-60, version 3.0, map scale 1:24,000, 13 p. and 1 map sheet.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    The Redington 7 ½' Quadrangle includes part of the northern San Pedro River and flanking valley fill, as well as two areas of bedrock on the east side of the valley (Figure 1). Production of this new geologic map continues the Arizona Geological Survey mapping program in the San Pedro River valley, and complements geologic mapping to the south of this quadrangle. The map area is located within the San Pedro River valley in the Basin and Range Province of southeastern Arizona. Oligocene to early Miocene, compositionally diverse volcanism in the Galiuro Mountains to the east of the map area occurred during the initiation of a period of severe tectonic extension that uncovered the Catalina-Rincon metamorphic core complex to the southwest (Dickinson and Shafiqullah, 1989; Dickinson, 1991). The San Pedro Valley was created in its basic form by this period of extensional faulting, which largely ended in the early to middle Miocene. Relative to this period of severe faulting, minor faulting affected the valley during late Miocene to Quaternary time, probably with declining activity over this time period. Laramide (latest Cretaceous to earliest Tertiary), steeply southwest dipping to locally overturned volcanic and sedimentary rocks are exposed over part of Redfield Canyon. These are overlain by gently dipping Oligocene to early Miocene Galiuro Volcanics. Tilting of the Laramide strata is thought to be Laramide, not middle Tertiary, because Galiuro Volcanics participated in the middle Tertiary extensional faulting in those areas where faulting occurred, and the Galiuro Volcanics that overlie the Laramide strata are only slightly tilted (Dickinson, 1991).
    URI
    http://hdl.handle.net/10150/631080
    Additional Links
    https://library.azgs.arizona.edu/item/ADGM-1674493496995-624
    Language
    en
    Series/Report no.
    DGM-60
    Sponsors
    Revised and re-released with funding from the USGS National Geological and Geophysical Data Preservation Program, award no. G17AP00114. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government.
    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
    32.5
    South Bounding Coordinate
    32.375
    West Bounding Coordinate
    -110.5
    East Bounding Coordinate
    -110.375
    Collections
    AZGS Document Repository

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