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    The Geology of the Safford-San Carlos Area, Graham and Gila Counties, East-Central Arizona

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    Author
    Mock, A.P.
    Issue Date
    2008
    Keywords
    Arizona Geological Survey Contributed Reports
    Arizona
    Gila County
    Graham County
    Safford
    San Carlos
    sedimentary deposits
    low-permeability rock
    fluvial deposits
    basins
    Geology
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    Citation
    Mock, A.P., 2008, The Geology of the Safford-San Carlos Area, Graham and Gila Counties, East-Central Arizona: Arizona Geological Survey Contributed Report CR-08-A, 59 p. with appendix and figures.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    In flowing from its origins in the mountains of west-central New Mexico down to the broad sedimentary basins of central Arizona's Salt River Valley, the Gila River and its enclosing fluvial deposits are tightly enclosed by strongly-consolidated, low-permeability rock. An exception is the broad and deep expanse of sedimentary deposits crossed by the Gila River in the Safford-San Carlos area of east-central Arizona. An interconnected chain or complex of geologic structural subbasins in this area is filled with thousands of feet of weakly- to moderately-consolidated sedimentary deposits. These sedimentary deposits have the potential for storing and transmitting much more water than the strongly-consolidated rock of surrounding mountain ranges. This chain of structural subbasins will collectively be called the Safford-San Carlos Area Subbasin Complex in this report.In flowing from its origins in the mountains of west-central New Mexico down to the broad sedimentary basins of central Arizona's Salt River Valley, the Gila River and its enclosing fluvial deposits are tightly enclosed by strongly-consolidated, low-permeability rock. An exception is the broad and deep expanse of sedimentary deposits crossed by the Gila River in the Safford-San Carlos area of east-central Arizona. An interconnected chain or complex of geologic structural subbasins in this area is filled with thousands of feet of weakly- to moderately-consolidated sedimentary deposits. These sedimentary deposits have the potential for storing and transmitting much more water than the strongly-consolidated rock of surrounding mountain ranges. This chain of structural subbasins will collectively be called the Safford-San Carlos Area Subbasin Complex in this report.
    URI
    http://hdl.handle.net/10150/630826
    Additional Links
    http://repository.azgs.az.gov/uri_gin/azgs/dlio/390
    Language
    en
    Series/Report no.
    CR-08-A
    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
    34.1618
    South Bounding Coordinate
    32.1756
    West Bounding Coordinate
    -111.665
    East Bounding Coordinate
    -109.116
    Collections
    AZGS Document Repository

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