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    Bedrock Geology of the Santan Mountains, Pinal and Maricopa Counties, Arizona v. 2.0

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    Author
    Ferguson, Charles A.
    Skotnicki, Steven J.
    Affiliation
    Arizona Geological Survey
    Issue Date
    2024
    Keywords
    bedrock geology
    crystalline rocks
    fissure
    Geology
    metamorphics
    pediment
    volcanic
    Cretaceous
    Laramide Orogeny
    Middle Tertiary
    Proterozoic
    Arizona
    Gila River
    Goldmine Mountain
    Higley Basin
    Maricopa County
    Mineral Butte
    Pinal County
    Poston Butte
    Sacaton Mountains
    Santan Mountains
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    Metadata
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    Citation
    Ferguson, C. A. and Skotnicki, S. J., 2024, Bedrock Geology of the Santan Mountains, Pinal and Maricopa Counties, Arizona v. 2.0, DGM-249
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    The Santan Mountains are a 25 km long, west-northwest trending uplift composed chiefly of Proterozoic and Cretaceous crystalline rocks overlain in the central and eastern part of the range by Mid-Tertiary sedimentary and volcanic rocks. Santan Mountain at an elevation of 3010 feet is the range's highest point, rising nearly 1700 feet above the basin floor. Elevations decrease rapidly to the southeast towards the Gila River. The eastern two thirds of the range are composed of low hills connected by extensive areas of pedimented bedrock where relief is rarely greater than 400 feet. The range is bounded to the north by the Higley basin, and no extensive, pedimented bedrock surfaces exist here. Instead, abrupt thickening of the basin fill is suggested by the numerous earth fissures along the range's north edge (Harris, 1994; Sank, 1975). To the south, like the east, an extensive dissected granitic pediment extends all the way to the Gila river. Extensive pediments in the Sacaton Mountains to the southwest also probably extend northward to the Gila River, suggesting that the low area between the two ranges was created more by erosional processes than by tectonic processes. At Poston Butte, near the eastern terminus of the Santan Mountains, crystalline bedrock occurs less than ISO meters below the Gila River (Hoag, 1996). This geodatabase is part of a digital reproduction of a 1996 geologic map originally created by the Arizona Geological Survey funded by the Arizona Geological Survey and the U.S. Geological Survey STATEMAP Program Contract#1434-95-A-1353. Preparation for republication was conducted by students from the University of Arizona with financial support from the U.S. Geological Survey, National Geological and Geophysical Data Preservation Program (G23AP00215) and included the production of a new GIS geodatabase and a revised map layout. The following text report has not been altered and remains identical to the 1996 original, but there may be situations where unit names, ages, symbology, or other geologic information contained within this report do not match the information presented in the new map layout or GIS geodatabase.
    URI
    http://hdl.handle.net/10150/678598
    Additional Links
    https://library.azgs.arizona.edu/
    Language
    en
    Series/Report no.
    DGM-249
    Rights
    Arizona Geological Survey. All rights reserved.
    Collection Information
    Documents in the AZGS Documents 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
    33.1997
    South Bounding Coordinate
    33.0019
    West Bounding Coordinate
    -111.802
    East Bounding Coordinate
    -111.469
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    AZGS Document Repository

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