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    Geologic map of the Oracle Junction 7.5' Quadrangle and the eastern third of the Tortolita Mountains 7.5' Quadrangle, Pima and Pinal Counties, Arizona v. 2.0

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    Author
    Skotnicki, S.J.
    Issue Date
    2022
    Keywords
    Arizona Geological Survey Open File Reports
    Paleozoic
    upper Jurassic
    cretaceous
    Quaternary
    Pleistocene
    Late Tertiary
    American Flag Formation
    Cambrian Abrigo Formation
    Carpas Wash
    Guild Wash Fault
    Faraway Tank
    Arizona
    Pinal County
    Pima County
    oracle junction
    Tortolita Mountains
    Pinal Schist
    Oro Valley
    Cambrian Bolsa Quartzite
    melanocratic bands
    micas
    quartz
    Cordones
    granitic rocks
    conglomerate
    sandstones
    metasedimentary
    Proterozoic
    Recent
    Mesozoic
    Holocene
    piedmont
    alluvium
    basalt
    Bisbee Group
    intrusives
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    Citation
    Skotnicki, S.J., 2000, Geologic map of the Oracle Junction 7.5' Quadrangle and the eastern third of the Tortolita Mountains 7.5' Quadrangle, Pima and Pinal Counties, Arizona. Arizona Geological Survey Open File Report, OFR-00-04, 1 map sheet, map scale 1:24,000, 19 p.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    This study encompasses the whole of the Oracle Junction 7.5' quadrangle and the eastern third of the Tortolita Mountains 7.5' quadrangle (see figure 1). Late Tertiary basin-fill deposits and younger Quaternary surficial deposits dominate most of the region and are well-exposed along the length of Oro Valley. The western third or so is underlain by a broad, flat pediment on the east side of the Tortolita Mountains. The pediment was etched into Proterozoic and Tertiary granitic rocks and is punctuated by more resistant hills of Pinal Schist and an east-northeast-trending band of younger metasedimentary rocks. Middle and Late Pleistocene sandstones and conglomerates lap up onto the pediment. These deposits contain material eroded from the granitic rocks and show very little topographic relief relative to the pediment. As a result, in aerial photographs, and locally even from a short distance away (tens to hundreds of meters), these deposits are nearly indistinguishable from the bedrock pediment.
    URI
    http://hdl.handle.net/10150/630615
    Additional Links
    https://library.azgs.arizona.edu/item/ADGM-1669146135392-574
    Language
    en
    Series/Report no.
    DGM-156
    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
    32.621
    South Bounding Coordinate
    32.5
    West Bounding Coordinate
    -111.038
    East Bounding Coordinate
    -110.871
    Collections
    AZGS Document Repository

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