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    Island Mountains of Southeastern Arizona: Geology, Vegetation & Wildlife

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    Author
    Bezy, J.V.
    Conway, F.M.
    Affiliation
    Arizona Geological Survey
    Issue Date
    2020
    Keywords
    Chiracahua Mountains
    Cochise County
    Galiuro Mounatins
    Huachuca Mountains
    Mule Mountains
    Pima County
    Pinal County
    Pinaleno Mountains
    Rincon Mountains
    Santa Catalina Mountains
    Santa Cruz County
    Santa Rita Mountains
    Sierrita Mountains
    Southeastern Arizona
    Tortolita Mountains
    Tucson Mountains
    Whetstone Mountains
    Cenozoic
    Miocene
    Pliocene
    Tertiary
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    Citation
    Bezy, J.V. and Conway, F.M., 2020. Island Mountains of Southeastern Arizona: Geology, Vegetation & Wildlife. Arizona Geological Survey Down-to-Earth #24, 99 p.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    Eleven island-like mountain ranges tower thousands of feet above adjacent basins in southeastern Arizona. In the order that they are presented in this book, these island ranges are: Santa Catalina, Rincón, Tortolita, Santa Rita, Tucson, Galiuro, Pinaleño, Chiricahua, Mule, Huachuca, and Whetstone Mountains (Figure 1). These island mountains, together with over a dozen other ranges, that are either lower in elevation or more difficult to access, make up the Basin and Range geologic province of southeastern Arizona. Most of these ranges and intervening basins trend northwest-southeast and are part of the huge geologic Basin and Range Province that extends from southern Oregon to central Mexico. This mountain-vally topography results from a period of extension from about 15 to 5 million years ago that broke the crustal rocks of western North America into blocks, separated by steeply dipping faults. Some of these crustal blocks were uplifted to form ranges; other blocks subsided as much as 2.4 mi (4 km) to form deep basins. Streams cut deep canyons into the rising ranges and transported eroded boulders, cobbles, gravel, sand and clay to aprons of sediment - alluvial fans and bajadas - in nearby subsiding basins. Many of these sediment-filled basins had no drainage outlets to the sea and held shallow lakes (playas) that fluctuated in size with changes in climate. As the Santa Cruz and San Pedro Rivers and other streams integrated the drainage of southeastern Arizona with that of the Gila and Colorado Rivers, their tributaries eroded headward into the alluvial fill of these formerly closed basins. Today, ephemeral or seasonal drainages continue to deeply erode alluvial fans and bajadas on all sides of the ranges (Figure 2).
    URI
    http://hdl.handle.net/10150/643297
    Additional Links
    https://library.azgs.arizona.edu/item/DTES-1674490239991-37
    Language
    en
    Series/Report no.
    Down-To-Earth Series
    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
    32.9917
    South Bounding Coordinate
    31.3551
    West Bounding Coordinate
    -112.633
    East Bounding Coordinate
    -109.073
    Collections
    AZGS Document Repository

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