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    Breccia-pipe Uranium Mining in the Grand Canyon Region and Implications for Uranium Levels in Colorado River Water

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    Author
    Spencer, J.E.
    Wenrich, K.
    Issue Date
    2011-04-28
    Keywords
    Arizona Geological Survey Open File Reports
    Recent
    Kaibab National Forest
    Grand Canyon National Park
    Mohave County
    Coconino County
    Colorado River
    Kanab Creek
    northern Arizona
    Grand Canyon
    Arizona Strip
    Redwall Limestone
    Hermit Shale
    water quality
    uranium mining
    water contamination
    mineralization
    Draft EIS
    breccia-pipes
    uranium
    breccia pipe
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    Citation
    Spencer, J.E. and Wenrich, K., 2011, Breccia-pipe Uranium Mining in the Grand Canyon Region and Implications for Uranium Levels in Colorado River Water. Arizona Geological Survey Open File Report, OFR-11-04, 1 appendix, 11 p.
    Description
    The Grand Canyon region contains over 1300 known or suspected breccia pipes, which are vertical, pipe-shaped bodies of highly fractured rock that collapsed into voids created by dissolution of underlying rock. Some breccia pipes were mineralized with uranium oxide as well as sulfides of copper, zinc, silver, and other metals. Renewed exploration during and following a steep rise in uranium prices during 2004-2007 led some to concerns about contamination of the Colorado River related to uranium mining and ore transport. Total breccia-pipe uranium production as of Dec. 31, 2010 has been more than 10,700 metric tons (23.5 million pounds) from nine underground mines, eight of which are north of Grand Canyon near Kanab Creek. Colorado River water in the Grand Canyon region currently contains about 4 µg/l (micrograms per liter) of uranium (equivalent to 4 ppb [parts per billion by mass]), with approximately 15 cubic kilometers annual discharge. Thus, approximately 60 metric tons of dissolved uranium are naturally carried by the Colorado River through the Grand Canyon in an average year. We consider a hypothetical, worst-case accident in which a truck hauling thirty metric tons (66,000 pounds) of one-percent uranium ore is overturned by a flash flood in Kanab Creek and its entire ore load is washed into the Colorado River where it is pulverized and dissolved during a one-year period to become part of the dissolved uranium content of the river (such a scenario is extremely unlikely if not impossible). This addition of 300 kilograms (660 pounds) of uranium over one year would increase uranium in river water from 4.00 ppb to 4.02 ppb. Given that the EPA maximum contaminant level for uranium in drinking water is 30 ppb, this increase would be trivial. Furthermore, it would be undetectable against much larger natural variation in river-water uranium content.
    URI
    http://hdl.handle.net/10150/629699
    Additional Links
    https://library.azgs.arizona.edu/item/AOFR-1552426569504-522
    Language
    en
    Series/Report no.
    OFR-11-04
    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
    36.7062
    South Bounding Coordinate
    35.4185
    West Bounding Coordinate
    -114.741
    East Bounding Coordinate
    -111.786
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