A finite-difference, inverse groundwater flow model of Pahute Mesa, Nevada Test Site, Nye County, Nevada

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A finite-difference inverse groundwater flow model was developed for Pahute Mesa located in Nye County, Nevada. The model results appear to support the existence of a hydraulic barrier at Pahute Mesa.

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Thesis Number: 3226.
Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.

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University of Nevada, Reno

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