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Some aspects of the hydrogeology of the Spring Mountains and Pahrump Valley, Nevada, and environs, as determined by spring evaluation
(University of Nevada, Reno, 1966)
The hydrogeology of the Spring Mountains and Pahrump Valley, Nevada has been evaluated. Analysis of geology indicates that nearly all springs are controlled by impermeable fault contacts or exposure of cavernous systems.
Hydrologic and geologic aspects of ground-water recharge along the Humboldt River near Winnemucca, Nevada
(University of Nevada, Reno, 1967)
A method of determining amounts of water available for groundwater recharge at various localities on the Humboldt River, Nevada, between Comus and Rose Creek is developed using a high flow frequency analysis.