Now showing items 1-4 of 4
Time-variant hydrogeologic and geochemical study of selected thermal springs in western Nevada
(University of Nevada, Reno, 1985)
Infiltrating waters take -from 24 weeks to less than two weeks to reach the watertables of individual thermal systems, based on temporal variability of physical and chemical parameters. Steamboat and Walley’s hot springs ...
Environmental isotope hydrology of the Dixie Valley geothermal system, Dixie Valley, Nevada
(University of Nevada, Reno, 1982)
Stable isotopic samples were analyzed from rain, snow, springs, irrigation wells, and two deep geothermal wells. The stable isotopic analysis indicate that meteoric water from the mountains surrounding Dixie Valley continually ...
Stratigraphy, structure, geophysics, and water chemistry of the Jersey Valley area, Pershing and Lander Counties, Nevada
(University of Nevada, Reno, 1981)
The stratigraphy, structure, geophysics, and water chemistry of the Jersey Valley area have been studied. Photogeologic interpretation indicate faults forming grabens within Jersey Valley. Maximum subsurface temperature ...
Source of recharge to the Beowawe geothermal system, north-central Nevada
(University of Nevada, Reno, 1987)
The source of recharge to the Beowawe geothermal system was studied using geochemistry and isotope hydrology.