If you have any problems related to the accessibility of any content (or if you want to request that a specific publication be accessible), please contact (email@example.com). We will work to respond to each request in as timely a manner as possible.
Time-variant hydrogeologic and geochemical study of selected thermal springs in western Nevada
AuthorLyles, Bradley F.
AdvisorJacobson, Roger L.
Geological Sciences and Engineering
AltmetricsView Usage Statistics
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 showed nearly instantaneous responses to precipitation events; conversely, Farad and Saratoga hot springs showed lagged responses of six to 24 weeks respectively. Chemical and isotopic variability suggests that thermal waters have appreciable near-surface mixing, particularly at springs that show rapid responses to precipitation events. Stable isotopes of oxygen and hydrogen ranged from -16.3 to -11.0 and -132.0 to -102.0 respectively, implying that recharge waters are derived from widely varying elevations. The thermal systems derive most of their recharge from the Sierra Nevada.
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.
Showing items related by title, author, creator and subject.
Hydrogeologic analysis of shallow hole temperatures at Allen Springs and Lee Hot Springs, Churchill County, Nevada Miller, Donn William (University of Nevada, Reno, 1978)Temperature data has been obtained at a depth of 1 meter in the area of Lee Hot Springs and Allen Springs and is used to interpret their hydrogeologic implications.
.Hiner, John E. (University of Nevada, Reno, 1979)Field mapping in the northern Hot Springs Mountains, Churchill County, Nevada, indicates that the intersection of Basin and Range faults with an earlier fault zone corresponds with the location of the Desert Peak Geothermal ...
A Fail-safe, Bi-Linear Liquid Spring, Controllable Magnetorheological Fluid Damper for a Three-dimensional Earthquake Isolation System Cesmeci, Sevki (2017)Building codes governing building design and construction require that loss of human life is not anticipated during a large, infrequently occurring earthquake. However, earthquake-induced damage to the building load carrying ...