Add to ORKGOnline 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.The geology of the Carbon Ridge area has been studied. The structure in area indicates that post-Mississippian warping of the Chainman and Diamond Peak Formations bent the units down toward the south in the southern part of the study area
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...