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.
Geology of the northern part of the Diamond Range, Eureka and White Pine Counties, Nevada
AuthorHaworth, Wiliam D.
AdvisorLintz, J., Jr.
Geological Sciences and Engineering
AltmetricsView Usage Statistics
Upper Paleozoic rocks of the post-orogenic overlap assemblage are exposed throughout the northern part of the Diamond Range. The limestones, siItstones, sandstones, shales, and conglomerates are characterized by abundant chert and quartz that was reworked from eugeosynclinal rocks exposed in the source area to the west. Continental sediments of the Newark Canyon Formation were deposited during the Early Cretaceous on an erosional surface above the Carbon Ridge Formation of Permian age.
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.
Newark Canyon Formation
Mackay Science Project