The Geology of the Mono Craters, California

The Geology of the Mono Craters, California

<p>The Mono Craters are a chain of extinct obsidian domes, coulees, and lapilli cones lying south of Mono Lake in eastern California. They are slightly more than ten miles long, are ranged along a curving fracture roughly parallel to the Sierra Nevada, and are divided into three nearly equal p...

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Bibliographic Details
Main Author: Putnam, William Clement
Format: Others
Published: 1937
Online Access:https://thesis.library.caltech.edu/7027/4/Putnam_wc_1937-1.pdf
Putnam, William Clement (1937) The Geology of the Mono Craters, California. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/E8PG-SX27. https://resolver.caltech.edu/CaltechTHESIS:05142012-135105262 <https://resolver.caltech.edu/CaltechTHESIS:05142012-135105262>

Internet

https://thesis.library.caltech.edu/7027/4/Putnam_wc_1937-1.pdf
Putnam, William Clement (1937) The Geology of the Mono Craters, California. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/E8PG-SX27. https://resolver.caltech.edu/CaltechTHESIS:05142012-135105262 <https://resolver.caltech.edu/CaltechTHESIS:05142012-135105262>

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