Abstract
“Buffalo”, Bull Lake, Pinedale; Temple Lake and Gannett Peak-Wyoming’s glacial geomorphology provides a scheme, derived largely from and near the Wind River Mountains, that is now used far beyond the provincial boundaries of the state. Although basically sound, existing controversy suggests a current need for evaluation of this chronological model, whose history gives a nice example of the nature of scientific work.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
