Open Journal of Geology

Volume 9, Issue 8 (August 2019)

ISSN Print: 2161-7570   ISSN Online: 2161-7589

Google-based Impact Factor: 0.83  Citations  h5-index & Ranking

Use of Topographic Map Evidence to Test a Recently Proposed Regional Geomorphology Paradigm: Wind River-Sweetwater River Drainage Divide Area, Central Wyoming, USA

HTML  XML Download Download as PDF (Size: 897KB)  PP. 404-423  
DOI: 10.4236/ojg.2019.98027    578 Downloads   1,500 Views  Citations
Author(s)

Affiliation(s)

ABSTRACT

Topographic map evidence from the Wyoming Wind River-Sweetwater River drainage divide area is used to test a recently proposed regional geomorphology paradigm defined by massive south- and southeast-oriented continental ice sheet melt water floods that flowed across the entire Missouri River drainage basin. The new paradigm forces recognition of an ice sheet created and occupied deep “hole” and is fundamentally different from the commonly accepted paradigm in which a pre-glacial north- and northeast-oriented slope would have prevented continental ice sheet melt water from reaching or crossing the Wind River-Sweetwater River drainage divide. Divide crossings (or low points) are identified as places where water once flowed across the drainage divide. Map evidence is interpreted first from the accepted paradigm perspective and second from the new paradigm perspective to determine the simplest explanation. Both paradigm perspectives suggest south-oriented water crossed the drainage divide, although accepted paradigm interpretations do not satisfactorily explain the large number of observed divide crossings and are complicated by the need to bury the Owl Creek and Bridger Mountains to explain why the Wind River now flows in a north direction through Wind River Canyon. New paradigm interpretations explain the large number of divide crossings as diverging and converging channel evidence (as in flood-formed anastomosing channel complexes), Owl Creek and Bridger Mountain uplift to have occurred as south-oriented floodwaters carved Wind River Canyon, and a major flood flow reversal (caused by ice sheet related crustal warping and the opening up of deep “hole” space by ice sheet melting) as being responsible for the Wind River abrupt turn to the north. While this test only addresses topographic map evidence, Occam’s Razor suggests the new paradigm offers what in science should be the preferred Wind River-Sweetwater River drainage divide origin interpretations.

Share and Cite:

Clausen, E. (2019) Use of Topographic Map Evidence to Test a Recently Proposed Regional Geomorphology Paradigm: Wind River-Sweetwater River Drainage Divide Area, Central Wyoming, USA. Open Journal of Geology, 9, 404-423. doi: 10.4236/ojg.2019.98027.

Cited by

[1] How a New Cenozoic Geology and Glacial History Paradigm Explains Arkansas-Red River Drainage Divide Area Topographic Map Evidence in and near …
Open Journal of Geology, 2022
[2] Yampa River-Colorado River Drainage Divide Origin Determined from Topographic Map Evidence, Southern Routt County, Colorado, USA
2021
[3] How a New Geology and Glacial Paradigm Explains Colorado South Platte-Arkansas River Drainage Divide Topographic Map Evidence, USA
Open Journal of Geology, 2021
[4] Use of Topographic Map Evidence from Drainage Divides Surrounding Wyoming's Great Divide Basin to Compare Two Fundamentally Different Regional …
2020
[5] Topographic map analysis of mountain passes crossing the Continental Divide between Colorado River headwaters and North and South Platte River …
2020
[6] Use of Stream and Dismembered Stream Valleys Now Crossing Wyoming's Northern Laramie Mountains to Test a Recently Proposed Regional …
2019

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.