全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

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

DOI: 10.4236/ojg.2019.98027, PP. 404-423

Keywords: Beaver Divide Escarpment, Continental Ice Sheet Melt Water Floods, East-West Continental Divide, Great Divide Basin, Wind River Basin, Wind River Mountains

Full-Text   Cite this paper   Add to My Lib

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.

References

[1]  Kuhn, T.S. (1970) The Structure of Scientific Revolutions. 2nd Edition, University of Chicago Press, Chicago, IL, 210 p.
[2]  Clausen, E. (2018) Deep Erosion by Continental Ice Sheets: A Northern Missouri River Drainage Basin Perspective: North America. Current Research in Geoscience, 8, 27-38.
https://doi.org/10.3844/ajgsp.2018.27.38
[3]  Love, J.D. and Christiansen, A.C. (1985) Geologic map of Wyoming: United States Geological Survey, Wyoming State Geological Survey Release, 2014.
[4]  Johnson, J.F. and Sutherland, W.M. (2009) Geologic Map of the Lander 30’ x 60’ Quadrangle, Fremont County, Wyoming. Wyoming State Geological Survey, Map Series.
[5]  Lohman, K.E. and Andrews, G.W. (1968) Late Eocene Nonmarine Diatoms from the Beaver Divide area, Fremont County, Wyoming. United States Geological Survey Professional Paper 593-E, 1-26.
https://doi.org/10.3133/pp593E
[6]  Bauer, C.M. (1934) Wind River Basin. Bulletin of the Geological Society of America, 45, 665-695.
https://doi.org/10.1130/GSAB-45-665
[7]  Mears Jr., B. (1993) Geomorphic History of Wyoming and High-Level Erosion Surfaces. In: Snoke, A.W., Steidtmann, J.R. and Roberts, S.M., Eds., Geology of Wyoming: Geological Survey of Wyoming Memoir No. 55, Laramie, Wyoming, 608-626.
[8]  Lillegraven, J.A. and Ostresh Jr., L.J. (1988) Evolution of Wyoming’s Early Cenozoic Topography and Drainage Patterns. National Geographic Research, 4, 303-327.
[9]  Galloway, W.E., Whiteaker, T.L. and Ganey-Curry, P. (2011) History of North American Drainage Evolution, Sediment Yield, and Accumulation in the Gulf of Mexico Basin. Geosphere, 7, 938-973.
https://doi.org/10.1130/GES00647.1
[10]  Sinclair, W.J. and Granger, W. (1911) Eocene and Oligocene of the Wind River and Bighorn Basins: American Museum of Natural History Bulletin, 30, 84-117.
[11]  Mackin, J.H. (1937) Erosional History of the Bighorn Basin, Wyoming. Geological Society of America Bulletin, 48, 813-894.
https://doi.org/10.1130/GSAB-48-813
[12]  Riihimaki, C.A., Anderson, R.S. and Safran, E.B. (2007) Impact of Rock Uplift on Rates of Late Cenozoic Rocky Mountain River Incision. Journal of Geophysical Research, 112, F03S02.
https://doi.org/10.1029/2006JF000557
[13]  Howard, A.D. (1960) Cenozoic History of Northeastern Montana and Northwest North Dakota with Emphasis on the Pleistocene. United States Geological Survey Professional Paper 326, 107.
https://doi.org/10.3133/pp326
[14]  Jackson, L. (2018) The Paleo-Bell River: North America’s Vanished Amazon. Earth, 63, 74-81.
[15]  White, W.A. (1972) Deep Erosion by Continental Ice Sheets. Geological Society of America Bulletin, 83, 1037-1056.
https://doi.org/10.1130/0016-7606(1972)83[1037:DEBCIS]2.0.CO;2
[16]  Gravenor, C.P. (1975) Erosion by Continental Ice Sheets. American Journal of Science, 275, 594-604.
https://doi.org/10.2475/ajs.275.5.594
[17]  Sugden, D.E. (1976) A Case against Deep Erosion of Shields by Continental Ice Sheets. Geology, 4, 580-582.
https://doi.org/10.1130/0091-7613(1976)4<580:ACADEO>2.0.CO;2
[18]  Clausen, E. (2018) Geomorphic History of the Beaver Creek Drainage Basin as Determined from Topographic Evidence: Eastern Montana and Western North Dakota. Journal of Geography and Geology, 10, 79-91.
https://doi.org/10.5539/jgg.v10n3p79
[19]  Clausen, E. (2019) Origin of the Redwater River Drainage Basin Determined by Topographic Map Interpretation: Eastern Montana, USA. Journal of Geography and Geology, 11, 42-54.
https://doi.org/10.5539/jgg.v11n1p42
[20]  Clausen, E. (2018) Probable Deep Erosion by Continental Ice Sheet Melt Water Floods: Chalk Buttes Area of Carter County, Montana, USA. International Journal of Geography and Geography (Conscientia Beam), 7, 14-26.
https://doi.org/10.18488/journal.10.2018.71.14.26
[21]  Clausen, E. (2018) Topographic Analysis of Laramie Range Bedrock-Walled Canyon Complex and the Goshen Hole Escarpment-Surrounded Basin, Albany and Platte Counties, Southeast Wyoming, USA. Open Journal of Geology, 8, 33-55.
https://doi.org/10.4236/ojg.2018.81003
[22]  Clausen, E. (2018) Topographic Map Analysis of High Elevation Black Hills through Valleys Linking Spearfish and Rapid Creek Headwaters Valleys, Lawrence County, South Dakota, USA. Journal of Geography and Geology, 10, 8-21.
https://doi.org/10.5539/jgg.v10n1p8
[23]  Clausen, E. (2019) Upper Sun River Drainage Basin Origin Determined by Topographic Map Interpretation Techniques: Lewis and Clark and Teton Counties, Montana, USA. Open Journal of Geology, 9, 257-277.
https://doi.org/10.4236/ojg.2019.95018
[24]  Clausen, E. (2019) Topographic Map Interpretation of the Bighorn River-Wind River Drainage Divide Area Located East of Wyoming’ Wind River Canyon. Universal Journal of Geoscience, 7, 56-67.
[25]  Steidtmann, J.R., Middleton, L.T. and Shuster, M.W. (1989) Post-Laramide (Oligocene) Uplift in the Wind River Range, Wyoming. Geology, 17, 38-41.
https://doi.org/10.1130/0091-7613(1989)017<0038:PLOUIT>2.3.CO;2
[26]  Baker, V.R. (1981) Large-Scale Erosional and Depositional Features of the Channel Scabland. In: Baker, V.R., Ed., Catastrophic Flooding: The Origin of the Channeled Scabland, Dowden, Hutchinson and Ross, Inc., Stroudsburg, 276-310.
[27]  Bishop, P. (1995) Drainage Rearrangement by River Capture, Beheading and Diversion. Progress in Physical Geography, 19, 449-473.
https://doi.org/10.1177/030913339501900402
[28]  Love, J.D. (1970) Cenozoic Geology of the Granite Mountains Area, Central Wyoming. United States Geological Survey Professional Paper 495-C, 154 p.
https://doi.org/10.3133/pp495C
[29]  Anderson, D.L. (2002) Occam’s Razor: Simplicity, Complexity, and Global Dynamics. Proceeding of the American Philosophical Society, 146, 56-76.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133