4.2 Article

In defence of the meltwater (megaflood) hypothesis for the formation of subglacial bedform fields

Journal

JOURNAL OF QUATERNARY SCIENCE
Volume 25, Issue 3, Pages 249-260

Publisher

WILEY
DOI: 10.1002/jqs.1264

Keywords

flow path; large-scale fluting; hummocky terrain; clast lags; ice-pushed moraines

Funding

  1. Natural Sciences and Engineering Research Council of Canada [G12110428]

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Characteristics of large-scale fluting and hummocky terrain on the Canadian Prairies test glacial and meltwater hypotheses for landform genesis. These tests defend the meltwater model. Neither sedimentary nor glaciotectonic processes can fully explain such erosional landforms. Province-scale flow paths, which mark palaeo-ice streams and subglacial flood routes, contain large-scale fluting with flanking hummock terrain. Antecedent relief causes these paths to differ from other flood landscapes such as the Scablands. Proponents of the glacial hypothesis use an invalid analogy between Icelandic and Prairie landsystems. They suggest that groove-ploughing formed large-scale fluting, and that ice pushing created hummocky terrain. However, landform location, form, and extent, surface lags, truncated architecture, and landform associations favour the meltwater hypothesis. A simple thought experiment and clear understanding of the principle of least number of assumptions answer the criticisms that meltwater forms cannot cross-cut and that the meltwater hypothesis disregards proper hypothesis testing. An example of cross-cutting erosional marks supports this theory. No narrow tract of smoothed terrain with fluting terminates at the glacially thrust Neutral Hills, negating an important point in the glacial hypothesis. While neither the glacial hypothesis nor postglacial winnowing explain boulder and cobble lags with percussion marks, meltwater processes explain them well. Copyright (C) 2009 John Wiley & Sons, Ltd.

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