Field testing of Glew and Ford's model of solution flute evolution
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Publication Date
July 2001
Abstract
Based on a laboratory simulation, Glew and Ford (Earth Surface Processes, 1980, vol. 5, pp. 25–36) put forward a model of solution flute formation which embraces both morphological evolution and time to formation. The occurrence of dated fluted surfaces in the field presents opportunities to test this model. The morphological development of flutes is consistent with the experimental observations in that width stabilizes early whereas depth continues to increase. The time to formation of flutes is confirmed as limestone (103 years)>gypsum (102 years)>salt (101 years), and is consistent with the solubility of the main rock‐forming minerals. Copyright © 2001 John Wiley & Sons, Ltd.
Keywords
Solution Flutes, Rate Of Formation, Dated Surfaces
Document Type
Article
Notes
Earth Surface Processes and Landforms, Vol. 26, no. 8 (2001-07-17).
Identifier
SFS0046511_00001
Recommended Citation
Mottershead, Derek and Lucas, Gerald, "Field testing of Glew and Ford's model of solution flute evolution" (2001). KIP Articles. 1907.
https://digitalcommons.usf.edu/kip_articles/1907