How River Rocks Round: Resolving the Shape-Size Paradox
Abstract
River-bed sediments display two universal downstream trends: fining, in which particle size decreases; and rounding, where pebble shapes evolve toward ellipsoids. Rounding is known to result from transport-induced abrasion; however many researchers argue that the contribution of abrasion to downstream fining is negligible. This presents a paradox: downstream shape change indicates substantial abrasion, while size change apparently rules it out....
Paper Details
Title
How River Rocks Round: Resolving the Shape-Size Paradox
Published Date
Feb 12, 2014
Journal
Volume
9
Issue
2
Pages
e88657 - e88657
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