Analyses of three different areas indicate that chain curvature controls chain length indirectly through valley‐side plan form. It follows that, since concave chains on one side of a stream are usually matched by convex chains on the other side, tributary development and abstraction do not occur independently along either side of a stream, as has hitherto been assumed.
Earth Surface Processes and Landforms – Wiley
Published: Jan 1, 1982
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