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Flood Plains

  • M. Gordon Wolman
  • Luna B. Leopold
Part of the Geographical Readings book series (GR)

Abstract

A Frequently quoted definition of a flood plain is that of Rice (1949, p. 139): ‘a strip of relatively smooth land bordering a stream [and] overflowed in times of high water’. Valley flats which would usually be considered flood plains, on this definition, include features formed by such processes as landslides and the building of low-angle fans. But the most important process resulting in the formation of valley flats is a combination of deposition on the inside of river curves and deposition from overbank flows. This process has produced many of the flat areas adjacent to river channels, and is probably responsible for most of the flood plains of the great rivers of the world. It is with this particular process that the present paper is concerned.

Keywords

Flood Plain Recurrence Interval Annual Flood Natural Levee Damage Stage 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Palgrave Macmillan, a division of Macmillan Publishers Limited 1970

Authors and Affiliations

  • M. Gordon Wolman
  • Luna B. Leopold

There are no affiliations available

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