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RIVER AVULSIONS AND THEIR DEPOSITS

Slingerland, Rudy, Smith, Norman D.·2004·Annual Review of Earth and Planetary Sciences

Abstract

▪ Abstract Avulsion is the natural process by which flow diverts out of an established river channel into a new permanent course on the adjacent floodplain. Avulsions are primarily features of aggrading floodplains. Their recurrence interval varies widely among the few modern rivers for which such data exist, ranging from as low as 28 years for the Kosi River (India) to up to 1400 years for the Mississippi. Avulsions cause loss of life, property damage, destabilization of shipping and irrigation channels, and even coastal erosion as sediment is temporarily sequestered on the floodplain. They are also the main process that builds alluvial stratigraphy. Their causes remain relatively unknown, but stability analyses of bifurcating channels suggest that thresholds in the relative energy slope and Shields parameter of the bifurcating channel system are key factors.

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Metadata

Authors
Slingerland, R., & Smith, N. D.
Venue
Annual Review of Earth and Planetary Sciences
Published
2004-05-19
Volume
32
Issue
1
Pages
257-285
ISSN
  • 0084-6597 (ISSN-L)
  • 1545-4495
OpenAlex
W2139920049
Cited by
689
References
0
FWCI
1.35
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: RIVER AVULSIONS AND THEIR DEPOSITS. https://app.cochat.ai/papers/10.1146/annurev.earth.32.101802.120201
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Slingerland, R., & Smith, N. D. (2004). RIVER AVULSIONS AND THEIR DEPOSITS. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.32.101802.120201

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