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Channel Initiation and the Problem of Landscape Scale

Montgomery, David R., Dietrich, William E.·1992·Science

Abstract

Since the 1940s it has been proposed that landscape dissection into distinct valleys is limited by a threshold of channelization that sets a finite scale to the landscape. This threshold is equal to the hillslope length that is just shorter than that necessary to support a channel head. A field study supports this hypothesis by showing that an empirically defined topographic threshold associated with channel head locations also defines the border between essentially smooth, undissected hillslopes and the valley bottoms to which they drain. This finding contradicts assertions that landscapes are scale-independent and suggests that landscape response to changes in climate or land use depends on the corresponding changes in the threshold of channelization.

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Metadata

Authors
Montgomery, D. R., & Dietrich, W. E.
Venue
Science
Published
1992-02-14
Volume
255
Issue
5046
Pages
826-830
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2135955237
Cited by
742
References
0
FWCI
21.81
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Channel Initiation and the Problem of Landscape Scale. https://app.cochat.ai/papers/10.1126/science.255.5046.826
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Montgomery, D. R., & Dietrich, W. E. (1992). Channel Initiation and the Problem of Landscape Scale. Science. https://doi.org/10.1126/science.255.5046.826

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.