Hostname: page-component-586b7cd67f-rdxmf Total loading time: 0 Render date: 2024-11-25T14:47:55.858Z Has data issue: false hasContentIssue false

Gradational Thresholds and Landform Singularity: Significance for Quaternary Studies—A Reply

Published online by Cambridge University Press:  20 January 2017

Z. B. Begin
Affiliation:
The Geological Survey of Israel Jerusalem, Israel
S. A. Schumm
Affiliation:
Colorado State University Fort Collins, Colorado USA

Abstract

Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Letters to the Editor
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Begin, Z.B. 1981 The relationship between flow shear stress and stream pattern Journal of Hydrology 52 307319 Google Scholar
Begin, Z.B. Schumm, S.A. 1979 Instability of alluvial valley floors—A method for its assessment American Society of Agricultural Engineers, Transactions 22 347350 Google Scholar
Bradley, M.T. 1980 Gully Development and Valley Stability, North-eastern Colorado Unpublished M.S. thesis Colorado State University Fort Collins Google Scholar
Brakenridge, G.R. 1985 Discussion of “gradational thresholds and landform singularity: significance for Quaternary studies” Quaternary Research 23 Google Scholar
Patton, P.E. Schumm, S.A. 1975 Gully erosion, northern Colorado, a threshold phenomenon Geology 3 8890 Google Scholar
Schumm, S.A. Harvey, M.D. Watson, C.C. 1984 Incised Channels: Morphology Dynamics and Control Water Resources Publications Littleton, Colo Google Scholar