Lateral sediment sources and knickzones as controls on spatio-temporal variations of sediment transport in an Alpine river

Author:

Bekaddour Toufik1,Schlunegger Fritz1,Attal Mikaël2,Norton Kevin P.3

Affiliation:

1. Institut of Geological sciences; Baltzerstrasse, 1 + 3; 3012; Bern; Switzerland

2. School of Geosciences; Institute of Geography; Drummond Street; Edinburgh; UK

3. School of Geography; Environment and Earth Sciences; Victoria University of Wellington; New Zealand

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference69 articles.

1. Dispersal and Preservation of Tectonically Generated Alluvial Gravels in Sedimentary Basins

2. Changes of bedload characteristics along the Marsyandi River (central Nepal), implications for understanding hillslope sediment supply, sediment load evolution along fluvial networks, and denudation in active orogenic belts;Attal;Geol. Soc. Am. Spec. Pap.,2006

3. Bed load transport by natural rivers;Bagnold;Water Resour. Res.,1977

4. An empirical correlation of bedload transport rates in flumes and natural rivers;Bagnold;Proc. Roy. Soc.,1980

5. Drainage basins, channels, and flow characteristics of selected streams in Central Pennsylvania;Brush;U.S. Geol. Surv. Prof. Pap.,1961

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