Landslides and Gullies Interact as Sources of Lake Sediments in a Rifting Context: Insights from a Highly Degraded Mountain Environment

Liuelsegad Belayneh Bunare, Olivier Dewitte, Guchie Gulie, Jean Poesen, Daniel O'Hara, Alemayehu Kasaye Tilahun, Tizita Endale Elcho, Matthieu Kervyn

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Like many other lakes in the world, the interconnected Abaya and Chamo lakes in the Southern Main Ethiopian Rift are affected by rapid sediment accumulation. Although land degradation is a well-known issue in this part of the African continent, the main sediment sources, their spatial distribution and interaction in the Abaya–Chamo lakes’ basin have not yet been documented. Here, we present a systematic inventory, characterization, and spatial analysis of landslides and gullies as concentrated sediment sources, for four representative river catchments impacted by landscape rejuvenation. Using Google Earth imagery and field surveys, we mapped with high accuracy a total of 7336 gullies and 430 landslides. Recent landslides observed during the last decade were few, small and shallow, and appear to have played a minor role in the current sediment dynamics. Large landslides are old and inactive. Although they do not contribute to the current sediment budget, they contribute indirectly to landscape dynamics by favoring the occurrence of gullies. Overall, large percentages of severe to extremely degraded areas of gully erosion are located in rejuvenated landscapes, especially at the level of the old landslides. Many active gullies are connected to the river network, as such acting as the source of sediment. Our analysis is a step towards understanding the nature and control of anthropic activities on sediment production in the region. We also highlight the importance of considering the interactions between sediment sources and the connectivity of the geomorphological system.

Original languageEnglish
Article number274
Pages (from-to)1-28
Number of pages28
Issue number7
Publication statusPublished - 8 Jul 2022

Bibliographical note

Funding Information:
We are very grateful to VLIR-UOS for supporting the PhD scholarship of Liuelsegad Belayneh and the field research in the framework of the Inter-University Cooperation with Arba Minch University. Arba Minch University is acknowledged for its facilitation and logistic arrangement for this research work. The authors would like to acknowledge those who helped during fieldwork.

Publisher Copyright:
© 2022 by the authors.

Copyright 2022 Elsevier B.V., All rights reserved.


  • gully erosion; landslide; river incision; connectivity; knickpoint; Africa


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