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Buried and forgotten—The non‐fluvial characteristics of postglacial rivers
River Research and Applications ( IF 1.7 ) Pub Date : 2020-02-26 , DOI: 10.1002/rra.3596
Christoph Hauer 1 , Ulrich Pulg 2
Affiliation  

“The systematic analysis and understanding of channel‐forming processes of rivers must be expanded by including semi‐ and non‐fluvial geomorphological processes. Such processes were particularly driven by glaciation during the Pleistocene and led to diamictic non‐fluvial deposits in the post‐glacial valleys. In the Holocene, rivers either covered these deposits with fluvial sediments or incised into them and exposed the non‐fluvial deposits. These processes have strong and so far overlooked implications for the understanding of the genesis, morphology and sediment composition of many rivers – and thus for river utilization, ecology, restoration and management.”

中文翻译:

被遗忘和遗忘—冰川后河流的非河流特征

“必须通过包括半河流和非河流地貌过程来扩展对河道形成过程的系统分析和理解。这些过程尤其受更新世时期的冰川作用驱动,并导致冰川后谷地的非河流沉积物迅速形成。在全新世,河流要么用河流沉积物覆盖这些沉积物,要么切入其中,然后露出非河流沉积物。这些过程对于理解许多河流的成因,形态和沉积物成分,以及因此对河流的利用,生态,恢复和管理,都具有强烈的,至今被忽视的影响。”
更新日期:2020-02-26
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