Das Mündungsgebiet der Ahr im Spät-Würm und Holozän

The area of the Ahr ri ver mouth during the late Würm and Holocene.Proceeding from the recent morphodynamics in the area of the Ahr river mouth and the geomorphological-sedimentological investigation of the older lower terrace and the younger lower terrace of the Rhine and Ahr rivers it can be established that the transition from periglacial to Holocene processes of river dynamics and the change in the rivers' outlines already occurred in the early Bölling period.Lesser "periglacial" conditions returned briefly during the Younger Dryas period.The most recent development of the mouth of the Ahr during the Holocene shows in model fashion the changes from a straight-flowing to a braided river

Geological formations and processes · Geology · Geology and Paleoclimatology Research · Hydrology and Sediment Transport Processes

• Influence of late glacial climate changes on sediment transport in the River Werra (Thuringia, Germany)

  Open Access•Roland Mäusbacher, Heike Schneider et al.•Quaternary International•2001

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