Fluviatile Dynamik im Mittelwesertal während des Spätglazials und Holozäns

Susanne Lipps
The investigations on Late Glacial and Holocene deposits in the middle Weser valley concentrated on high-flood sediments as well as on sedimentary and sedentary fillings of abandoned river meanders. A stratigraphy of the Late Glacial and Holocene was developped in which some events are of fundamental importance: 1. During the Late Glacial, at latest in the younger Dryas period, change from a braided to a meandering river in connection with an insignificant deepening of the...