Last edited by Nikozragore
Monday, August 3, 2020 | History

2 edition of Glacifluvial estuaries on the Narke Plain. found in the catalog.

Glacifluvial estuaries on the Narke Plain.

Arvid Bergdahl

Glacifluvial estuaries on the Narke Plain.

by Arvid Bergdahl

  • 60 Want to read
  • 11 Currently reading

Published by Gleerup in Lund .
Written in English


Edition Notes

SeriesLund studies in geography -- no.13
ID Numbers
Open LibraryOL20890721M

A small hill, knob, or mound of glaciofluvial sorted sand and gravel that forms on the surface of a glacier and is later left on the left surface after the glacier retreats is a(n)-drumlin.-till plain.-kame.-kettle.-esker. The book discusses the background to this issue and the measures to be taken over the next years to overcome some of the difficulties that can be foreseen, and the means of avoiding others.

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Glacifluvial estuaries on the Narke Plain by Arvid Bergdahl Download PDF EPUB FB2

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Additional Physical Format: Online version: Bergdahl, Arvid. Glacifluvial estuaries on th Närke Plain. Lund: Royal University of Lund, Dept. of Geography,   Fluvial processes include the motion of sediment and erosion or deposition on the river bed.

Erosion by moving water can happen in two ways. Firstly, the movement of water across the stream bed exerts a shear stress directly onto the bed. If the cohesive strength of the substrate is lower than the shear exerted, or the bed is composed of loose sediment which can be mobilized by such stresses.

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