Waarnemingen over de beweging van het landijs in Overijssel
Grondboor & Hamer , Volume 26 - Issue 6 p. 175- 181
The plucking of material from the subsoil by the ice sheet in the eastern Netherlands has been very dissimilar. Dependent on the character of the subsoil, but also, to a larger extent dependent on the movement of the ice sheet. Large floes were transported and deposited again undisturbed. Not far from these places, however, a very homogeneous mixing of the materials occurs. The local very great differences in thickness of the ground moraine remain remarkable.
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