>
A new subdivision of crystalline Fennoscandian erratic pebble assemblages (Saalian) in the central Netherlands in Special issue in the honour of J. D. De Jong.
(supprimer)
The inland-ice cap in the Saalian in the central part of the Netherlands caused the formation of glacial basins and ice-pushed ridges and the deposition of till as well as glaciofluvial and glaciocustrine material (Drente Formation). Crystalline