Abstract
Permafrost was present throughout the Netherlands during the Late Pleniglacial. Evidence of
this permafrost consists of several periglacial features of which pingo remnants are the most
prominent. Permafrost distribution, minimum depth and characteristics of decay of permafrost
throughout the Netherlands during the Weichselian Late Pleniglacial and the following
Weichselian Late-glacial was reconstructed by information
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