Frost-mound scars and the evolution of a Late Dryas environment (northern Netherlands)
article
Small oval to round depressions in Weichselian deposits near Scheemda were formed in Late Dryas time. Lithology, sedimentology, and stratigraphic position indicate that these depressions were produced by seasonal frost action followed by thermokarst solution. -from Authors
TNO Identifier
230449
Source
Geologie en Mijnbouw, 66(3), pp. 239-250.
Pages
239-250