During the last ice age, the land surface of Drenthe was covered with glaciers and ice, slowly moving in from Scandinavia. This shift of stone and ice resulted in the creation of the Hondsrug, an elevation at the centre of Drenthe. It gave Drenthe somewhat of a ‘upside down soup plate’-look.
During the last ice age, the land surface of Drenthe was covered with glaciers and ice, slowly moving in from Scandinavia. This shift of stone and ice resulted in the creation of the Hondsrug, an elevation at the centre of Drenthe. It gave Drenthe somewhat of a ‘upside down soup plate’-look.
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