Frisian Islands - Origins

Origins

During the last ice age, which ended approximately 12,000 years ago, the sea level was about 60 meters lower and what is now the North Sea was dry land. With the melting of the ice caps, the level rose to form the North Sea, reaching the current coast line around the beginning of the Holocene era, approximately 7000 years ago. Tidal action transported large quantities of sand to form a line of dunes extending over 500 km from contemporary Belgium through the Netherlands to the mouth of the river Elbe in Germany. The sea broke through the dunes in many places to form the Wadden Islands, with the low-lying country behind becoming the tidal Wadden mudflats.

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