Dithmarschen - Geography

Geography

The district is located on the North Sea. It is embraced by the Elbe estuary to the south and the Eider estuary to the north. Today it forms a kind of artificial island, surrounded by the Eider river in the north and the Kiel Canal in both the east and southeast. It is a rather flat countryside that was once full of fens and swamps.

To the north it borders on Nordfriesland and Schleswig-Flensburg, to the east on Rendsburg-Eckernförde, and in the southeast on Steinburg. Its landward boundaries have remained basically the same since the times of Charlemagne. Land reclamation, however, has almost doubled the size of Dithmarschen as land has been wrested from the sea.

Important towns are Hamburg and Itzehoe to the south, Husum to the north, and Kiel and Rendsburg to the east. The main roads and rail lines in Schleswig-Holstein follow a north-south direction, making Hamburg its most accessible city.

The district has a maximum north-south length of 54 kilometers and an east-west length of 41 kilometers. The highest point, near Schrum in the Geestland, is 78 meters above sea level and the lowest point, near Burg, is 0.5 meters below sea level.

Dithmarschen's landscape owes its character to the North Sea. From west to east Dithmarschen consists of the Wadden Sea, marsh, bog, and the Geestland. The North Sea had a higher sea level 6,500 years ago than today and the coastline then ran along the Geestland. About 4,500 years ago, Geestland structures were connected by sand and gravel depositions that formed spits. Bogs, lakes, and swamps emerged as the area behind the spits no longer flooded. After the first plants (glasswort) took root, the land transformed first to salt marshes and finally to marshes. These marshes rank among the most fertile of Germany's soils. Vegetable farming in Dithmarschen produces the highest yields in Schleswig-Holstein.

Since about the 8th century, the people of Dithmarschen have been living on warfts for protection from the sea. In the 12th century, they began building dikes to protect their pastures and fields. Since about the 15th century, they have been reclaiming land from the sea.