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Sallandse Heuvelrug National Park

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  • 5 chapters

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Through Glacial period, Holocene and World War II

The National Park is located in its entirety south of the N35 (Zwolle-Almelo), and encapsulates Haarlerberg, Holterberg, Noetselerberg and Koningsbelten. The park covers an area of approximately 35 square kilometres. Its highest point is the Koningsbelt, standing 75 metres above Normaal Amsterdams Peil (NAP).

Landscape and history

The Sallandse heuvelrug is a moraine, created in the second-last glaciation, Saalien, 150,000 years ago. During the Holocene forests started to develop, but after the growth of the human population, these forests had been cut. From the Middle Ages onwards the area was used for grazing by sheep and goats, and the upper layer of the soil was removed to use it as fertilizer for the crop fields. In this period, the area became a heathland because of sand-drifting. In the beginning of the 20th century the state started forestry programs, to prevent this erosion and to produce pine wood. The area is well known for its scenery because of its relatively large heathlands.

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