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最終更新日: 6月 22, 2026
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Nice to walk through with water on both sides.
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The name "Koolputten" would refer to the former unloading place for coal that was located here in the vicinity of the current Durme bridge. This iron bridge was preceded by a wooden bridge, built in 1826 to replace the old ferry or Hammeveer between Sombeke and Hamme. In this area on the Durme there was also a small eel quay or beer quay known as " 't Kaaiken".
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When you leave the information center, keep the lake on your right. The route past the chapel is not worth it unless you like residential areas. Once you reach the green area towards the duck decoy, the walk becomes really beautiful. At the campsite on the other side of the lake it is best to turn around and walk back. As you continue, you walk along the busy road surrounding the lake. Only the green side of the lake is worth it.
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The Mira Bridge is a bridge over the Durme, on the border of the Belgian municipalities of Hamme and Waasmunster. It was built in the period 1896-1900. The bridge got its name and fame thanks to the feature film Mira, the 1971 film adaptation of the book De teleurgang van de Waterhoek by Stijn Streuvels by Fons Rademakers, with Willeke van Ammelrooy and Jan Decleir in the leading roles. The script was by Hugo Claus. The bridge that Streuvels described was not between Hamme and Waasmunster, but was the Vierendeel Bridge that connected Ruien with Avelgem. However, it was dynamited and replaced twice. The current bridge is a much more modern version of the original. At the beginning of the First World War, the middle section of the bridge was blown up by the local population, in an attempt to stop the Germans and their war material. (Wikipedia)
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During the end of the last ice age, the Scheldt between Ghent and Dendermonde left behind various fossil meander bends, such as those of Overmere-Donk and the Dam valley in Laarne. About 10,000 years ago, the Overmere meander was cut off. It took thousands of years for the meander to be completely filled by silting processes, after which peat formation took place. The thick layer of peat remained virtually untouched until the second half of the 17th century. Only then did peat begin to be extracted. As part of this peat extraction, the eastern part of the old Scheldt meander was excavated again, transforming the area into a large water surface. It was only finally drained at the beginning of the last century. The vacated land was planted with willows for basket weaving. After the Second World War, poplars were planted for the production of matches. Today, these poplars are gradually being replaced by native tree and shrub species as part of current forest management.
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