Source: Vanmaele, Nele, 08-05-2015, ©Vlaamse Gemeenschap
Copyright: All rights reserved
The castle site is located in a sand cover area that is part of the Flemish Valley filled by Pleistocene sediments. The castle site largely coincides with a slight depression in the micro-relief, the lowest part of which is occupied by silty sandy soils. The water drainage was originally defective; the route of the Scheidbeek, which now drains the depression, shows that this stream was completely artificially constructed.
Source: Inventaris Onroerend Erfgoed
| | Public | Dutch
Zwijnaarde, Gent, Belgium
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Source: Vanmaele, Nele, 08-05-2015, ©Vlaamse Gemeenschap
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Source: Vanmaele, Nele, 08-05-2015, ©Vlaamse Gemeenschap
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