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Photographer’s Note

The whole dune range starts in Halsteren (Holland) and stretches into the Kalmthoutse Heide in Flanders over a total of 25 kilometres. In Holland it is also called Brabantse Wal (Brabant Wall) but it is often forgotten that part of this ‘geological wonder’ lies in Flanders.
It is located on the border of the lower sea clay area of Zeeland and the higher sandy grounds of the Kempen.
The steering forces behind the origin of the Brabantse Wal are dual. Firstly the tilting movements of the Belgian-Dutch soil play an important role. The massif of Brabant was lifted and parts of Noord-Brabant and Midden-Nederland dropped. This is the reason why south of Bergen op Zoom sediment from the Ice Age can be found close to the surface. This sediment of clay and sand is the foundation for the Brabantse Wal. Near Ossendrecht the layer is about 30-40 metres thick. The clay banks that originated this way are called Kempisch Klei. And because of the presence of this clay, the Northern course of the river Scheldt could not touch the Brabantse Wal, and the actual steep slopes came into existence. During the last Ice Age the Brabantse Wal was covered with wind-borne sand deposit, which gave it its actual shape.



here you can find this good note.

Realy I love that place it is a dream for a photographer. This one I took in november. it was a fantastic day and the sun was shining through the trees and gives this fantastic effec, i hope you like it too,
gr. jaap

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Additional Photos by jaap polak (carper) Gold Star Critiquer/Gold Star Workshop Editor/Gold Note Writer [C: 9664 W: 426 N: 18435] (65696)
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