Source: Pascal Brackman
In questa parte del sentiero sembra che sia stata pavimentata. Ma sono le banche di arenaria che emergono in superficie qui. La strada si incide letteralmente in quelle banche di arenaria, ma poiché sono abbastanza resistenti, formano piccoli gradini. Queste banche di arenaria sono una pietra naturale locale che si forma negli strati sabbiosi della sabbia busseliana o Formazione di Bruxelles. Questo strato di sabbia è stato depositato qui in un mare poco profondo durante il terziario.
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Source: Pascal Brackman
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Source: Pascal Brackman
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