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3.2.1. The Rozebeke Formation - Rb


Authors: Tavernier & De Moor, 1974.

Description: Clayey-sandy rich gravel, preserved at the highest terrace level (at about 80 to 90m above the present main river in the reference area). The gravel is composed of rounded flint, often superficially weathered. Locally with flint fragments. Involutions are present at the base.

Stratotype: Road incision Rozebeke.

Area: Schelde basin.

Thickness: 1 to 2m.

Age: Pliocene to Lower Pleistocene.