• Copyright: Schmitz

Weinberg

Kerpen

Heute geöffnet

The vineyard consists of limestone and dolomite stone layers of the Middle Devonian period. They originated from calcareous marine deposits in the area of a reef belt. The rocks of this layer sequence consist of dickbankingen reef limestone, which are rich in fossils.


Parking possibility: 500 meters

The vineyard consists of limestone and dolomite stone layers of the Middle Devonian period. They originated from calcareous marine deposits in the area of a reef belt. The rocks of this layer sequence consist of bigreef limestones, which are rich in fossils.

Kontakt

Weinberg
Adenauer Str. 31
Kerpen

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