The Terrace Moselle and how it all began
The terraces tower impressively between the slate rocks. Our vines grow here under special conditions: we grow wine on extremely steep slopes.
400 million years ago, in a distant chapter of the Earth's history, the Devonian period, there was a primeval ocean in the area of today's Mosel. Thick layers of sediment formed in it, several kilometers high. The primeval ocean was pushed together between the continental plates and the seabed was compressed under enormous pressure and high temperatures. The sediments turned into slate, which eventually folded into a mountain range. When the primeval continents of Gondwana and Laurussia collided, the foundations of today's soil formations were created.
The first written evidence of winegrowing in Winningen can be found in a document from the year 871. Little by little, the vineyards expanded into the extremely steep slopes, which were formed into our unique cultural landscape by the manual construction of terraces and thus became usable for winegrowing.
¹ Karl J. Gilles (1999) - Bacchus and Sucellus. Rhein-Mosel-Verlag