In the transition to the Waldviertel, the vines thrive on the acidic granite of the Moravian, which breaks down over time into quartz-rich sand. To the east, there are two basins of loose rock, separated by the Leiser Berge mountain range and the striking cliffs of the Waschberg zone of light-colored, hard limestone. The central section of the Weinviertel also includes the Flysch in the southern area, which comprises calcareous sandstones and marls on the Bisamberg and mostly acidic, quartz-rich sandstones and clays on the eastern edge of the Korneuburg Basin.
To the west of the Waschberg zone extends the molasse with sands, gravels, clayey silts and the special feature of diatomite horizons on one side, and on the other side with the broad, gravelly ridge of the Ur-Danube.
The region east of the Waschberg zone belongs to the Vienna Basin and consists mainly of loose, mostly calcareous rocks such as gravels, sands and clayey silts. Solid limestones or calcareous sandstones only occur locally in both basins. Overall, the Weinviertel is an important wine region in Austria, known for its high-quality white wines. The history of viticulture in the region, the continental climate and the favorable soil conditions help the Weinviertel wines maintain their unique taste and quality.