Denominación de Origen Toro. Geomorfología.


The soil is made up of sand sediment, clay and calcareous conglomerates from the Pliocene, which cause brown limestone topsoils on loose material. The materials alternate from loamy materials to large and fine grain sand, with limestone and detrytic marl formed during the Miocene.

The height above sea level of the vineyards stands between 620 m and 750 m, and the soils belong to the Tertiary Era.