Belonging to the hilly area of Langhe, characterized by an asymmetric profile of the slopes within an area recognized in the geological sequence oligo-Miocene. It’s Located on the right side of the Tanaro river, characterized by a succession of gullies, it belongs to the formation of marl of Sant’Agata, which is the result of the geological
phenomenon known as “Capture the Tanaro river” that occurred about 65 thousand years ago. The chalky clay interspersed with sandstones give birth here in a structured and long-lived wines.
