The Great Vineyards

MONVIGLIERO – Verduno

Geological substrate: LAMINATED SANT’AGATA FOSSIL MARL; 8 million years old (TORTONIAN STAGE).

The vineyard extends entirely over Sant’Agata Fossil Marl in its particular “laminated” form…

Geological substrate: SANT’AGATA FOSSIL MARL; 9 million years old (TORTONIAN STAGE).

The vineyard is situated at the heart of the Sant’Agata Marl geological formation, which differs considerably here to its typical form…

Geological substrate: LAMINATED SANT’AGATA FOSSIL MARL in transition to SANDY SANT’AGATA FOSSIL MARL; 8 million years old (TORTONIAN STAGE).

The vineyards that produce this cru are located in the upper and intermediate parts of the…

Geological substrate: SANT’AGATA FOSSIL MARL; 10 million years old (TORTONIAN STAGE).

Here we find ourselves in the central area of Sant’Agata Marl, within the outcrop of the Marl of Gallo d’Alba.

Geological substrate: SANT’AGATA FOSSIL MARL in transition to DIANO SANDSTONE; 9 million years old (TORTONIAN STAGE).

The Bussia cru is one of the most extensive in the Barolo growing area, approaching 300 hectares…

Geological substrate: SANDY SANT’AGATA FOSSILI MARL; 9 million years old (TORTONIAN).

The vineyards are located on the mainly south-westerly facing part of the cru…

Geological substrate: SANDY SANT’AGATA FOSSILI MARL; 9 million years old (TORTONIAN).

The vineyard is located at the top of the ridge that separates the Cannubi and Albarella crus…

Geological substrate: LEQUIO FORMATION; 12 million years old (SERRAVALLIAN STAGE).

The vineyard extends over the Lequio formation, the oldest in the whole of the Barolo growing area…

Geological substrate: DIANO SANDSTONE in transition to SANT’AGATA FOSSIL MARL; 9 million years old (TORTONIAN STAGE).

The vineyard stands on the area of contact between two geological formations, Diano Sandstone and Sant’Agata Fossil Marl…