The Great Vineyards - ArnaldoRivera
17107
page-template,page-template-full_width,page-template-full_width-php,page,page-id-17107,qode-quick-links-1.0,ajax_fade,page_not_loaded,,qode_grid_1300,qode-child-theme-ver-1.0.0,qode-theme-ver-11.0,qode-theme-bridge,wpb-js-composer js-comp-ver-6.2.0,vc_responsive

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…

RAVERA – Novello

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…

ROCCHE DELL’ANNUNZIATA AND BOIOLO – La Morra

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…

CASTELLO – Grinzane Cavour

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.

BUSSIA – Monforte 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…

VILLERO – Castiglione Falletto

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…

CANNUBI – Barolo

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…

VIGNARIONDA – Serralunga d’Alba

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…

ROCCHE DI CASTIGLIONE – Castiglione Falletto

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…