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ATELIER DEVINO
Home
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Wine Region Of The Month
Wine events around Sydney
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Home
Store
About
Wine Region Of The Month
Wine events around Sydney
Wine List Creation
Store 2018 Marchesi Di Barolo LINEA CRU STORICI Barolo Cannubi DOCG - Piemonte
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2018 Marchesi Di Barolo LINEA CRU STORICI Barolo Cannubi DOCG - Piemonte

A$231.00

Cannubi is the long, gradually rising hill in the centre of the Barolo area. Here, Serravallian and Tortonian soils meet and merge, creating bluish-gray marls rich in magnesium and manganese carbonates that take on a whitish-gray hue at the surface due to weathering: clays mixed with very fine sands, impregnated with a strong limestone content composed of magnesium and manganese carbonates. Their technical name is “Sant’Agata fossil marls”, but they are commonly called Toû and on average they comprise clays (55%), sands (30%) and limestone (15%). Surrounded by higher hills that protect it from bad weather and excessive flow of air, Cannubi enjoys a very special, unique microclimate.

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Cannubi is the long, gradually rising hill in the centre of the Barolo area. Here, Serravallian and Tortonian soils meet and merge, creating bluish-gray marls rich in magnesium and manganese carbonates that take on a whitish-gray hue at the surface due to weathering: clays mixed with very fine sands, impregnated with a strong limestone content composed of magnesium and manganese carbonates. Their technical name is “Sant’Agata fossil marls”, but they are commonly called Toû and on average they comprise clays (55%), sands (30%) and limestone (15%). Surrounded by higher hills that protect it from bad weather and excessive flow of air, Cannubi enjoys a very special, unique microclimate.

Cannubi is the long, gradually rising hill in the centre of the Barolo area. Here, Serravallian and Tortonian soils meet and merge, creating bluish-gray marls rich in magnesium and manganese carbonates that take on a whitish-gray hue at the surface due to weathering: clays mixed with very fine sands, impregnated with a strong limestone content composed of magnesium and manganese carbonates. Their technical name is “Sant’Agata fossil marls”, but they are commonly called Toû and on average they comprise clays (55%), sands (30%) and limestone (15%). Surrounded by higher hills that protect it from bad weather and excessive flow of air, Cannubi enjoys a very special, unique microclimate.

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