Dolcetto d'Alba
Styles
Principal grape varieties
Terroir
Natural factors
- The production area extends over 35 communes around Alba, and the vine-clad hills, especially those of Miocene origin on the right bank of the Tanaro river, have grown Dolcetto vines for centuries.
- The hills of the Langhe have their geological origin in the Tertiary or Cenozoic Era, which began nearly 70 million years ago.
- The high hills overlooking the Tanaro river are characterized by white tufaceous marl in the production area.
- The soil is largely made up of the geological formation known as Tortonian soil, one of the 14 sedimentary layers of the Tertiary basin of Piedmont.
- Tortonian soil is characterized by layered, weakly resistant, grey-bluish marls and sands, which form low, rounded, whitish hills favourable to vine-growing.
Human factors
- Dolcetto d'Alba wine was granted DOC status in 1974, after the variety had for centuries been a mainstay of Piedmontese rural life and a trading commodity with Liguria. (via Wikipedia · CC BY-SA 4.0)
Product characteristics
- The wine has a ruby red colour of variable intensity depending on the soil type, with deep, very pronounced violet highlights.
- The nose is vinous and fragrant with fruity notes in which cherry and plum can be recognized, while the palate is dry, with modest acidity and a delicate bitter note.
Terroir / wine link
- In the soils of the Langhe, Dolcetto finds its ideal habitat, and the clayey marls give a fresh, elegant wine.
Facts drawn from the specification's terroir-link section by automatic interpretation — see the source.
About this boundary
Area: the official production zone published by the regional geoportal (Piemonte).
Sources
- eAmbrosia register (EU) — File number PDO-IT-A1142
- Official trade body site — Consorzio di Tutela Barolo Barbaresco Alba Langhe e Dogliani