Greco di Bianco
Styles
Principal grape varieties
Terroir
Natural factors
- Soils developed on Pliocene sediments resting on a Palaeozoic crystalline basement, with Miocene conglomerate outcrops.
- On the hilly terrain, sandy or conglomerate formations predominate: shallow soils with hydromorphic conditions within 50 cm of the surface.
- On fluvial terrace surfaces: medium-textured soils with a slightly acid reaction and an argillic accumulation horizon.
- Climate ranging from sub-humid to sub-arid: rainfall concentrated in autumn and winter, a marked summer moisture deficit, and peak temperatures in August.
Human factors
- Origins in the 7th century BC: the first vines arrived with landings at what is now Capo Bruzzano, the variety then known as 'aminea' (not a red grape).
- Drying (appassimento) on cane racks or in dedicated drying lofts: the grapes lose up to 35% of their weight before pressing.
Product characteristics
- Amber-yellow in appearance, with aromas of orange blossom; soft, sweet, and harmonious on the palate.
- A passito-style wine: the grapes undergo drying (appassimento) on cane racks or in dedicated drying lofts, with a weight reduction of up to 35%.
Terroir / wine link
- Pliocene sediments overlying a Palaeozoic crystalline basement, with varicoloured clays and sandy hillside soils: a pedological diversity that is reflected in the character of the wine.
Facts drawn from the cahier's terroir-link section (Lien au terroir) by automatic interpretation — see the source.
Sources
- eAmbrosia register (EU) — File number PDO-IT-A0617
- Official trade body site — Consorzio Greco di Bianco DOP