Campi Flegrei
Styles
Principal grape varieties
Terroir
Natural factors
- Soils of volcanic origin rich in ash, lapilli, pumice, and tufo, derived from more than 60 eruptive centers active over the last 39,000 years.
- Caldera structure formed by the superimposition of two collapse events linked to the Campanian Ignimbrite and the Campanian Yellow Tufo.
- Bradyseismic phenomena accelerated the fragmentation of the Campi Flegrei area from the sixth century onward.
- Volcanic soils of a texture that has historically prevented the spread of phylloxera: some vines still grow on their own rootstocks.
- The orography and aspect of the vineyards ensure an adequately ventilated and sun-exposed environment, favorable to vegetative and productive functions.
Human factors
- Falanghina: the name is thought to derive from 'falanga,' the local wooden stake; vines are still trained by long layering using the 'metodo Puteolano,' with century-old plants. (via Wikipedia · CC BY-SA 4.0)
Product characteristics
- Unique aromas and flavors attributed to the volcanic soil: ash, lapilli, pumice, and tufo impart organoleptic characteristics that cannot be replicated elsewhere.
- On the nose and palate, the aromas typical of indigenous varieties dominate, with balanced physico-chemical characteristics across all wine types.
Terroir / wine link
- Volcanic soils (ash, lapilli, pumice, tufo) give rise to unique aromas and flavors in the grapes and wines of the Campi Flegrei.
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-A0239
- Official trade body site — Consorzio Tutela Vini Campi Flegrei e Ischia