Colline Lucchesi

Styles

Principal grape varieties

Terroir

• Soils derive from two Tuscan geological formations: calcareous alberese marl and Tuscan macigno sandstone, of Paleocene and Miocene origin.
• Calcareous clayey marls promote body and longevity; Tuscan macigno, rich in minerals, contributes aging potential.
• The Serchio river divides two slopes: the western one (Valfreddana), suited to whites, and the eastern one, suited to reds.
• The plain of Lucca is humid and prone to frost; the steep hillsides protect the vineyards, which are situated mostly at mid-slope with full sun exposure.

• Documents predating the year 1000 attest to vineyards 'in the ninth century' on the hills north of Lucca; in 1334 more than 168,000 barrels were exported.
• The presence of complementary grape varieties is historically established to ensure consistent quality between Apennine and Mediterranean influences.

• Calcareous alberese marl yields wines of body and longevity; Tuscan macigno sandstone imparts aging potential thanks to its richness in minerals.
• Excellent development of color and tannins is achieved through Apennine diurnal temperature variation and the intense light of the Tyrrhenian coast, resulting in softness and intensity.

• Calcareous marls yield body and longevity; Tuscan macigno, rich in minerals, contributes aging potential.

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-A1387