Pentro di Isernia

Styles

Principal grape varieties

Terroir

• Dominant substrate: Paleogene marnoso-calcaree formations and Miocene arenaceo-marnose formations, with outcroppings of tectonically derived "Argille Varicolori".
• Predominantly mountainous territory (55.3%) with slopes subject to calanchi erosion; mean annual temperature between 13.5 and 14.8 °C.

• A substrate of Paleogene calcareous marne and Miocene marnose arenarie characterizes the vineyards of Pentro di Isernia.

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-A0684