Aprilia
Styles
Principal grape varieties
Terroir
Natural factors
- Flatland soils: fluvio-lacustrine, aeolian, and pyroclastic sediments originating from the Monti Lepino–Ausoni during the Quaternary.
- Coastal area dominated by the 'Duna Antica': Pleistocene aeolian sands overlying organogenic calcareous sands, with a total thickness of up to ~100 m.
- Towards the interior: fluvio-palustrine deposits with alternating sandy, sandy-clayey, and travertine layers, as well as peat horizons.
- The zone falls partly within the Lazio Volcanic District, the southernmost of Lazio's volcanic districts, with pyroclastic contributions to the soils.
- Mediterranean climate: rainfall 842–996 mm/year, summer aridity (May–August), mean temperature 14.5–16.1°C, west and south aspects.
Human factors
- Pre-Roman viticulture, followed by Pontine land reclamation from Leo X (Renaissance) to Pius VI (late 18th century), completed in the 1930s.
- Around 1932, approximately 60,000 settlers from Veneto, Friuli-Venezia Giulia, and Emilia-Romagna repopulated the reclaimed Agro, establishing a viticulture tradition rooted in the Po Valley.
Terroir / wine link
- Coastal-area soils: aeolian sand dunes (Upper Pleistocene) overlying organogenic calcareous sands (Middle–Lower Pleistocene), the whole formation known as the 'Duna Antica'.
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-A0691