Planting layout 75/230
The vineyard extends over a linear slope with a modest slope, facing northwest, consisting of marine poligenic conglomerates from the Pliocene era (3-5 million years) at an average altitude of 515 meters. The reddish soils are moderately deep, rich in pebbles and weathered skeleton, predominantly sandy loamy clay texture, non-calcareous, acidic pH, well-structured, well-drained, with moderate water reserves.
Planting layout 120/300 spurred cordon
The vineyard extends over a plateau on the slope formed by marine poligenic conglomerates from the Pliocene era (3-5 million years) at an average altitude of 507 meters. The brown-colored soils are generally deep, with frequent skeleton consisting of well-altered pebbles, predominantly sandy loamy clay texture, non-calcareous, acidic pH, well-structured, well-drained, with high water reserves.
Planting layout 125/290 spurred cordon
The vineyard extends over a convex slope, with a gentle slope, facing west at an average altitude of 500 meters. Geologically, the area is characterized by the presence of the Sillano-Santa Fiora Formation of the Upper Cretaceous-Paleocene period (60-75 million years), consisting of clayey, marly limestone, silty, and calcilutite (carbonate granules the size of clay and silt). The soils are deep, with a useful depth of about 120 cm, with frequent skeleton consisting mainly of fragments of marly limestone and silt, predominantly loamy clay texture, moderately calcareous, subalkaline pH, well-structured, well-drained, with high water reserves.
Planting layout 100/290 spurred cordon
The vineyard extends over a convex slope, with a moderate slope, facing South, Southwest at an average altitude of 495 meters. Geologically, the area is characterized by the presence of the Sillano-Santa Fiora Formation of the Upper Cretaceous-Paleocene period (60-75 million years), consisting of clayey, marly limestone, silty, and calcilutite (carbonate granules the size of clay and silt), and occasionally calcarenite. The soils are moderately deep, with a useful depth of about 100-110 cm, with frequent skeleton consisting mainly of fragments of marly limestone and silt, predominantly loamy clay texture, slightly calcareous, subalkaline pH, moderately structured.
