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Soils mostly belongs to the Pliocene formation of Villamagna. Their origin is marine from the granular weathering of limestones and sands, which are intercalated with more clayey layers. This formation, widespread in the Pisan hills, finds in this area a greater limestone component In the form of rocks and gravels..
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The subsoil hides layers of an ancient seabed that has transformed into the heart of our terroir: the blue marl.
\nThe structure of the soils leads to the identification of parcels with a greater presence of clay and others with greater content of sand.
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The hill of Montefoscoli tells of an ancient rural civilization (Museum of peasant civilization of Montefoscoli). The entire area surrounding the town is divided into a multitude of estates and farms, which identify different parcels, all bordering each other. Tenuta di Montefoscoli contains six of these farms. Each of them, based on their position, is characterized by a different and original micro-terroir unit. Our goal is to understand the potential of each parcel and convey it in our wines.
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