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Geologically, it is a graben, a tectonic structure formed in the mid-Pliocene/early Pleistocene (4 to 2 millions years ago). Later it was subject to large sedimentary deposition phenomena, creating an overall thickness of 600 m of sediments.
The plain is crossed by the Tirso River, the longest in Sardinia.
Agriculture has been successful in Campidano since the Neolithic, continuing on through the Punic and the Romans, who cultivated here grains and grape. Dams of the large Sardinian rivers nourish the artichoke and wheat cultures, also typical products of this zone. Paddy fields are present near Oristano.
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