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The acropolis, with its pointed arch and Cicero's tower, is located above Arpino along the path of San Benedetto

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A few kilometers from the town of Alvito, among the mountains bordering Abruzzo, there is the so-called Fossa Maiura (815 m), a karst depression that almost forms a natural amphitheater: it is a gigantic sinkhole about 100 meters deep and about 3 km in circumference, in the shape of an inverted truncated cone with a perimeter of more than a kilometer. This is where the waters that feed the Fibreno originate.

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Fossa Maiura is a chasm located near Alvito. It forms a natural amphitheater with a deep sinkhole and water springs.

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According to some, it can be placed in the middle of the Iron Age between the VIII/VII century BC. the pointed arch of the acropolis of Civitavecchia is the only survivor of its kind in the whole Mediterranean area. This is a typical shelf arch which forms a "scea" door. The whole Acropolis is beautiful, as is the view from up there.

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Acropolis of Arpino, commonly called the Acropolis of Civitavecchia, is an important site for the knowledge of the megalithic architecture of southern Lazio.

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Hidden passage in the Cyclopean walls, probably used during enemy sieges to reach the outside of the acropolis. From the place where it is located you can also enjoy a beautiful glimpse of Arpino.

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One of the best viewpoints to admire the historic center of Arpino.

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"Fossa Maiura", a gigantic chasm already mentioned in ancient times ("description of Alvito et his Contato" Prudentio 1574) in the texts of historians and naturalists, for its geological and naturalistic peculiarities. The area still remains an example of integration between human activities (agricultural and pastoral) and natural balances, despite the relentless process of land abandonment, now revealing the testimony of an almost lost era. A few kilometers from the village of Alvito, in the mountains bordering Abruzzo, there is the so-called Fossa Maiura (815 m), a karst depression that almost forms a natural amphitheater: it is a gigantic sinkhole about 100 meters deep and about 3 km in circumference, in the shape of an inverted truncated cone that has a perimeter greater than a kilometer. Here the feeding waters of the Fibreno originate. Within the territory there is a spring from which sulphurous-ferruginous water flows. This very particular karst depression with the ancient districts of Cortignale and Cappudine, now abandoned, present themselves as real ghost towns. The two villages were completely depopulated already after the war, but within the walls of the stone houses you can still understand the customs and rules of the disappeared peasant civilization.

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