Cala Domestica - 4 Things to Know Before Visiting

Pan di Zucchero, original name in Sardinian Concali su Terràinu, is a stack that rises from the sea a short distance from the coast, near Masua, a hamlet of Iglesias, in the south-west of Sardinia. It has an area of ​​0.03 km² and a height of 133 meters. It is composed of Cambric limestone and originated from the action of marine erosion which determined its isolation from the mainland. On the rocky coast, a few hundred meters to the east is the mouth of the fascinating Porto Flavia mining site

Porto Flavia is a service infrastructure of the mining area of Masua, no longer operational, located in the south-western area of Sardinia and falls administratively in the municipality of Iglesias, Province of South Sardinia, in what is now the seaside resort of Masua. Although it was a mining site, it was not a mine, but a port of embarkation for the material extracted from the nearby mines. It was designed by the Venetian engineer Cesare Vecelli and built-in 1924; it was named after the elde

The Temple of Antas is an ancient Punico-Roman temple in the commune of Fluminimaggiore in southern Sardinia. One of Sardinia's most important monuments dating back the Roman period is located in a lush valley in the Iglesias area, a site that emerged as a Nuragic sanctuary, also used in the Carthaginian and Punic-Hellenistic era.

Piscinas is an Italian town of 823 inhabitants in the province of Southern Sardinia, in the Sulcis-Iglesiente region. Human settlements in the territory are witnessed since the Neolithic ( VII - VI millennium BC ). There are also traces of the subsequent Nuragic, Phoenician - Punic, and Roman civilizations. |One of the iconic area which shows light to the ancient life.

The Campidano is the largest plains of Sardinia, located in the southwestern portion of the island, approximately between 40 ° and 39 ° of latitude north and 8 ° 30 'and 9 ° of longitude east. From a geological point of view, it is a rift valley composed of a system of extending faults that have caused the sinking of a part of the earth's crust.

The Sinis is a peninsula of the Sardinian west-central located between the Bay of Is Arenas in the north, and the Gulf of Oristano in the south. In the sea to the west of the peninsula is the island of Mal di Ventre and the Scoglio del Catalano. The coast is rocky in the southern part around San Giovanni di Sinis, proceeding northwards it first becomes sandy then, proceeding further north, it is characterized by high cliffs up to Capo Mannu.