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Travel guide

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The mountains, the plains,<br />

the Rivers, the Coast<br />

Sardinia is an island of the Western Mediterranean Basin, larger than<br />

Corsica and second in size only to Sicily, and surrounded by the Tyrrhenian<br />

and Sardinian Seas. Inland its territory is predominantly hilly and<br />

mountainous, with a group of massifs amongst which is the Gennargentu,<br />

peaking at Punta La Marmora. However, the average altitude of the Island<br />

is overall low. In the western part, the wide plains of the Campidani divide<br />

the inland massifs from the mountainous group of the Iglesiente and<br />

Sulcis. There are no major earthquake events with only seven in recorded<br />

history, the oldest of which was documented in Cagliari in 1616, whereas<br />

the most recent in 1948. The geological history of Sardinia began in the<br />

Cambrian. Indeed, Cambrian sandstones form the backbone of the Sulcis-<br />

Iglesiente, together with its mining fields. These sedimentary rocks are<br />

followed in the Carboniferous by volcanic ones, an indication of the<br />

mighty eruptions of those times. Later, as a result of orogenesis the Island<br />

emerged in all of its extension, was then flooded again by the sea in the<br />

Eocene, and eventually achieved its current morphology starting from the<br />

Lower Pliocene. The lithologic structure consists mainly of metamorphic<br />

rocks (gneiss, schist), which form the foundation over which rest all the<br />

other formations of the Island: volcanic rocks, both intrusive (granite) and<br />

effusive (andesite, basalt), and sedimentary rocks (limestone, sandstone),<br />

which originated as a result of flooding events. The morphology is far from<br />

being monotonous, as each geologic epoch has modelled quite different<br />

landscapes. Thus, the granitic mountains of Gallura have craggy contours<br />

and are on average low, except for Mount Limbara (reaching 1362<br />

metres), with its typical pinnacles and spikes so evocative in the Aggius<br />

chain overlooking the valley of Tempio. South of the Gallura region, the<br />

granite becomes more predominantly mountainous, with wide ridges<br />

increasing in altitude towards the peaks of Barbagia, with the tacchi and<br />

7

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