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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 />
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