Alghero Holidays in Sardinia

Giulia Alghero Holidays in Sardinia. The actual morphology of the island is the result of the complex tectonic removals and the intrusive and effusive volcanic demonstrations verified him in the era cenozoica on a plinth of Paleozoic rocks emerged by the sea and intensely wrinkled during the orogenesi ercinica and subsequently flattened by the incessant levelling work of the agents esogenia. The Sardinian relief is constituted therefore from an irregular and chaotic succession of mountainous alignments, isolated groups, highlands and ledges, deeply notched by the erosive action and apparently prepared without order. Alghero Holidays in Sardinia. They prevail the mountainous areas, at times also steep, in the oriental band formed by schists siluriani and from vast intrusions granite masses to the open one from the erosion; they prevail the hilly areas in the western band, characterized by a various and complex geologic structure, in which the basaltic pianoris and trachitici are alternated, the sedimentary formations mioceniche, the limestones resting mesozoici on the underlying Paleozoic base, in wide part now to the open one. A characteristic element in the structural architecture of Sardinia is the presence of the tectonic pit of the Campidano, filled by deposits eocenicie pleistocenici, that crosses the southern sector of the island with direction NW-if connecting the gulf of Oristano with that of Cagliari and separating the mountainous district of the Sulcis and the Iglesiente, rich of mining layers, to SW, from her well vast mountainous region to N and to And that it interests big part of the island and that it raises him to the 1834 ms of the Point the Marmora in the group of the Gennargentu. The coasts (1849 km, included the smaller islands), if the lines are excluded in correspondence of the coastal lowlands, they are tall and often steep and picturesque. The climate is type Mediterranean, with long, dry and warm summers but you ventilate and brief winters, rainy and you don't cool, to exception of the most elevated areas. The annual middle temperatures oscillate among the 18 long ºCs the coastal bands and the 14 ºCs of the inside, still going down however to values more lower part, up to 12 ºCs, in the mountainous region of the Gennargentu. The precipitations are assembled in wide measure in the winter months and they are distributed in rather irregular way in consequence of the morphological splitting up of the island: in the most elevated areas they reach the 1300 annual mms, but in the Campidano, in the Gallura and in wide coastal bands they don't overcome the 600 mms.

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