Discover Santadi in Italy
Santadi in the region of Sardinia with its 3,767 habitants is a town located in Italy - some 277 mi or ( 446 km ) South-West of Rome , the country's capital .
Local time in Santadi is now 03:44 PM (Saturday) . The local timezone is named " Europe/Rome " with a UTC offset of 1 hours. Depending on your flexibility, these larger cities might be interesting for you: Tunis, Kairouan, Villacidro, Tulni, and Tratalias. When in this area, you might want to check out Tunis . We found some clip posted online . Scroll down to see the most favourite one or select the video collection in the navigation. Are you looking for some initial hints on what might be interesting in Santadi ? We have collected some references on our attractions page.
Videos
CASA TEULADA - luxury retreat
CASA TEULADA is a stunning example of an incredible renovation work. Based on the ruins of a typical 19th century rural sardinian country house, CASA TEULADA has been painstakingly restored to a state ..
quanto è bella cagliari
una vista su cagliari e il poetto ..
CASA TEULADA 2 - short preview
a short video broadcasting outstanding rental property CASA TEULADA 2 - www.casateulada.com - located in pristine southwestern Sardinia, Italy ..
The making of CASA TEULADA 2
a short video broadcasting renovation for outstanding rental property CASA TEULADA 2, located in pristine southwestern ..
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Interesting facts about this location
Sulcis Mountains
The Sulcis Mountains (Italian: Monti del Sulcis) is a mountain chain in Sardinia, Italy. Together with the Monte Linas massif, from which they are separated by the flood plain of the Cixerri River, they form the Sulcis-Iglesiente Mountains, one of the most ancient geological formations in the island.
Located at 39.15 8.83 (Lat./Long.); Less than 11 km away
Monte Arcosu
Monte Arcosu is a mountain in the Sulcis massif, in southern Sardinia, Italy. It has an elevation of 948 metres . The mountain has a characteristically truncated cone shape, resulting from the differential erosion which followed its formation during the Variscan orogeny. The massif is formed by a granitic intrusion from the Carboniferous, lying on a Paleozoic schist basement and in turn surmounted by Paleozoic scists.
Located at 39.19 8.86 (Lat./Long.); Less than 17 km away
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Information of geographic nature is based on public data provided by geonames.org, CIA world facts book, Unesco, DBpedia and wikipedia. Weather is based on NOAA GFS.