Touring Santadi Basso in Italy
Santadi Basso in the region of Sardinia is a city located in Italy - some 277 mi or ( 446 km ) South-West of Rome , the country's capital city .
Time in Santadi Basso is now 08:40 AM (Sunday) . The local timezone is named " Europe/Rome " with a UTC offset of 1 hours. Depending on your travel resources, these more prominent places might be interesting for you: Tunis, Kairouan, Villacidro, Tulni, and Tratalias. Being here already, consider visiting Tunis . We collected some hobby film on the internet . Scroll down to see the most favourite one or select the video collection in the navigation. Check out our recommendations for Santadi Basso ? 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 12 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
Related Locations
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.