Explore Su de is Gattas in Italy
Su de is Gattas in the region of Sardinia is a town in Italy - some 280 mi or ( 450 km ) South-West of Rome , the country's capital city .
Current time in Su de is Gattas is now 03:33 AM (Sunday) . The local timezone is named " Europe/Rome " with a UTC offset of 1 hours. Depending on the availability of means of transportation, these more prominent locations might be interesting for you: Tunis, Kairouan, Villacidro, Tulni, and Tratalias. Since you are here already, make sure to check out Tunis . We saw some video on the web . Scroll down to see the most favourite one or select the video collection in the navigation. Where to go and what to see in Su de is Gattas ? 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 16 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 22 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.