Touring Piscinas in Italy
Piscinas in the region of Sardinia with its 886 citizens is a city located in Italy - some 280 mi or ( 450 km ) South-West of Rome , the country's capital city .
Time in Piscinas is now 12:54 PM (Tuesday) . 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, Tratalias, and Teulada. 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 Piscinas ? We have collected some references on our attractions page.
Videos
Madonna Tratalias caduta al termine della processione - Lunedì 21.05.2012
Questo video non vuol colpevolizzare gli organizzatori o altre persone, riporta solo quanto successo; un incidente che può avvenire quando c'è molta gente, che è capitato a Tratalias ma che sarebbe po ..
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 ..
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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 21 km away
Historical Weather
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.