Explore Genniomus in Italy
Genniomus in the region of Sardinia is a place in Italy - some 278 mi or ( 448 km ) South-West of Rome , the country's capital city .
Time in Genniomus is now 07:06 PM (Saturday) . The local timezone is named " Europe/Rome " with a UTC offset of 1 hours. Depending on your budget, these more prominent locations might be interesting for you: Tunis, Kairouan, Villacidro, Tulni, and Teulada. Since you are here already, consider visiting Tunis . We saw some hobby film on the internet . Scroll down to see the most favourite one or select the video collection in the navigation. Where to go and what to see in Genniomus ? 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 ..
Mistral force 9 at South-Sardinia
A strong Mistral hit Sardinians south coast on march 2006 ..
TEULADA Pescaturismo 'Lucia Madre'
Navigare con la Lucia Madre sulle acque limpide e cristalline della Sardegna fino a raggiungere la punta 'Capo Teulada' (estremo sud dell'isola)è un viaggio alla scoperta del vero mare!!ESCURSIONI GIO ..
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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 14 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 19 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.