map of cyprus

map of cyprus, the island of cyprus

Volcanic atoll in the Mediterranean

Photo of a small volcano in the western Mediterranean sea. Standing on the very edge of the continental self its crystaline waters are full of life.

need opinion? mediterrenean look

here is one of our design. we are building 3 designs for a single subdivision here in the philippines. I just would like to know your opinion whether this design would fit a modern mediterranean village. Any comment will be appreciated. Color, ove all look, theme, accents..thnx

A point between Minorca and Barcelona.

The geology of the Mediterranean is complex, involving the break-up and then collision of the African and Eurasian plates and the Messinian Salinity Crisis in the late Miocene when the Mediterranean dried up. The Mediterranean Sea has an average depth of 1,500 metres (4,920 ft) and the deepest recorded point is 5,267 meters (about 3.27 miles) in the Calypso Deep in the Ionian Sea. The coastline extends for 46,000 kilometres (28,600 mi). A shallow submarine ridge (the Strait of Sicily) between the island of Sicily and the coast of Tunisia divides the sea in two main subregions (which in turn are divided into subdivisions), the Western Mediterranean and the Eastern Mediterranean. The Western Mediterranean covers an area of about 0.85 million km² (0.33 million sq mi) and the Eastern Mediterranean about 1.65 million km² (0.64 million sq mi). Geodynamic The geodynamic evolution of the Mediterranean Sea was provided by the convergence of European and African plates. This process was driven by the differential spreading along the Atlantic ridge, which led to the closure of the Tethys Ocean and eventually to the Alpine orogenesis. However, the Mediterranean also hosts wide extensional basins and migrating tectonic arcs, in response to its land-locked configuration. Eastern Mediterranean In middle Miocene times, the collision between the Arabian microplate and Eurasia led to the separation between the Tethys and the Indian Oceans. This process determined profound changes in the oceanic circulation patterns, which shifted global climates towards colder conditions. The Hellenic Arc, which has a land-locked configuration, underwent a widespread extension for the last 20 Myr due to a slab roll-back process. In addition, the Hellenic Arc experienced a rapid rotation phase during the Pleistocene, with a counterclockwise component in its eastern portion and a clockwise trend in the western segment. Central Mediterranean The opening of small oceanic basins of the central Mediterranean follows a trench migration and back-arc opening process that occurred during the last 30 Myr. This phase was characterized by the counterclockwise rotation of the Corsica-Sardinia block, which lasted until the Langhian (ca.16 Ma), and was in turn followed by a slab detachment along the northern African margin. Subsequently, a shift of this active extentional deformation led to the opening of the Tyrrenian basin. Western Mediterranean Since Mesozoic to Tertiary times, during convergence between Africa and Iberia, it developed the Betic-Rif mountain belts. Tectonic models for its evolution include: rapid motion of Alboran microplate, subduction zone and radial extentional collapse caused by convective removal of lithosferic mantle. The development of these intramontane Betic and Rif basins led to the onset of two marine gateways which were progressively closed during the late Miocene by an interplay of tectonic and glacio-eustatic processes.

Mediterranean

Cool Sunset in mediterranean

Pizza

A pizza.

Cyprus

At Petra tou Romiou, the birthplace of Aphrodite, in Cyprus

Mediterranean Meal

Mediterranean foods are very health.

Oil An Olive

Mediterranean Diet