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The Adriatic Sea (/ ˌ eɪ d r i ˈ æ t ɪ k /) is a body of water separating the Italian Peninsula from the Balkan Peninsula.The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po Valley.
The Adriatic Abyssal Plain, more commonly referred to as the Adriatic Basin, is an oceanic basin under the Adriatic Sea. The Adriatic Sea's average depth is 252.5 metres (828 ft), and its maximum depth is 1,233 metres (4,045 ft); however, the North Adriatic basin rarely exceeds a depth of 100 metres (330 ft).
Main European drainage divides (red lines) separating catchments (green regions). The main European watershed is the drainage divide ("watershed") which separates the basins of the rivers that empty into the Atlantic Ocean, the North Sea and the Baltic Sea from those that feed the Mediterranean Sea, the Adriatic Sea and the Black Sea.
The Venetian Lagoon (Italian: Laguna di Venezia; Venetian: Łaguna de Venesia) is an enclosed bay of the Adriatic Sea, in northern Italy, in which the city of Venice is situated. Its name in the Italian and Venetian languages , Laguna Veneta (cognate of Latin lacus ' lake ' ), has provided the English name for an enclosed, shallow embayment of ...
The opening of backarc basins like the Thyrrenian Sea caused the Calabro-Peloritan block to be separated from Sardinia, moving further south-east and finally included in the southern apenninic arc. Uplift continues today and since the Pleistocene, Calabrian sedimentary rocks have uplifted more than one kilometre (0.62 mi).
By Early Pliocene, the retreat of Calabria consumed the oceanic slab of the Ionian sea while new oceanic crust was created in the Tyrrhenian Sea by back-arc magmatism. Since Pleistocene, the eastern portion of the arc formed the Apennine mountain of Italy, while the Calabrian block slid to Sicily through right lateral strike-slip motion ...
The Adriatic Sea is a carbonate platform structural belt with Mesozoic-Paleogene flysch, chert, and limestone superimposed on it. Cenozoic Paleogene rocks unconformably overlie Cretaceous rocks with bauxite , coal and freshwater limestone, overlain by marine limestone from the Eocene and flysch formed in a trough between two carbonate platforms.
The plains are interspersed by the horst and graben structures, believed to break the Pannonian Sea surface as islands. The greatest concentration of ground at relatively high elevations is found in Lika and Gorski Kotar areas in the Dinaric Alps, but such areas are found in all regions of Croatia to some extent.