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The Mediterranean Outflow is a current flowing from the Mediterranean Sea towards the Atlantic Ocean through the Strait of Gibraltar. Once it has reached the western side of the Strait of Gibraltar, it divides into two branches, one flowing westward following the Iberian continental slope, and another returning to the Strait of Gibraltar ...
The main Zanclean flood may have been preceded by an earlier smaller flood event, [10] [44] and the presence of deep sea terraces has been used to infer that the refilling of the Mediterranean occurred in several pulses. [45] Complete refilling of the Mediterranean may have taken about a decade. [7]
In oceanography, a mediterranean sea (/ ˌ m ɛ d ɪ t ə ˈ r eɪ n i ə n / MED-ih-tə-RAY-nee-ən) is a mostly enclosed sea that has limited exchange of water with outer oceans and whose water circulation is dominated by salinity and temperature differences rather than by winds or tides.
Outflow may refer to: Capital outflow, the capital leaving a particular economy; Bipolar outflow, in astronomy, two continuous flows of gas from the poles of a star; Outflow (hydrology), the discharge of a lake or other reservoir system; Outflow (meteorology), air that flows outwards from a thunderstorm
The Camarinal Sill is the sill separating the Mediterranean Sea and the Atlantic Ocean. This threshold is the shallowest seafloor pass between the Iberian Peninsula and Africa . It is located approximately 25 km west of the narrowest section of the Strait of Gibraltar and 20 km east of the Espartel Sill , at 35°56′N 5°45′W / 35. ...
Popular discussion of this early Holocene Black Sea flood scenario was headlined in The New York Times in December 1996 [10] and later published as a book. [9] In a series of expeditions widely covered by mainstream media, a team of marine archaeologists led by Robert Ballard identified what appeared to be ancient shorelines, freshwater snail shells, drowned river valleys, tool-worked timbers ...
The 1997 Central European flood or the 1997 Oder Flood of the Oder and Morava river basins in July 1997 affected Poland, the Czech Republic and Germany, taking the lives of 114 people and causing material damages estimated at $4.5 billion (3.8 billion euros in the Czech Republic and Poland and 330 million euros in Germany). The flooding began ...
The river's discharge at that location depends on the rainfall on the catchment or drainage area and the inflow or outflow of groundwater to or from the area, stream modifications such as dams and irrigation diversions, as well as evaporation and evapotranspiration from the area's land and plant surfaces. In storm hydrology, an important ...