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The Zanclean flood caused a major change in the environment of the Mediterranean basin; the continental "Lago Mare" facies was replaced by Zanclean deep sea deposits. [7] The flood may have affected global climate, considering that the much smaller flood triggered when Lake Agassiz drained did result in a cold period. [ 50 ]
Physical and political map of the Mediterranean basin. In biogeography, the Mediterranean basin (/ ˌ m ɛ d ɪ t ə ˈ r eɪ n i ən / MED-ih-tə-RAY-nee-ən), also known as the Mediterranean region or sometimes Mediterranea, is the region of lands around the Mediterranean Sea that have mostly a Mediterranean climate, with mild to cool, rainy winters and warm to hot, dry summers, which ...
The Messinian Erosional Crisis is a phase in the Messinian evolution of the central Mediterranean basin resulting from major drawdown of the Mediterranean seawater (the "Messinian Salinity Crisis"). As outlined in numerous studies, erosional events along the margins of the Mediterranean Basin during the Messinian timespan, before and during the ...
In the empty Mediterranean Basin, the summertime temperatures would probably have been extremely high. As a first approximation, using the dry adiabatic lapse rate of around 10 °C (18 °F) per kilometer, the maximum possible temperature of an area 4 km (2.5 mi) below sea level would be about 40 °C (72 °F) warmer than it would be at sea level.
Klepáč – one of six places in Europe where three watersheds meet Rhine–Danube watershed marker near Weitnau, Germany European watershed marker (Lviv Oblast, 2009). The divide continues northwards along the Albula Alps to Julier Pass, Albula Pass and Flüela Pass south of Davos, between the catchment area of the Rhine, which empties into the North Sea via the Netherlands, and the Danube ...
Two thirds of the damage was attributed to the production sector (500 million direct and 569 million indirect), of which 228 million in the agricultural sector. Total damage on the housing was 227.3 million, while the infrastructure damage (transportation, communications and water management) was assessed at 192 million. [40]
The result is the formation of the Mediterranean Water that finally spreads into the interior of the North Atlantic forming the most prominent basin-scale thermohaline anomaly at mid-depths, the Mediterranean Salt Tongue, recognizable as a basin-scale salinity anomaly at 1000–1200 m depth through the North Atlantic (see Figure 2).
The term Mediterranean-Mjosa Zone (Mittelmeer-Mjösen-Zone) was coined by the German geologist Hans Stille in about 1930 to describe a rift in the continental Crust crossing Europe from the Mediterranean Sea via Marseille, the Rhine rift as far as Mjøsa in the south of Norway, a total length of 2000 km.