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The first drilling of the Messinian salt at the deeper parts of the Mediterranean Sea came in the summer of 1970, when geologists aboard the Glomar Challenger brought up drill cores containing arroyo gravels and red and green floodplain silts; and gypsum, anhydrite, rock salt, and various other evaporite minerals that often form from drying of ...
The Zanclean flood or Zanclean deluge is theorized to have refilled the Mediterranean Sea 5.33 million years ago. [1] This flooding ended the Messinian salinity crisis and reconnected the Mediterranean Sea to the Atlantic Ocean, although it is possible that even before the flood there were partial connections to the Atlantic Ocean. [2]
Fleur de sel. Fleur de sel ("flower of salt" in French; French pronunciation: [flœʁ də sɛl]) or flor de sal (also "flower of salt" in Portuguese, Spanish and Catalan) is a salt that forms as a thin, delicate crust on the surface of seawater as it evaporates.
Sea of Marmara: mediterranean sea: Between the Balkan Peninsula and the Anatolian peninsula [31] 3.17: Chilika Lake: lagoon: India [32] 1.30–2.30: Black Sea: mediterranean sea: Between Europe and Asia - Balkan Peninsula, Eastern Europe, Anatolia, Caucasus [33] 2.30: Lake Van: salt lake: Turkey [34] 1.40 Qinghai Lake: salt lake China [35] 1.25 ...
Unrefined sea salt is minimally processed, retaining trace minerals that might lend color or flavor to the salt. (Refined sea salt, though, has been washed to remove minerals and contaminants, so ...
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 ...
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