Levantine Sea to be the oldest known ocean crust worldwide. The Suez Canal was completed in 1869, linking the Levantine Sea to the Red Sea. The Red Sea's level is higher than the Eastern Mediterranean, so the canal serves as a tidal strait that pours Red Sea water into the Mediterranean. The Bitter Lakes, which are hypersaline natural lakes that form part of the canal, blocked the migration of Red Sea species into the Mediterranean for many decades, but as the salinity of the lakes gradually equalized with that of the Red Sea, the barrier to migration was removed, and plants and
Mediterranean–Dead Sea Canal Mediterranean–Dead Sea Canal The Mediterranean–Dead Sea Canal (MDSC) is a proposed project to dig a canal from the Mediterranean Sea to the Dead Sea, taking advantage of the 400-metre difference in water level between the seas. It is not to be confused with the Red Sea–Dead Sea Water Conveyance. The project could correct the drop in the level of the Dead Sea observed in recent years. The canal could also be used to generate hydroelectric power because of surface difference and maybe by salinity gradient power, and desalinate water by reverse osmosis. The idea was first proposed by William Allen