The Sharon Escarpment or Sharon Cliff is the escarpment in Israel that connects the level of the coastal plain with the level of the Mediterranean Sea beach and the continental shelf and stretches along the Sharon coastal ridge approximately between Giv'at Olga and Tel Aviv, i.e., along the Sharon plain. The ridge was formed during the Late Pleistocene and the cliff developed when at about 7,500 years Before Present (BP) the sea level reached the western edge of the current ridge. Now this edge is at about 8 m. below the sea level.
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