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The Dead Sea: Tectonic concurrence below ten kilometres of sediments
Science Centric (30 Jan 2009 19:15 GMT) - The Dead Sea lies in a basin structure situated below the sea level. This deep subsidence is a result of a tectonic concurrence between processes in the upper lithosphere that led to subsiding and a compensating upward flow of rocks in the deeper layers of the lithosphere…— copy and paste the formatted text using the form to the left.