Dead Sea hypothesis is that the Dead Sea lies in a true rift zone, an extension of the Red Sea Rift, or even of the Great Rift Valley of eastern Africa. A more recent hypothesis is that the Dead Sea basin is a consequence of a "step-over" discontinuity along the Dead Sea Transform, creating an extension of the crust with consequent subsidence. Around 3.7 million years ago, what is now the valley of the Jordan River, Dead Sea, and the northern Wadi Arabah was repeatedly inundated by waters from the Mediterranean Sea. The waters formed in a narrow, crooked bay that is
Dead River (Sabattus River tributary) the north, in the northern part of Leeds. Dead River (Sabattus River tributary) The Dead River is a tributary of Sabattus Pond in the U.S. state of Maine. Via the Sabattus River, the outflow of the pond, the Dead River is part of the Androscoggin River watershed, flowing to the Kennebec River and ultimately the Atlantic Ocean. The Dead River rises in the southern part of the town of Leeds and flows south, passing through the northwest corner of the town of Wales, then flowing through Greene to its outlet at the north end of Sabattus Pond. Another Dead River