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The Zofar Fault -- A major intra-rift feature in the Arava rift valley

, , , and . Geological Survey of Israel Current Research, (1998)

Abstract

The margins of the Arava Rift, from the Dead Sea to the Gulf of Elat, have been investigated in the last five years by combining several methods previously not utilized in this area. These investigations included new surface geological mapping, as well as several seismic reflection surveys, accompanied by a detailed study of two continental units: the Miocene Hazeva and the Pliocene-Pleistocene Arava formations. These investigations led to the identification of several new structural features within this segment of the rift, which is characterized by a series of elongated en-echelon tectonic basins. The depths of these basins, which are filled with clastic sediments, vary from several hundred meters to a few kilometers.

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