Lake Van is the fourth largest terminal lake in the world (volume 607km3, area 3570km2, maximum depth 460m), extending for 130km WSW–ENE on the Eastern Anatolian High …
C Montenat, P Barrier, C Hibsch - Sedimentary Geology, 2007 - Elsevier
The main types of seismites are reviewed following the proposed classification and are illustrated by our own case studies. The large variety of seismites, depends on the …
Lake Lisan, the late Pleistocene precursor of the Dead Sea, existed from∼ 70,000 to 15,000 yr BP It evolved through frequent water-level fluctuations, which reflected the regional …
The Dead Sea is a terminal lake of one of the largest hydrological systems in the Levant and may thus be viewed as a large rain gauge for the region. Variations of its level are indicative …
Y Enzel, A Agnon, M Stein - Geological Society of …, 2004 - pubs.geoscienceworld.org
This work presents a high-resolution lake-level record of the late Holocene Dead Sea, a hypersaline terminal lake whose drainage basin encompasses both Mediterranean and …
GI Alsop, S Marco - Journal of Structural Geology, 2011 - Elsevier
The Late Pleistocene Lisan Formation preserved next to the Dead Sea provides exceptional 3-D exposures of folds and faults generated during soft-sediment slumping and deformation …
C Migowski, A Agnon, R Bookman… - Earth and Planetary …, 2004 - Elsevier
A high-resolution Holocene seismic history of the Dead Sea Transform (DST) is established from laminated sedimentary cores recovered at the shores of the Dead Sea. Radiocarbon …
This article presents the role of climate fluctuations in shaping southern Levantine human history from 3600 to 600 BCE (the Bronze and Iron Ages) as evidenced in palynological …
Abstract The Late Pleistocene Lisan Formation contains superb examples of soft-sediment deformation generated during gravity-driven slumping and failure down extremely gentle (< …