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The Judean Desert—The Major Hypogene Cave Region of the Southern Levant

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Book cover Hypogene Karst Regions and Caves of the World

Part of the book series: Cave and Karst Systems of the World ((CAKASYWO))

Abstract

The Judean Desert in eastern Israel consists of a Late Cretaceous epicontinental carbonate terrain formed at the interface between the Neotethys Ocean and the Gondwanian African-Arabian plate. Various rock types were deposited through fluctuations between marine and continental environments due to ingressions and regressions. Orogenic folding of the Syrian Arc fold system occurred between the Late Cretaceous and the Neogene. The folds formed a barrier for deep flowing groundwater, which upwelled along the SE flank of the folds. Possibly mixing with local confined circulation, the hypogene flow created maze caves at the top of the Late Cretaceous limestone, under the confinement of thick chalk, and marl successions. The larger caves are up to 3.5-km-long 2D mazes, less commonly with some additional tiers. Speleogenesis occurred most likely during the Oligocene, when far-field recharge could reach the Judean Desert. During the Neogene, the Dead Sea transform has dissected the region, forming a deep endorheic depression at the eastern border of the Judean Desert. This was followed by the lowering of the water table and related dewatering of the caves. Fault escarpments and downcutting canyons have dissected the caves, forming the present entrances. The caves are mostly dry, with rare speleothems. Gypsum rinds indicate that hydrogen sulfide and sulfuric acid took part in speleogenesis.

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Authors and Affiliations

  1. Cave Research Center, Institute of Earth Sciences, The Hebrew University of Jerusalem, 91904, Jerusalem, Israel

    Amos Frumkin, Boaz Langford & Roi Porat

Authors
  1. Amos Frumkin
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  2. Boaz Langford
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  3. Roi Porat
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Corresponding author

Correspondence to Amos Frumkin .

Editor information

Editors and Affiliations

  1. Department of Hydrogeological Problems, Institute of Geological Sciences, Kiev, Ukraine

    Alexander Klimchouk

  2. Department of Earth and Atmospheric Sciences, State University of New York, Oneonta, New York, USA

    Arthur N. Palmer

  3. Department of Biological, Geological, and Environmental Sciences, Universita di Bologna, Bologna, Italy

    Jo De Waele

  4. Instituto do Carste, Belo Horizonte, Minas Gerais, Brazil

    Augusto S. Auler

  5. University of Nice Sophia Antipolis, Sophia Antipolis Cedex, France

    Philippe Audra

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Frumkin, A., Langford, B., Porat, R. (2017). The Judean Desert—The Major Hypogene Cave Region of the Southern Levant. In: Klimchouk, A., N. Palmer, A., De Waele, J., S. Auler, A., Audra, P. (eds) Hypogene Karst Regions and Caves of the World. Cave and Karst Systems of the World. Springer, Cham. https://doi.org/10.1007/978-3-319-53348-3_28

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