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50 - Evolution of the Southeastern Mediterranean Coastal Plain

from Part V: - Quaternary Geomorphology

Published online by Cambridge University Press:  04 May 2017

Yehouda Enzel
Affiliation:
Hebrew University of Jerusalem
Ofer Bar-Yosef
Affiliation:
Harvard University, Massachusetts
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Summary

Field surveys, chronology, geology, geomorphology, pedology and archaeological records were used in comprehensive synthesis outlining the evolution of the Israeli Coastal Plain under late Quaternary sea level changes. We discuss buried soil-stratigraphy vs. sediments, sand dunes, and the formation of the observed topography and terrain morphology. This synthesis indicates that extensive sand field active during eustatic sea regression were stabilized during glacial maxima by vegetation; this was followed by pedogenesis and erosion of fine eolian sediments into depressions. During interglacials, additional sand accumulated covering regressive deposits. During interglacial, the sedimentation is followed by erosion under coastal cliff activity and incision of the fluvial systems due to high gradient and stream capturing. This sequence of glacial-interglacial scale processes results in east to west accretion of the Quaternary Coastal Plain, forming the typical series of coast parallel relict sedimentary ridges (complexes) and fluvial-filled troughs.
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Quaternary of the Levant
Environments, Climate Change, and Humans
, pp. 433 - 446
Publisher: Cambridge University Press
Print publication year: 2017

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