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The River Orontes in Syria and Turkey: downstream variation of fluvial archives in different crustal blocks

Bridgland, D.R.; Westaway, R.; Romieh, M.A.; Candy, I.; Daoud, M.; Demir, T.; Galiatsatos, N.; Schreve, D.C.; Seyrek, A.; Shaw, A.D.; White, T.; Whittaker, J.

The River Orontes in Syria and Turkey: downstream variation of fluvial archives in different crustal blocks Thumbnail


R. Westaway

M.A. Romieh

I. Candy

M. Daoud

T. Demir

N. Galiatsatos

D.C. Schreve

A. Seyrek

A.D. Shaw

T. White

J. Whittaker


The geomorphology and Quaternary history of the River Orontes in western Syria and south-central Turkey have been studied using a combination of methods: field survey, differential GPS, satellite imagery, analysis of sediments to determine provenance, flow direction and fluvial environment, incorporation of evidence from fossils for both palaeoenvironments and biostratigraphy, uranium-series dating of calcrete cement, reconciliation of Palaeolithic archaeological contents, and uplift modelling based on terrace height distribution. The results underline the contrasting nature of different reaches of the Orontes, in part reflecting different crustal blocks, with different histories of landscape evolution. Upstream from Homs the Orontes has a system of calcreted terraces that form a staircase extending to ~200 m above the river. New U-series dating provides an age constraint within the lower part of the sequence that suggests underestimation of terrace ages in previous reviews. This upper valley is separated from another terraced reach, in the Middle Orontes, by a gorge cut through the Late Miocene–Early Pliocene Homs Basalt. The Middle Orontes terraces have long been recognized as a source of mammalian fossils and Palaeolithic artefacts, particularly from Latamneh, near the downstream end of the reach. This terraced section of the valley ends at a fault scarp, marking the edge of the subsiding Ghab Basin (a segment of the Dead Sea Fault Zone), which has been filled to a depth of ~ 1 km by dominantly lacustrine sediments of Pliocene–Quaternary age. Review of the fauna from Latamneh suggests that its age is 1.2–0.9 Ma, significantly older than previously supposed, and commensurate with less uplift in this reach than both the Upper and Lower Orontes. Two localities near the downstream end of the Ghab have provided molluscan and ostracod assemblages that record somewhat saline environments, perhaps caused by desiccation within the former lacustrine basin, although they include fluvial elements. The Ghab is separated from another subsiding and formerly lacustrine depocentre, the Amik Basin of Hatay Province, Turkey, by a second gorge, implicit of uplift, this time cut through Palaeogene limestone. The NE–SW oriented lowermost reach of the Orontes is again terraced, with a third and most dramatic gorge through the northern edge of the Ziyaret Dağı mountains, which are known to have experienced rapid uplift, probably again enhanced by movement on an active fault. Indeed, a conclusion of the research, in which these various reaches are compared, is that the crust in the Hatay region is significantly more dynamic than that further upstream, where uplift has been less rapid and less continuous.


Bridgland, D., Westaway, R., Romieh, M., Candy, I., Daoud, M., Demir, T., …Whittaker, J. (2012). The River Orontes in Syria and Turkey: downstream variation of fluvial archives in different crustal blocks. Geomorphology, 165-166, 25-49.

Journal Article Type Article
Publication Date Sep 1, 2012
Deposit Date Mar 8, 2012
Publicly Available Date Mar 28, 2013
Journal Geomorphology
Print ISSN 0169-555X
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 165-166
Pages 25-49
Keywords River Orontes, River terraces, Fluvial deposits, Uplift, Subsidence.


Accepted Journal Article (4.1 Mb)

Copyright Statement
NOTICE: this is the author’s version of a work that was accepted for publication in Geomorphology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Geomorphology, 165-166, 2012, 10.1016/j.geomorph.2012.01.011

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