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R. Dalongeville and P. sanlaville, “Variations Relatives du Niveau Marin du Golfe Persique,” In: O. Aurenche, J. Evin and F. Hours, Eds., Chronologies in the Near East, CNRS International Symposium, Lyon, BAR International Series, Vol. 379, 1986, pp. 568-580.

has been cited by the following article:

• TITLE: Geo-Historical and Geomorphological Evolution of the Sabkhas and Ridges at the Al-Khiran Area, State of Kuwait

  AUTHORS: Adeeba E. Al-Hurban, Hamdy I. El-Gamily

  KEYWORDS: Geo-History; Geodatabase; GIS; Remote Sensing; Coastal Ridges; Sabkha; Kuwait; Arabian Gulf

  JOURNAL NAME: Journal of Geographic Information System, Vol.5 No.3, June 17, 2013

  ABSTRACT: The State of Kuwait is located in the northwestern Arabian Gulf. It is characterized by arid to semi-arid weather. This study’s concerned with the southern coastal area of the Al-Khiran. The purpose of this study is to evaluate and study the geo-history and evolution of geomorphologic features, especially coastal Ridges and Sabkhas in the Al-Khiran study area. This study based on the field observations as well as the application of Geographic Information Systems (GIS) and Remote Sensing techniques to establish a geodatabase for the study area in different disciplines. The results showed that the Al-Khiran coastal area was affected by the sea level fluctuation and coastal sedimentation during the Holocene and late Pleistocene. The coastal Ridges were originally coastal dunes, which were composed during the sea regression periods and consolidated with time. These Ridges were developed with time and separated the Al-Khiran area as a closed lagoon. This lagoon dried with time and formed a Sabkha field, especially on the depression zone that intersected or surrounded with the coastal Ridges. The Remote Sensing change detection technique shows that the changes were mainly concentrated on covering Sabkhas in some locations and might be due to the impact of active sand sheets and Aeolian sands. Land development in the Al-Khiran area led to the demolition of most of the coastal Ridges and Sabkha deposits.