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Geomorphology of the Mesopotamian Plain: A Critical Review
University of Kurdistan Hewler. Private Consultant Geologist, Erbil.
Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, Geoteknologi.ORCID-id: 0000-0002-6790-2653
Consultant Dam Engineer, Sweden.
Chief Geologist, Iraq Geological Survey, Baghdad.
Vise andre og tillknytning
2020 (engelsk)Inngår i: Journal of Earth Sciences and Geotechnical Engineering, ISSN 1792-9040, E-ISSN 1792-9660, Vol. 10, nr 4, s. 1-25Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The Mesopotamian Plain is part of the large Mesopotamia which extends in Iraq and surrounding countries. The plain is almost flat and vast lowland, which has clearly defined physiographic boundaries with the other surrounding physiographic provinces. From the north and east, it is limited by the Low Amplitude Mountainous Province. From the west, the upper part is limited by Al-Jazira Plain, whereas in the lower part by the Western Desert Province. From the south it is limited by the Southern Desert Province. The plain is a huge accumulational geomorphologic unit, where the fluvial, lacustrine, and Aeolian landforms prevail; the fluvial units being the abundant among others. However, estuarine and marine forms also are developed, but restricted to the extreme south-eastern reaches of the plain. Moreover, some erosional landforms are developed in different places, but are not well expressed. In the central eastern part, large alluvial fans are developed with five stages covering vast areas along the Iraqi – Iranian international borders. The geomorphic units are classified according to origin, geomorphic position, and lithology. Some of the significant features are described with some details.

sted, utgiver, år, opplag, sider
UK: Scientific Press International Limited , 2020. Vol. 10, nr 4, s. 1-25
Emneord [en]
Mesopotamian plain, fluvial units, Alluvial fans, Marshes, Aeolian forms
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Identifikatorer
URN: urn:nbn:se:ltu:diva-78074OAI: oai:DiVA.org:ltu-78074DiVA, id: diva2:1414829
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Validerad;2020;Nivå 1;2020-04-24 (marisr)

Tilgjengelig fra: 2020-03-16 Laget: 2020-03-16 Sist oppdatert: 2020-04-24bibliografisk kontrollert

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Al-Ansari, NadhirLaue, Jan

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