Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers

We present the geomorphological map of the northwestern part of the Kurdistan Region of Iraq, where the landscape expresses the tectonic activity associated with the Arabia-Eurasia convergence and Neogene climate change. These processes influenced the evolution of landforms and fluvial pathways, whe...

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Main Authors: Luca Forti, Alessandro Perego, Filippo Brandolini, Guido S. Mariani, Mjahid Zebari, Kathleen Nicoll, Eleonora Regattieri, Cecilia Conati Barbaro, Daniele Morandi Bonacossi, Hasan Ahmed Qasim, Mauro Cremaschi, Andrea Zerboni
Format: Article
Language:English
Published: Taylor & Francis Group 2021-03-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2021.1906339
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spelling doaj-1fbd913130034b5a9f871f670f8ab3a22021-04-21T16:14:24ZengTaylor & Francis GroupJournal of Maps1744-56472021-03-010011210.1080/17445647.2021.19063391906339Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab RiversLuca Forti0Alessandro Perego1Filippo Brandolini2Guido S. Mariani3Mjahid Zebari4Kathleen Nicoll5Eleonora Regattieri6Cecilia Conati Barbaro7Daniele Morandi Bonacossi8Hasan Ahmed Qasim9Mauro Cremaschi10Andrea Zerboni11Università degli Studi di MilanoUniversità degli Studi di MilanoUniversità degli Studi di MilanoUniversità degli Studi di CagliariFriedrich-Schiller University JenaThe University of UtahIstituto di Geoscienze e Georisorse, CNRSapienza Università di RomaUniversità degli Studi di UdineDirectorate of Antiquities Kurdistan RegionUniversità degli Studi di MilanoUniversità degli Studi di MilanoWe present the geomorphological map of the northwestern part of the Kurdistan Region of Iraq, where the landscape expresses the tectonic activity associated with the Arabia-Eurasia convergence and Neogene climate change. These processes influenced the evolution of landforms and fluvial pathways, where major rivers Tigris, Khabur, and Great Zab incise the landscape of Northeastern Mesopotamia Anticlinal ridges and syncline trough compose the Zagros orogen. The development of water and wind gaps, slope, and karsts processes in the highlands and the tilting of fluvial terraces in the flat areas are the main evidence of the relationship between tectonics, climate variations and geomorphological processes. During the Quaternary, especially after the Last Glacial Maximum, fluctuating arid and wet periods also influenced local landforms and fluvial patterns of the area. Finally, the intensified Holocene human occupation and agricultural activities during the passage to more complex societies over time impacted the evolution of the landscape in this part of Mesopotamia.http://dx.doi.org/10.1080/17445647.2021.1906339compressive tectonicfoldingfluvial networkkarstzagros mountainstigris river
collection DOAJ
language English
format Article
sources DOAJ
author Luca Forti
Alessandro Perego
Filippo Brandolini
Guido S. Mariani
Mjahid Zebari
Kathleen Nicoll
Eleonora Regattieri
Cecilia Conati Barbaro
Daniele Morandi Bonacossi
Hasan Ahmed Qasim
Mauro Cremaschi
Andrea Zerboni
spellingShingle Luca Forti
Alessandro Perego
Filippo Brandolini
Guido S. Mariani
Mjahid Zebari
Kathleen Nicoll
Eleonora Regattieri
Cecilia Conati Barbaro
Daniele Morandi Bonacossi
Hasan Ahmed Qasim
Mauro Cremaschi
Andrea Zerboni
Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers
Journal of Maps
compressive tectonic
folding
fluvial network
karst
zagros mountains
tigris river
author_facet Luca Forti
Alessandro Perego
Filippo Brandolini
Guido S. Mariani
Mjahid Zebari
Kathleen Nicoll
Eleonora Regattieri
Cecilia Conati Barbaro
Daniele Morandi Bonacossi
Hasan Ahmed Qasim
Mauro Cremaschi
Andrea Zerboni
author_sort Luca Forti
title Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers
title_short Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers
title_full Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers
title_fullStr Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers
title_full_unstemmed Geomorphology of the northwestern Kurdistan Region of Iraq: landscapes of the Zagros Mountains drained by the Tigris and Great Zab Rivers
title_sort geomorphology of the northwestern kurdistan region of iraq: landscapes of the zagros mountains drained by the tigris and great zab rivers
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2021-03-01
description We present the geomorphological map of the northwestern part of the Kurdistan Region of Iraq, where the landscape expresses the tectonic activity associated with the Arabia-Eurasia convergence and Neogene climate change. These processes influenced the evolution of landforms and fluvial pathways, where major rivers Tigris, Khabur, and Great Zab incise the landscape of Northeastern Mesopotamia Anticlinal ridges and syncline trough compose the Zagros orogen. The development of water and wind gaps, slope, and karsts processes in the highlands and the tilting of fluvial terraces in the flat areas are the main evidence of the relationship between tectonics, climate variations and geomorphological processes. During the Quaternary, especially after the Last Glacial Maximum, fluctuating arid and wet periods also influenced local landforms and fluvial patterns of the area. Finally, the intensified Holocene human occupation and agricultural activities during the passage to more complex societies over time impacted the evolution of the landscape in this part of Mesopotamia.
topic compressive tectonic
folding
fluvial network
karst
zagros mountains
tigris river
url http://dx.doi.org/10.1080/17445647.2021.1906339
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