GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS

Study area is in boundary province of Osmaniye at the sub region where it is Adana Part of Mediterranean Region. It has very difference topography because it is very young and active in terms of tectonic. Study area occurs a lot of geomorphologic units. Tectonism is the most importance factor to for...

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Autores principales:	İsmail EGE, İbrahim KORTUK
Formato:	article
Lenguaje:	DE EN FR TR
Publicado:	Fırat University 2019
Materias:	geomorphology düziçi plain north amanos düziçi osmaniye Social Sciences H Social sciences (General) H1-99
Acceso en línea:	https://doaj.org/article/85921d2c6cfb4f7983fe44867cabc68d
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id	oai:doaj.org-article:85921d2c6cfb4f7983fe44867cabc68d
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spelling	oai:doaj.org-article:85921d2c6cfb4f7983fe44867cabc68d2021-11-24T09:20:56ZGEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS2148-416310.9761/JASSS2538https://doaj.org/article/85921d2c6cfb4f7983fe44867cabc68d2019-08-01T00:00:00Zhttps://jasstudies.com/index.jsp?mod=tammetin&makaleadi=1507759839_20-Yrd.%20Do%C3%A7.%20Dr.%20%C4%B0smail%20EGE.pdf&key=27224https://doaj.org/toc/2148-4163Study area is in boundary province of Osmaniye at the sub region where it is Adana Part of Mediterranean Region. It has very difference topography because it is very young and active in terms of tectonic. Study area occurs a lot of geomorphologic units. Tectonism is the most importance factor to form. Furthermore, fluvial processes and karstification are secondary factors to take on shaping. Main geomorphologic units on the Düziçi plain which is nearly 90 km2 and near surrounding are Mountain-hills area, plateaus, valleys, brings alluvial fans and karstic forms which are small scale. Düziçi plain is elevation between 250 and 450 meters (average 350m.). Alluvial fans are between 300-400 meters in the east part of plain and mountainous-hilly areas are especially between 400-2246 meters in the part of east. Very small hills which are pressed down and volcanic cone are between 200-700 meters except for east other sides near the plain. Study area shaping had started from Miosen after that time tectonic activities had continued so, plain area has collapsed but mountainously area has increased since Miosen and along Pliosen-Quaternary. In the study area volcanic activity especially basalt flow and deposition in the lake had continued during the Plio-Quaternary and Quaternary era. In this way, Düziçi plain which is between 250-400 meters and its near surrounding have occurred and shaping which is especially erosion-deposition have been continued by rivers-weather present days (Holocene).İsmail EGEİbrahim KORTUKFırat Universityarticlegeomorphologydüziçi plainnorth amanosdüziçiosmaniyeSocial SciencesHSocial sciences (General)H1-99DEENFRTRJournal of Academic Social Science Studies , Vol 8, Iss 33, Pp 295-313 (2019)
institution	DOAJ
collection	DOAJ
language	DE EN FR TR
topic	geomorphology düziçi plain north amanos düziçi osmaniye Social Sciences H Social sciences (General) H1-99
spellingShingle	geomorphology düziçi plain north amanos düziçi osmaniye Social Sciences H Social sciences (General) H1-99 İsmail EGE İbrahim KORTUK GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS
description	Study area is in boundary province of Osmaniye at the sub region where it is Adana Part of Mediterranean Region. It has very difference topography because it is very young and active in terms of tectonic. Study area occurs a lot of geomorphologic units. Tectonism is the most importance factor to form. Furthermore, fluvial processes and karstification are secondary factors to take on shaping. Main geomorphologic units on the Düziçi plain which is nearly 90 km2 and near surrounding are Mountain-hills area, plateaus, valleys, brings alluvial fans and karstic forms which are small scale. Düziçi plain is elevation between 250 and 450 meters (average 350m.). Alluvial fans are between 300-400 meters in the east part of plain and mountainous-hilly areas are especially between 400-2246 meters in the part of east. Very small hills which are pressed down and volcanic cone are between 200-700 meters except for east other sides near the plain. Study area shaping had started from Miosen after that time tectonic activities had continued so, plain area has collapsed but mountainously area has increased since Miosen and along Pliosen-Quaternary. In the study area volcanic activity especially basalt flow and deposition in the lake had continued during the Plio-Quaternary and Quaternary era. In this way, Düziçi plain which is between 250-400 meters and its near surrounding have occurred and shaping which is especially erosion-deposition have been continued by rivers-weather present days (Holocene).
format	article
author	İsmail EGE İbrahim KORTUK
author_facet	İsmail EGE İbrahim KORTUK
author_sort	İsmail EGE
title	GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS
title_short	GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS
title_full	GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS
title_fullStr	GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS
title_full_unstemmed	GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS
title_sort	geomorphology of duziçi plain (duziçi/osmaniye) and its near surroundings
publisher	Fırat University
publishDate	2019
url	https://doaj.org/article/85921d2c6cfb4f7983fe44867cabc68d
work_keys_str_mv	AT ismailege geomorphologyofduziciplainduziciosmaniyeanditsnearsurroundings AT ibrahimkortuk geomorphologyofduziciplainduziciosmaniyeanditsnearsurroundings
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GEOMORPHOLOGY OF DUZIÇI PLAIN (DUZIÇI/OSMANIYE) AND ITS NEAR SURROUNDINGS

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