Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi

In this study, structural and tectonic factors which are effecting geomorphology of Çalıdere Basin which is one of the basin located at the north of Armutlu Peninsula, one of important morphotectonic factor in Marmara are assessed with geomorphometric index applications. The study is a geomorphometr...

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Main Author: Yıldız Güney
Format: Article
Language:English
Published: Ankara University 2018-10-01
Series:Coğrafi Bilimler Dergisi
Subjects:
Online Access:https://dergipark.org.tr/tr/pub/aucbd/issue/44742/556041
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author Yıldız Güney
author_facet Yıldız Güney
author_sort Yıldız Güney
collection DOAJ
description In this study, structural and tectonic factors which are effecting geomorphology of Çalıdere Basin which is one of the basin located at the north of Armutlu Peninsula, one of important morphotectonic factor in Marmara are assessed with geomorphometric index applications. The study is a geomorphometric analysis of river basin. And aim of the study is defining effects geologic structure and tectonic to basin's geomorphology and it's results. The structural and tectonic factors which are effecting basin's topography may be revealed quantitatively by using geomorphometric indexes. Therefore, geomorphometric indexes which are usually used for defining effects of geologic structure and tectonic on topograhpy such as hypsometric curve-hypsometric integral, transverse topographic symmetry, stream length gradient index, valley height-width ratio, are implemented into Çalıdere Basin. In implementation, 10 meter-resolution digital elevation model, geology data, active fault data of the research area and ArcGIS 10.2 which is one of the Geographic Information System software. Results have shown that the fault below the basin is an important tectonic factor for the geomorphology of the basin. The reason of both anormality in the stream lenght gradient index and the bow in the hypsometric curve is reflection of fault to morphology. Hypsometric integral, valley height-width ratio of the basin show that this is a young basin which was shaped by the effects of active tectonic process. The results of the study include data which can support geologic, tectonic and morphotectonic studies of the area.
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spelling doaj.art-0de52800cd154d5fafa8ad2410b57ee72023-03-15T08:28:11ZengAnkara UniversityCoğrafi Bilimler Dergisi1303-58511308-97652018-10-0116225927110.1501/Cogbil_0000000201Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle DeğerlendirilmesiYıldız Güney0https://orcid.org/0000-0002-0756-9246Uşak Üniversitesi, Fen-Edebiyat Fakültesi, Coğrafya Bölümü, Uşak In this study, structural and tectonic factors which are effecting geomorphology of Çalıdere Basin which is one of the basin located at the north of Armutlu Peninsula, one of important morphotectonic factor in Marmara are assessed with geomorphometric index applications. The study is a geomorphometric analysis of river basin. And aim of the study is defining effects geologic structure and tectonic to basin's geomorphology and it's results. The structural and tectonic factors which are effecting basin's topography may be revealed quantitatively by using geomorphometric indexes. Therefore, geomorphometric indexes which are usually used for defining effects of geologic structure and tectonic on topograhpy such as hypsometric curve-hypsometric integral, transverse topographic symmetry, stream length gradient index, valley height-width ratio, are implemented into Çalıdere Basin. In implementation, 10 meter-resolution digital elevation model, geology data, active fault data of the research area and ArcGIS 10.2 which is one of the Geographic Information System software. Results have shown that the fault below the basin is an important tectonic factor for the geomorphology of the basin. The reason of both anormality in the stream lenght gradient index and the bow in the hypsometric curve is reflection of fault to morphology. Hypsometric integral, valley height-width ratio of the basin show that this is a young basin which was shaped by the effects of active tectonic process. The results of the study include data which can support geologic, tectonic and morphotectonic studies of the area.https://dergipark.org.tr/tr/pub/aucbd/issue/44742/556041geomorphometric analysisriver basin morphometrymorphotectonicgeographical information systems
spellingShingle Yıldız Güney
Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
Coğrafi Bilimler Dergisi
geomorphometric analysis
river basin morphometry
morphotectonic
geographical information systems
title Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
title_full Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
title_fullStr Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
title_full_unstemmed Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
title_short Çalıdere Havzası'nın (Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
title_sort calidere havzasi nin armutlu yarimadasi yalova morfotektoniginin jeomorfometrik analizlerle degerlendirilmesi
topic geomorphometric analysis
river basin morphometry
morphotectonic
geographical information systems
url https://dergipark.org.tr/tr/pub/aucbd/issue/44742/556041
work_keys_str_mv AT yıldızguney calıderehavzasınınarmutluyarımadasıyalovamorfotektonigininjeomorfometrikanalizlerledegerlendirilmesi