Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun
The North Anatolian Fault Zone (NAFZ) is one of the most important Neotectonic structures of Türkiye. In this study, the section of the NAFZ between Kızılırmak and Tersakan Stream was examined. The study was conducted with Geographic Information Systems and field observations. In order to numericall...
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Ankara University
2025-04-01
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| Series: | Coğrafi Bilimler Dergisi |
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| Online Access: | https://dergipark.org.tr/tr/pub/aucbd/issue/88528/1613195 |
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| author | Serkan Gürgöze Ali Uzun |
| author_facet | Serkan Gürgöze Ali Uzun |
| author_sort | Serkan Gürgöze |
| collection | DOAJ |
| description | The North Anatolian Fault Zone (NAFZ) is one of the most important Neotectonic structures of Türkiye. In this study, the section of the NAFZ between Kızılırmak and Tersakan Stream was examined. The study was conducted with Geographic Information Systems and field observations. In order to numerically analyse the effect of tectonics on drainage, 8 drainage basins were analysed using the hypsometric curve-hypsometric integral (HI:0,33-0,59), mountain front sinuosity (Smf: 1,21-1,75), Valley floor width- to-height ratio (Vf:0,15-1,85), Stream length gradient index (SL:269,55-1159,25), Basin shape (Bs:1,32-5,51) and Asymmetry factor (AF:33,21-81,9). According to the Relative Tectonic Activity (IAT) classification, 3 of the 8 drainage basins (Soruk, Istavloz streams and Ovacık Creek) are in very high tectonic activity class, 2 (Ulu Stream and Zeytin Creek) are in high tectonic activity class and 3 (Göl, Susuz streams and Çorak Creek) are in medium tectonic activity class. According to these results, it was determinted that tectonic activity was high in the drainage basins controlled by the NAFZ, and the degree of tectonic activity decreases as one moves away from the NAFZ. |
| format | Article |
| id | doaj-art-f1a6c5ba8e2a421a934cc143e1b4e3f2 |
| institution | DOAJ |
| issn | 1303-5851 1308-9765 |
| language | English |
| publishDate | 2025-04-01 |
| publisher | Ankara University |
| record_format | Article |
| series | Coğrafi Bilimler Dergisi |
| spelling | doaj-art-f1a6c5ba8e2a421a934cc143e1b4e3f22025-08-20T03:10:54ZengAnkara UniversityCoğrafi Bilimler Dergisi1303-58511308-97652025-04-0123115117810.33688/aucbd.1613195Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, SamsunSerkan Gürgöze0https://orcid.org/0000-0002-3025-2327Ali Uzun1https://orcid.org/0000-0003-3854-2780Ondokuz Mayıs Üniversitesi, İnsan ve Toplum Bilimleri Fakültesi, Coğrafya Bölümü, Samsun/TürkiyeOndokuz Mayıs Üniversitesi, İnsan ve Toplum Bilimleri Fakültesi, Coğrafya Bölümü, Samsun/TürkiyeThe North Anatolian Fault Zone (NAFZ) is one of the most important Neotectonic structures of Türkiye. In this study, the section of the NAFZ between Kızılırmak and Tersakan Stream was examined. The study was conducted with Geographic Information Systems and field observations. In order to numerically analyse the effect of tectonics on drainage, 8 drainage basins were analysed using the hypsometric curve-hypsometric integral (HI:0,33-0,59), mountain front sinuosity (Smf: 1,21-1,75), Valley floor width- to-height ratio (Vf:0,15-1,85), Stream length gradient index (SL:269,55-1159,25), Basin shape (Bs:1,32-5,51) and Asymmetry factor (AF:33,21-81,9). According to the Relative Tectonic Activity (IAT) classification, 3 of the 8 drainage basins (Soruk, Istavloz streams and Ovacık Creek) are in very high tectonic activity class, 2 (Ulu Stream and Zeytin Creek) are in high tectonic activity class and 3 (Göl, Susuz streams and Çorak Creek) are in medium tectonic activity class. According to these results, it was determinted that tectonic activity was high in the drainage basins controlled by the NAFZ, and the degree of tectonic activity decreases as one moves away from the NAFZ.https://dergipark.org.tr/tr/pub/aucbd/issue/88528/1613195morphometric indexrelative tectonic activitykızılırmaknorth anatolian fault zonesamsun |
| spellingShingle | Serkan Gürgöze Ali Uzun Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun Coğrafi Bilimler Dergisi morphometric index relative tectonic activity kızılırmak north anatolian fault zone samsun |
| title | Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun |
| title_full | Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun |
| title_fullStr | Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun |
| title_full_unstemmed | Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun |
| title_short | Tektoniğin Drenaj Havzalarına Etkisinin Morfometrik İndislerle İncelenmesi, Kuzey Anadolu Fay Zonu’nun Kızılırmak ile Tersakan Çayı Arası, Samsun |
| title_sort | tektonigin drenaj havzalarina etkisinin morfometrik indislerle incelenmesi kuzey anadolu fay zonu nun kizilirmak ile tersakan cayi arasi samsun |
| topic | morphometric index relative tectonic activity kızılırmak north anatolian fault zone samsun |
| url | https://dergipark.org.tr/tr/pub/aucbd/issue/88528/1613195 |
| work_keys_str_mv | AT serkangurgoze tektonigindrenajhavzalarınaetkisininmorfometrikindislerleincelenmesikuzeyanadolufayzonununkızılırmakiletersakancayıarasısamsun AT aliuzun tektonigindrenajhavzalarınaetkisininmorfometrikindislerleincelenmesikuzeyanadolufayzonununkızılırmakiletersakancayıarasısamsun |