THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS

In this study, distribution of landslides densely seen Karlıova Basin and surrounding is observed in accordance with elevation, slope, aspect and NDVI parts. Karlıova Basin is a tectonic origin depression which has begun to open between right-lateral strike-slip North Anatolian Fault (NAF), and left...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Vedat AVCI, Halil GÜNEK
Formato:	article
Lenguaje:	DE EN FR TR
Publicado:	Fırat University 2019
Materias:	landsl Social Sciences H Social sciences (General) H1-99
Acceso en línea:	https://doaj.org/article/1f4babddf3404e2e8db58ca641f1b75f
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:1f4babddf3404e2e8db58ca641f1b75f
record_format	dspace
spelling	oai:doaj.org-article:1f4babddf3404e2e8db58ca641f1b75f2021-11-24T09:20:58ZTHE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS2148-416310.9761/JASSS2470https://doaj.org/article/1f4babddf3404e2e8db58ca641f1b75f2019-08-01T00:00:00Zhttps://jasstudies.com/index.jsp?mod=tammetin&makaleadi=265814108_25-Dr.%20Vedat%20AVCI.pdf&key=27181https://doaj.org/toc/2148-4163In this study, distribution of landslides densely seen Karlıova Basin and surrounding is observed in accordance with elevation, slope, aspect and NDVI parts. Karlıova Basin is a tectonic origin depression which has begun to open between right-lateral strike-slip North Anatolian Fault (NAF), and left-lateral strike-slip, Eastern Anatolian Fault (EAF) in Kuvaterner. These faults have an important effect on formation and development of basin. The major effect is that high slopes are seen in intersection of the basin and mountainsides surrounding the basin and Karlıova Basin run parallel to the faults. The seismic-activity rate is very high in around the basin because of the effect of faulting. The lithology in Karlıova Basin and surrounding mostly consists of basaltic and tufa. That lithologic construction leads the basin to be more rainy, the landslides in Karlıova Basin to happen densely and high slope, seismic activity. The landslides are densely seen in Göynük Stream Valley and Kargapazarı Basin around the basin. Apart from these areas, they are densely seen in surrounding the basin due to tectonic and lithological formation. As it used to be in Göynük Stream Valley, the happening of the landslides accelerates along steep slopes where plant cover is weak and volcanites are broken by faults. The landslides directly affecting human activities like accommodation and transportation in Karlıova Basin and the surrounding have a deep effect. However, agriculture, range fields and drinkable water supply network of Bingöl City are affected negatively by the landslides per year. Morphology is constantly changing because of the landslides. Considering the seismic and tectonic formation of that area, the ongoing of these moves is indispensable. To decrease the probable harms of the landslides, it needs to construct the landslide susceptibility maps including the basin and surrounding. This study largely contributes to formation of the landslide susceptibility maps.Vedat AVCIHalil GÜNEKFırat UniversityarticlelandslSocial SciencesHSocial sciences (General)H1-99DEENFRTRJournal of Academic Social Science Studies , Vol 7, Iss 28, Pp 445-464 (2019)
institution	DOAJ
collection	DOAJ
language	DE EN FR TR
topic	landsl Social Sciences H Social sciences (General) H1-99
spellingShingle	landsl Social Sciences H Social sciences (General) H1-99 Vedat AVCI Halil GÜNEK THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS
description	In this study, distribution of landslides densely seen Karlıova Basin and surrounding is observed in accordance with elevation, slope, aspect and NDVI parts. Karlıova Basin is a tectonic origin depression which has begun to open between right-lateral strike-slip North Anatolian Fault (NAF), and left-lateral strike-slip, Eastern Anatolian Fault (EAF) in Kuvaterner. These faults have an important effect on formation and development of basin. The major effect is that high slopes are seen in intersection of the basin and mountainsides surrounding the basin and Karlıova Basin run parallel to the faults. The seismic-activity rate is very high in around the basin because of the effect of faulting. The lithology in Karlıova Basin and surrounding mostly consists of basaltic and tufa. That lithologic construction leads the basin to be more rainy, the landslides in Karlıova Basin to happen densely and high slope, seismic activity. The landslides are densely seen in Göynük Stream Valley and Kargapazarı Basin around the basin. Apart from these areas, they are densely seen in surrounding the basin due to tectonic and lithological formation. As it used to be in Göynük Stream Valley, the happening of the landslides accelerates along steep slopes where plant cover is weak and volcanites are broken by faults. The landslides directly affecting human activities like accommodation and transportation in Karlıova Basin and the surrounding have a deep effect. However, agriculture, range fields and drinkable water supply network of Bingöl City are affected negatively by the landslides per year. Morphology is constantly changing because of the landslides. Considering the seismic and tectonic formation of that area, the ongoing of these moves is indispensable. To decrease the probable harms of the landslides, it needs to construct the landslide susceptibility maps including the basin and surrounding. This study largely contributes to formation of the landslide susceptibility maps.
format	article
author	Vedat AVCI Halil GÜNEK
author_facet	Vedat AVCI Halil GÜNEK
author_sort	Vedat AVCI
title	THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS
title_short	THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS
title_full	THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS
title_fullStr	THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS
title_full_unstemmed	THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS
title_sort	distribution of active landslides in karliova basin and surrounding (bi̇ngöl) according to lithology, elevation, slope, inspection and ndvi parts
publisher	Fırat University
publishDate	2019
url	https://doaj.org/article/1f4babddf3404e2e8db58ca641f1b75f
work_keys_str_mv	AT vedatavci thedistributionofactivelandslidesinkarliovabasinandsurroundingbingolaccordingtolithologyelevationslopeinspectionandndviparts AT halilgunek thedistributionofactivelandslidesinkarliovabasinandsurroundingbingolaccordingtolithologyelevationslopeinspectionandndviparts AT vedatavci distributionofactivelandslidesinkarliovabasinandsurroundingbingolaccordingtolithologyelevationslopeinspectionandndviparts AT halilgunek distributionofactivelandslidesinkarliovabasinandsurroundingbingolaccordingtolithologyelevationslopeinspectionandndviparts
_version_	1718415339026382848

THE DISTRIBUTION OF ACTIVE LANDSLIDES IN KARLIOVA BASIN AND SURROUNDING (BİNGÖL) ACCORDING TO LITHOLOGY, ELEVATION, SLOPE, INSPECTION AND NDVI PARTS

Ejemplares similares