Analysis the morphometric features of KabirKooh landslide
The KabirKooh landslide was studied as one of the immediate catastrophic events which causes falling rocks from the KabirKooh hillside and the obstruction of the Seymarreh river course and also formed a lot of geomorphological shapes in this area. This landslide was located at 5 km of the Poldokhta...
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Language: | fas |
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Kharazmi University
2016-06-01
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Series: | تحقیقات کاربردی علوم جغرافیایی |
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Online Access: | http://jgs.khu.ac.ir/article-1-2652-en.pdf |
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description | The KabirKooh landslide was studied as one of the immediate catastrophic events which causes falling rocks from the KabirKooh hillside and the obstruction of the Seymarreh river course and also formed a lot of geomorphological shapes in this area. This landslide was located at 5 km of the Poldokhtar city at the south between the Ilam and Lorestan province. The main purpose of this research to provide and analyzie of Morphometric feature of the landslide inclusive, width of the rupture surface (), length of the displaced mass (), length of the rupturesurface(), width of the displaced mass (), the depth of the rupture surface (), the depth of the displaced mass to it will be discussed (),(/),(/), (/) and volume. For this work by using by using Global mapper11 software, to be conform the topographic area maps in the scale of 1/50000 and the digital elevation model. Arc Gis 9.3 and Surfer 10 software was used for preparing and producing new data and information. Considering the analyse of this indexs is, : equal to 15/5 ,: 16/06, :15.5,: 300 M,: 300 M, /:0.50, /:51.67, /:26.03 and volume 3908200970 . |
format | Article |
id | doaj-art-4fe3d09c944f4a21b141cd7da6040807 |
institution | Kabale University |
issn | 2228-7736 2588-5138 |
language | fas |
publishDate | 2016-06-01 |
publisher | Kharazmi University |
record_format | Article |
series | تحقیقات کاربردی علوم جغرافیایی |
spelling | doaj-art-4fe3d09c944f4a21b141cd7da60408072025-01-31T17:23:03ZfasKharazmi Universityتحقیقات کاربردی علوم جغرافیایی2228-77362588-51382016-06-0116413153Analysis the morphometric features of KabirKooh landslide012 The KabirKooh landslide was studied as one of the immediate catastrophic events which causes falling rocks from the KabirKooh hillside and the obstruction of the Seymarreh river course and also formed a lot of geomorphological shapes in this area. This landslide was located at 5 km of the Poldokhtar city at the south between the Ilam and Lorestan province. The main purpose of this research to provide and analyzie of Morphometric feature of the landslide inclusive, width of the rupture surface (), length of the displaced mass (), length of the rupturesurface(), width of the displaced mass (), the depth of the rupture surface (), the depth of the displaced mass to it will be discussed (),(/),(/), (/) and volume. For this work by using by using Global mapper11 software, to be conform the topographic area maps in the scale of 1/50000 and the digital elevation model. Arc Gis 9.3 and Surfer 10 software was used for preparing and producing new data and information. Considering the analyse of this indexs is, : equal to 15/5 ,: 16/06, :15.5,: 300 M,: 300 M, /:0.50, /:51.67, /:26.03 and volume 3908200970 .http://jgs.khu.ac.ir/article-1-2652-en.pdflandslidekabirkoohcatastrophicgeomorphic landformmorphometry. |
spellingShingle | Analysis the morphometric features of KabirKooh landslide تحقیقات کاربردی علوم جغرافیایی landslide kabirkooh catastrophic geomorphic landform morphometry. |
title | Analysis the morphometric features of KabirKooh landslide |
title_full | Analysis the morphometric features of KabirKooh landslide |
title_fullStr | Analysis the morphometric features of KabirKooh landslide |
title_full_unstemmed | Analysis the morphometric features of KabirKooh landslide |
title_short | Analysis the morphometric features of KabirKooh landslide |
title_sort | analysis the morphometric features of kabirkooh landslide |
topic | landslide kabirkooh catastrophic geomorphic landform morphometry. |
url | http://jgs.khu.ac.ir/article-1-2652-en.pdf |