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https://doi.org/10.5194/nhess-2020-87
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-2020-87
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
08 May 2020
| 08 May 2020
Status: this preprint has been withdrawn by the authors.
Effect of the Slope Angle and Its Classification on Landslide
Abstract. The phase after the determination of the landslide area in landslide susceptibility studies is the selection of methods and parameters to be used. Approximately 1500 randomly selected publications show that it is necessary to select a parameter based on the area. Research has shown that the parameter of slope is greatly preferred. There is nearly consensus of opinion among researchers regarding the use of the parameter. The research included the definition of slope made by different researchers, the advantages and disadvantages of the use of the parameter, different classifications that are used, the formation intervals of landslides, their use together with other parameters, and its effect on the formation of landslides. Classifications were studied based on the slope values at which landslides. Generally, automatic slope classifications are used in the preparation of landslide maps. There isn’t standard in parameter maps. Therefore, there isn’t class range that is referenced when preparing slope maps.
In this study, preferred class ranges and slope values where landslides occur were determined in the literature. 40 landslides area has been selected in Turkey. These were evaluated in the slope classes determined according to the literature. The results compared with the literature were found to be compatible.
This preprint has been withdrawn.
How to cite. Çellek, S.: Effect of the Slope Angle and Its Classification on Landslide, Nat. Hazards Earth Syst. Sci. Discuss. [preprint], https://doi.org/10.5194/nhess-2020-87, 2020.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Interactive discussion
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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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RC1: 'Review of the paper nhess-2020-87', Lorenzo Marchi, 13 May 2020
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AC1: 'Answer', Seda Çellek, 13 May 2020
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AC1: 'Answer', Seda Çellek, 13 May 2020
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RC2: 'Review', Anonymous Referee #2, 29 May 2020
Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
- Printer-friendly version
- Supplement
-
RC1: 'Review of the paper nhess-2020-87', Lorenzo Marchi, 13 May 2020
-
AC1: 'Answer', Seda Çellek, 13 May 2020
-
AC1: 'Answer', Seda Çellek, 13 May 2020
-
RC2: 'Review', Anonymous Referee #2, 29 May 2020
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Latest update: 02 May 2026
Seda Çellek
Department of Geology Engineering, Kırşehir Ahi Evran University, Kırşehir, 40100, Turkey
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Short summary
In this study, the slope parameter used in the preparation of landslide susceptibility maps has been studied in detail. With the extensive literature research, it was determined how the researchers used the parameter and the its class ranges. Class ranges in selected areas of Turkey was determined to compare with the literature. Thus a highly preferred parameter has been studied in detail.
In this study, the slope parameter used in the preparation of landslide susceptibility maps has...
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