Natural Hazards

, Volume 46, Issue 3, pp 323–351 | Cite as

Implementation of reconstructed geomorphologic units in landslide susceptibility mapping: the Melen Gorge (NW Turkey)

  • T. Gorum
  • B. Gonencgil
  • C. Gokceoglu
  • H. A. Nefeslioglu
Original Paper

Abstract

In the international literature, although considerable amount of publications on the landslide susceptibility mapping exist, geomorphology as a conditioning factor is still used in limited number of studies. Considering this factor, the purpose of this article paper is to implement the geomorphologic parameters derived by reconstructed topography in landslide susceptibility mapping. According to the method employed in this study, terrain is generalized by the contours passed through the convex slopes of the valleys that were formed by fluvial erosion. Therefore, slope conditions before landsliding can be obtained. The reconstructed morphometric and geomorphologic units are taken into account as a conditioning parameter when assessing landslide susceptibility. Two different data, one of which is obtained from the reconstructed DEM, have been employed to produce two landslide susceptibility maps. The binary logistic regression is used to develop landslide susceptibility maps for the Melen Gorge in the Northwestern part of Turkey. Due to the high correct classification percentages and spatial effectiveness of the maps, the landslide susceptibility map comprised the reconstructed morphometric parameters exhibits a better performance than the other. Five different datasets are selected randomly to apply proper sampling strategy for training. As a consequence of the analyses, the most proper outcomes are obtained from the dataset of the reconstructed topographical parameters and geomorphologic units, and lithological variables that are implemented together. Correct classification percentage and root mean square error (RMSE) values of the validation dataset are calculated as 86.28% and 0.35, respectively. Prediction capacity of the different datasets reveal that the landslide susceptibility map obtained from the reconstructed parameters has a higher prediction capacity than the other. Moreover, the landslide susceptibility map obtained from the reconstructed parameters produces logical results.

Keywords

Landslide susceptibility Topographic reconstruction Indirect mapping methods GIS Geomorphology Melen Gorge (Turkey) 

Notes

Acknowledgment

We would like to extend our cordial thanks to S. Cigdem Erdogan (Head of Elective Foreign Languages Department) for her contribution to the improvement of the language of the paper.

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Copyright information

© Springer Science+Business Media B.V. 2008

Authors and Affiliations

  • T. Gorum
    • 1
  • B. Gonencgil
    • 2
  • C. Gokceoglu
    • 3
  • H. A. Nefeslioglu
    • 4
  1. 1.Natural Sciences Research CenterYildiz Technical UniversityIstanbulTurkey
  2. 2.Department of Geography, Faculty of LettersIstanbul UniversityIstanbulTurkey
  3. 3.Department of Geological Engineering, Applied Geology DivisionHacettepe UniversityAnkaraTurkey
  4. 4.Department of Geological ResearchGeneral Directorate of Mineral Research and ExplorationAnkaraTurkey

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