Landslide susceptibility analysis using decision tree method, Phidim, Eastern Nepal

Authors

  • Chandra Prakash Poudyal Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu

DOI:

https://doi.org/10.3126/bdg.v15i0.7419

Keywords:

Landslide Susceptibility, GIS, Decision Tree, Nepal

Abstract

The decision tree is one of the new methods used for the determination of landslide susceptibility in the study area. The Phidim area is selected for the application of this method. The total surface area is 168.07 sq. km, and is located at the eastern part of Nepal. There are total of 10 different data bases used for this study which are; geological formation, elevation, slope, curvature, aspect, stream power index, topographic wetness index, distance from drainage, lineaments, and slope length, and are considered as landslide conditioning factors. Geographical information system (GIS) is used as basic tools and ARC/View is used for the processing data analysis and final map preparation. For the decision tree analysis the PASW 18 (statistical tool) is used to generate values of each factor. According to the results of decision tree, two geological formations; stream power index and slope are found as the most effective parameters on the landslide occurrence in the study area. Using the predicted values, the landslide susceptibility map of the study area is produced. To assess the performance of the produced susceptibility map, the area under curve (AUC) is drawn. The AUC value of the produced landslide susceptibility map has been obtained as 95.9%. According to the results of the AUC evaluation, the produced map has showed a good performance. As to wrap up, the produced map is able to be used for medium scaled and regional planning purposes.

DOI: http://dx.doi.org/10.3126/bdg.v15i0.7419

Bulletin of the Department of Geology, Vol. 15, 2012, pp. 69-76

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Published

2013-01-21

How to Cite

Poudyal, C. P. (2013). Landslide susceptibility analysis using decision tree method, Phidim, Eastern Nepal. Bulletin of the Department of Geology, 15, 69–76. https://doi.org/10.3126/bdg.v15i0.7419

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