Abstract

The purposes of this study is to create a landslide susceptibility map (LSM) for Lompobattang Mountain area in Indonesia. The foot of the Lompobattang Mountain area suffered flash flood and landslides in 2006, which led to significant adverse impact on the nearby settlements. There were 158 identified landslides covering a total area of 3.44 km2. Landslide inventory data were collected using google earth image interpretations. The landslide inventories were prepared out of the past landslide events, and future landslide occurrence was predicted by correlating landslide causal factors. In this study landslide inventories were divided into landslide data for training and landslide data for validation. The LSM was prepared by Frequency Ratio (FR) and Logistic Regression (LR) statistical methods. Lithology, distance from the road, distance from the river, distance from the fault, land use, curvature, aspect, and slope degree were used as conditioning parameters. Area under the curve (AUC) of the Receiver Operating Characteristic (ROC) was used to check the performance of the models. In the analysis, the FR model results in 85.8 % accuracy in the AUC success rate while the LR model was found to have 86.9 % accuracy. However, the accuracy of both these models in AUC predictive rate is the same at around 85.1 %. The LR model is 6.34 % higher than the FR model in comparison to its accuracy for ratio of landslide validation. The landslide susceptibility map consist of the predicted landslide area, hence it can be used to reduce the potential hazard associated with the landslides in this study area.

Highlights

  • Earthquakes, intense rainfall, and snowmelt are general triggering factors of landslides

  • The application of frequency ratio The frequency ratio method was used to find the correlation between landslide locations in the past and each factor that affects landslides

  • Besides creating landslide susceptibility maps, this research shows the performance of Frequency Ratio (FR) and Logistic Regression (LR) models as well

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Summary

Introduction

Earthquakes, intense rainfall, and snowmelt are general triggering factors of landslides. Other factors can be geology, land cover, slope geometry, solar radiation, surface and subsurface hydrology, and human activities. In Indonesia, landslides are serious problem that cause debris flow or flash flood disasters every year during or after heavy rainfalls. During 2005 to 2014, around 1926 landslide events were reported which resulted in loss of 1035 human casualties and 853 disappearance, and in Landslide susceptibility, hazard and risk zoning are parts of landuse planning. As first stage of landslide hazard mitigation, landslide susceptibility mapping must provide important information to support decisions for urban development, which considerably reduces potential landslide damage. Landslide susceptibility maps are produced to help humans to recognize and adapt to landslide hazard mitigation procedures (Pourghasemi et al 2012)

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