Journal
GEOENVIRONMENTAL DISASTERS
Volume 8, Issue 1, Pages -Publisher
SPRINGERNATURE
DOI: 10.1186/s40677-020-00170-y
Keywords
Landslide; Susceptibility; Geographic information system (GIS); Certainty factor; Frequency ratio; Information value; Ethiopia
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Uatzau basin in northwestern Ethiopia is prone to landslides, and a landslide susceptibility mapping study was conducted using GIS-based frequency ratio, information value, and certainty factor methods. The study identified six factors affecting landslides and categorized the area into different susceptibility classes. Results showed high accuracy in identifying landslide-prone zones. The statistical methods used in this study can be recommended for landslide susceptibility mapping and regional land use planning for landslide hazard mitigation.
Uatzau basin in northwestern Ethiopia is one of the most landslide-prone regions, which characterized by frequent high landslide occurrences causing damages in farmlands, non-cultivated lands, properties, and loss of life. Preparing a Landslide susceptibility mapping is imperative to manage the landslide hazard and reduce damages of properties and loss of lives. GIS-based frequency ratio, information value, and certainty factor methods were applied. The landslide inventory map was prepared from detailed fieldwork and Google Earth imagery interpretation. Thus, 514 landslides were mapped, and out of which 359 (70%) of landslides were randomly selected keeping their spatial distribution to build landslide susceptibility models, while the remaining 155 (30%) of the landslides were used to model validation. In this study, six factors, including lithology, land use/cover, distance to stream, slope gradient, slope aspect, and slope curvature were evaluated. The effects of the landslide factor of slope instability were determined by comparing with landslide inventory raster using the GIS environment. The landslide susceptibility maps of the Uatzau area were categorized into very low, low, moderate, high and very high susceptibility classes. The landslide susceptibility maps of the three models validated by the ROC curve. The results for the area under the curve (AUC) are 88.83% for the frequency ratio model, 87.03% for certainty factor, and 84.83% of information value models, which are indicating very good accuracy in the identification of landslide susceptibility zones of a region. From these resulted maps, it is possible to recommend, the statistical methods (Frequency Ratio, Information Value, and Certainty Factor Methods) are adequate to landslide susceptibility mapping. The landslide susceptibility maps can be used for regional land use planning and landslide hazard mitigation purposes.
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