Analysis of Factors Determining Landslide Disaster Evacuation Routes in Cipongkor District, West Bandung Regency, West Java
DOI:
https://doi.org/10.33332/jgsm.geologi.v27i1.12891Keywords:
disaster mitigation, evacuation routes, safety, gathering points, West BandungAbstract
West Bandung is a region in Indonesia that is prone to landslides, floods, and other hydrometeorological disasters. The local government has taken measures to reduce the impacts of natural disasters by issuing early warnings and establishing disaster response teams. The National Disaster Management Agency (BNPB) has strengthened community-based early warning systems to enhance the capacity of communities to respond to natural disasters. This study aims to identify alternatives for disaster mitigation in the form of evacuation routes that are safe and easily accessible for the community. The methods used in this research include identifying potential locations, mapping potential evacuation routes, classifying routes based on safety and ease of access, evaluating the mapped routes using spatial analysis, and determining the final evacuation routes. Based on the results of the study, which considered hazard-prone areas, morphological conditions, and access from residential areas, two locations were designated as gathering points and several evacuation routes were identified for use. The nearest disaster-prone areas around the settlements are located approximately 5 km away and consist of two landslide-prone zones situated to the southeast and northwest. Two gathering points were designated from the mapping, with a total area of 500 m². The distance from the residential area to the farthest gathering point can be reached in about 10 minutes (740 m), while the nearest can be reached in about 4 minutes (290 m). The main factors in determining geological disaster evacuation routes in Cipongkor include the spatial distribution of settlements, the distance between hazard- prone areas and settlements, the morphological conditions of the disaster area, and the geological characteristics of the bedrock in hazard-prone zones. The morphology of the hazard-prone area is moderately undulating (45%) in the northwest and steeply undulating (55%) in the southeast, while the community is relatively widely dispersed, with about 38% of residents living in the northeast and 62% in the southwest.
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