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Indonesia landslide death toll climbs to 25 as dozens still missing WEST JAVA, INDONESIA - JANUARY 26 : An aerial view of a landslide that buried dozens of houses and plantations, leaving dozens of victims, that occurred at around 2 a.m. on Saturday (January 24) in Bandung Regency, West Java, Indonesia, photographed on January 26, 2026. The landslide was caused by heavy rain, and landslide activity upstream along the slope formed a natural dam, blocking the flow of water and sediment until it eventually broke, triggering a flow of mud mixed with sand, rocks and wood downstream. As a result, the affected homes were not damaged at the landslide site itself, but by the debris carried downstream through the river channel. Dasril Roszandi Anad

Indonesia landslide death toll climbs to 25 as dozens still missing WEST JAVA, INDONESIA - JANUARY 26 : An aerial view of a landslide that buried dozens of houses and plantations, leaving dozens of victims, that occurred at around 2 a.m. on Saturday (January 24) in Bandung Regency, West Java, Indonesia, photographed on January 26, 2026. The landslide was caused by heavy rain, and landslide activity upstream along the slope formed a natural dam, blocking the flow of water and sediment until it eventually broke, triggering a flow of mud mixed with sand, rocks and wood downstream. As a result, the affected homes were not damaged at the landslide site itself, but by the debris carried downstream through the river channel. Dasril Roszandi Anad

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Credit: Anadolu Agency

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Recording Date: Jan 26, 2026

Media Size: 5,000×3,391 Pixels

Indonesia landslide death toll climbs to 25 as dozens still missing WEST JAVA, INDONESIA - JANUARY 26 : An aerial view of a landslide that buried dozens of houses and plantations, leaving dozens of victims, that occurred at around 2 a.m. on Saturday (January 24) in Bandung Regency, West Java, Indonesia, photographed on January 26, 2026. The landslide was caused by heavy rain, and landslide activity upstream along the slope formed a natural dam, blocking the flow of water and sediment until it eventually broke, triggering a flow of mud mixed with sand, rocks and wood downstream. As a result, the affected homes were not damaged at the landslide site itself, but by the debris carried downstream through the river channel. Dasril Roszandi Anad

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