Residents of a village in Sancheong-eup are preparing for the return of the monsoon season while recovery work from a deadly landslide remains unfinished [1].

The situation highlights the vulnerability of rural South Korean communities to extreme weather and the slow pace of infrastructure reinforcement required to prevent future tragedies.

The landslide occurred during heavy rains in 2023, when saturated slopes gave way and buried several homes [1]. The disaster resulted in the deaths of four villagers [1]. Approximately one year has passed since the event, and the community is now navigating the psychological and physical aftermath as the next rainy season arrives [1].

Local authorities have implemented several engineering measures to stabilize the area. These include the construction of stone-step walls and a "sabang dam," a specialized structure designed to control erosion and block debris from flowing downstream [1]. While some of these projects are complete, other sites remain under construction [1].

Village chief Noh Myeong-su said the experience has left residents highly sensitive to weather forecasts [1]. He said that while the fear remains, there is a sense of hope that the new protections will offer better security than the village had before the disaster [1].

According to reports, the remaining construction work is targeted for completion by next month [1]. Until those projects are finalized, residents must rely on the partially completed defenses to protect their homes from potential new landslides during the current monsoon period [1].

The landslide occurred during heavy rains in 2023, when saturated slopes gave way and buried several homes.

The delay in completing critical slope stabilization and debris-control structures before the onset of the monsoon season underscores a recurring gap in disaster preparedness. As climate patterns shift toward more intense rainfall, the reliance on traditional 'sabang dams' and stone walls may be insufficient if construction timelines do not outpace the increasing frequency of extreme weather events in mountainous regions.