Earthquake-induced landslides
Earthquake-induced landslides occur when strong ground shaking during an earthquake destabilizes slopes or cliffs, causing soil, rocks, and debris to slide downhill. This can happen in hilly or mountainous areas where the ground is steep. The shaking can weaken the structure of the earth, especially if it's already loose or saturated with water. Landslides can cause significant damage, bury structures, and pose a risk to life and property by blocking roads and rivers. Understanding this phenomenon helps in planning and mitigating risks in earthquake-prone regions.
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Earthquake-induced landslides occur when the shaking from an earthquake destabilizes slopes and causes soil, rock, or debris to move downhill. The intense vibrations can weaken the ground, especially if it's wet or steep, leading to sudden collapses. These landslides can vary in size, from small mudslides to massive rockfalls, posing hazards to people, buildings, and infrastructure. They are particularly common in mountainous or hilly areas. Understanding these risks helps in planning and reducing damage during seismic events.