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Earthquake Landslides
Earthquake-triggered landslides turn shaking, steep slopes, fractured rock, saturated soil, roads, rivers and aftershocks into a ground-failure hazard that can cut off communities after the shaking stops.
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Brief text
Earthquake-triggered landslides turn shaking, steep slopes, fractured rock, saturated soil, roads, rivers and aftershocks into a ground-failure hazard that can cut off communities after the shaking stops.
- Frame 1Indonesia quake turns steep wet slopes into landslide risk for residents, roads, rescue crews.
- Frame 2A slope fails when shaking and rain push soil past its strength threshold.
- Frame 3Hazard teams map the data path: shaking intensity, slope angle, soil, water, exposed roads.
- Frame 4Slides can cut roads, bury homes, block rivers and build unstable landslide dams.
- Frame 5Liquefaction routes saturated ground into a flow when shaking lowers soil strength.
- Frame 6Aftershocks, rainfall, satellite scars, blocked valleys, road closures and alerts become watch signals.
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- Published
- Aug 16, 12:40 PM EDT
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