Tsunami & Coastal Hazards
The vast majority of tsunamis impacting Indonesia are 'near-field' local events where the destructive wave crest strikes the shoreline within 10 to 30 minutes following the triggering rupture. Tsunamis can be spawned by thrust-fault undersea megathrust earthquakes, submarine canyon collapses (as observed in Palu Bay in 2018), or island volcano flank collapses into the sea (such as Anak Krakatau in the Sunda Strait in 2018). The initial wave is rarely the largest; subsequent waves arriving over several hours are often significantly higher and carry enormous kinetic energy.