Abstract The tectonic/lithospheric plates of the Indo-Australian and the Eurasian meet near Kulon Progo Regency, which faces the Indian Ocean. Large earthquakes that could produce tsunami waves could be caused by the plate. The Kulon Progo Regency is situated exactly next to the Indian Ocean, 225 kilometres away from the subduction zone. The coastline of the regency stretches for 24 kilometres, making the coastal region there hazard to tsunami disasters. In order to predict when tsunami waves will reach the region’s shoreline and gauge the level of tsunami risk based on inundation or immersion of tsunami waves, this study simulates probable tsunamis in Kulon Progo Regency. TUNAMI, is a programme used for tsunami modelling. The TUNAMI programme is run using Fortran programming discussion with Microsoft Developer Studio software. The method used in this study is a numerical method with TUNAMI-F1 and TUNAMI-N3 software. The study’s findings demonstrated that the expected wave arrival time from the moment of wave creation to the Kulon Progo shoreline area was thirty minutes for tsunami waves generated by an 8.9 Mw megathrust earthquake. The majority of Kulon Progo Regency’s coastal areas are low to moderately dangerous, only areas that border the shoreline and the western coastal section of the regency have high levels of tsunami hazard.
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