The tsunami triggered by the 24 June 2026 Venezuela earthquakes: tectonic context and tsunami modelling
This paper analyzes the June 24, 2026, Venezuela earthquake and its resulting tsunami by demonstrating that while finite-fault numerical models successfully reproduce regional waveforms, the significant discrepancy between simulated and observed local amplitudes suggests that factors such as coastal effects, grid resolution limits, or a submarine landslide likely contributed to the event's intensity.