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Keywordshazard assessment; impulse wave; landslide; landslide tsunami; physical modelling; wave generation; submarine seismic source; submarine mass failure; triggering event; sources interactions; long- and short-term hazard; Naples-Ischia; PTHA; hydraulics; impulse product parameter; impulse wave; physical modeling; subaerial landslide; water wave; Biblical Exodus; tsunamis; numerical modelling; sea parting; Reed Sea; tsunami on land flow; flow-structure interaction; vortex shedding; drag force; inertia force; tsunami; vulnerability; hazard; urban environment; GIS procedure; Napoli city; ADDS; ASSS; tsunamigenic earthquake; tsunami magnitude; seismic tsunami; gravity wave; ionosphere; electron density; electric field; total electron content (or TEC); tsunami; San Diego; port modificationsdamages.; tsunami; Baja California; event deposit; coastal hazards; long wave; tsunami run-up; pump-driven wave generator; discontinuous Galerkin model; shallow water equations; seismic tsunami; gravity wave; nonisothermality; wind shears
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