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Investigation of impact tsunamiites is particularly significant for global studies of the earth’s past; therefore, the present contribution is focused on this specific type, while ancient volcanism and slide-induced tsunamiites are not dealt with in detail. The occurrence of tsunamiites reflects the occurrence patterns in time of tsunamis, including the frequency of impact-induced tsunamis and the recurrence rate of earthquake-induced tsunamis. This may help to find out records of ancient tsunamis. For example, a high frequency of impact tsunamiites between 1.5 and 1.9 Ga is expected because of the meteorite-impact periodicity that has been proposed on the basis of impact craters. Earthquake-induced tsunamis reflect global and regional tectonics such as plume tectonics, plate-subduction tectonics and ridge subduction, and tend to occur with higher frequencies during sea-level rise than during sea-level fall. As far as studies of the pre-Quaternary are concerned, submarine tsunamiites are more important than the run-up tsunamiites on land, because of their preservation potential. It is suggested that the possibility is relatively high to find tsunamiites in bays and shallow seas. Tsunami-induced sediment gravity-flow deposits as those of the Mediterranean homogenite-type deposits may be found much more often in prehistorical and older sedimentary records than has previously been expected. 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