en-ENΕditor: K.N.K.]]>Editor: K.N.K.]]>Editor: K.N.K.   Κ.Ν.Κ.]]>Editor: K.N.K.]]>Editor: K.N.K.]]> Editor: K.N.K.]]>Editor: K.N.K.]]>Editor: K.N.K.]]>1 km2) lateral area. The presence of this deposit is evidence that tsunami waves from the Santorini eruption radiated throughout the Eastern Mediterranean Sea, affecting the coastal people living there. Dates for the tsunami deposit bracket both the so-called "high" and "low" chronology for the Santorini eruption. In addition to resolving the question of the extent of tsunami impact from the Santorini eruption, the research presented also provides a new means of discovering, identifying, and studying continuous records of paleotsunami deposits in the upper shelf coastal environment. The latter is key to understanding past events, better interpreting sedimentological records, and creating stronger models for understanding tsunami propagation, coastal management, and hazard preparation worldwide. Sources: http://geology.gsapubs.org, http://www.msnbc.msn.com Writer: Κ.Ν.Κ.]]>