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Seismic and landslide source of the 1908 Straits of Messina tsunami(Sicily, Italy)

机译:1908年墨西拿海啸海峡的地震和滑坡源(意大利西西里岛)

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摘要

One hundred years ago (December 1908) a devastatingtsunami associated with an earthquake struck the Straitsof Messina area, causing many casualties. On the basis ofseismic data and observed runups and arrival times, wesuggest that the tsunami was likely generated by coseismicseafloor displacement coupled with a small submarinelandslide triggered by the earthquake. Backwards ray-tracing using a depth-dependent velocity field, submarineslope analysis and inferences form the main drainagenetwork allowed us To identify possible locations for thesource of the submarine landslide. We then performeddirect simulations of tsunamis generated by the earthquakeand landslides and identified the tsunami source(earthquake plus landslide) that best fits observationaldata in a small volume submarine landslide (1-5 km3)located offshore Nizza, Sicily.
机译:一百年前(1908年12月),与地震相关的毁灭性海啸袭击了墨西拿海峡地区,造成许多人员伤亡。根据地震数据以及观测到的上升和到达时间,我们建议海啸可能是由同震海底位移加上地震引发的海底小滑坡引起的。使用与深度有关的速度场进行向后的射线跟踪,形成主要的排水网络的海底斜坡分析和推论使我们能够确定海底滑坡源的可能位置。然后,我们对地震和滑坡产生的海啸进行了直接模拟,并确定了最适合西西里岛尼扎(Nizza)近海小体积海底滑坡(1-5 km3)的观测数据的海啸源(地震加滑坡)。

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