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• W3046325406 abstract "Sediments are archives that aid in the reconstruction of overwash processes. For onshore tsunami deposits, sedimentary structures provide information regarding the flow characteristics at a particular site. The spatial distribution of sediments allows for an estimation of the minimum inundation distance, and structures that document flow direction (e.g., cross-stratification, imbrication) may provide evidence of runup or backwash phases of individual tsunami waves. Multiple layers may indicate single waves of the tsunami wave train. Flow conditions (i.e., upper or lower flow regime) that prevail during the overwash process are represented by features such as antidunes and planar lamination. Transport modes (i.e., bed load or suspended load) and related modes of deposition and settling are revealed by structures, such as normal grading and mud caps. In general, tsunami deposits are highly variable in their appearance as they contain components from marine and terrestrial sources. Finally, as the geological record reaches beyond the limit of any historical documentation, sediments are fundamental archives for long-term risk assessment." @default.
• W3046325406 created "2020-08-07" @default.
• W3046325406 creator A5071557990 @default.
• W3046325406 date "2020-01-01" @default.
• W3046325406 modified "2023-10-13" @default.
• W3046325406 title "The sedimentology and geometry of fine-grained tsunami deposits from onshore environments" @default.
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• W3046325406 doi "https://doi.org/10.1016/b978-0-12-815686-5.00011-0" @default.
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