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<p><strong>Abstract.</strong> The 2004 Indian Ocean Tsunami and the 2011 Great East Japan earthquake and tsunami caused large-scale topographic changes in coastal areas. Whereas much research has focused on coastlines that have or had large human populations, little focus has been paid on coastlines that have little or no infrastructure. The importance of examining erosional and depositional mechanisms of tsunami events lies in the rapid reorganisation that coastlines must undertake immediatelydoi:10.5194/nhess-2019-263 fatcat:hkq7wnhmm5ebrdx6r4gyh54uk4