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Thickness and grain-size distribution of Indian Ocean tsunami deposits distributed in the Khao Lak and Phra Thong Island, south-western Thailand, <b><i>in</i></b>: Shiki, T. <i>et al.</i> (Ed.) <i>Tsunamiites: features and implications.</i> pp. 123-132","BEntID":117672,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Shiki, T. <i>et al.</i> <i>Tsunamiites: features and implications.</i> pp. 123-132","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Fujino, S.; Naruse, H.; Suphawajruksakul, A.; Jarupangsakul, T.; Maruyama, M.; Ichihara, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Fujino, S. <i>et al.</i>","Englishabstract":"The landward changes in grain size and thickness of the 26 December 2004 Indian Ocean tsunami deposit on Phra Thong Island and in the Khao Lak Area, south-western Thailand, are summarized in this chapter. Themaximum heights of the tsunami on Phra Thong Island and Khao Lak were 7 and 10 m, respectively. The tsunami produced 1- to 4-m-high erosional scarps at the shoreline in these areas. The tsunami deposit is a sheet of sand ranging froma few centimetres to 22-cm thick over a distance of 1500 m inland. It thins near its distal margin, but the thickness is strongly affected by local topography and lacks a consistent trend. The deposit is composed ofmediumto very fine sand, and fines inland, reflecting loss of energy. It is graded or massive. Sets of graded units result from multiple waves. 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