TY - JOUR
T1 - Palaeotsunamis in the Pacific Islands
AU - Goff, James
AU - Chagué-Goff, Catherine
AU - Dominey-Howes, Dale
AU - McAdoo, Brian
AU - Cronin, Shane
AU - Bonté-Grapetin Michael, M.
AU - Nichol, Scott
AU - Horrocks, Mark
AU - Cisternas, Marco
AU - Lamarche, Geoffroy
AU - Pelletier, Bernard
AU - Jaffe, Bruce
AU - Dudley, Walter
PY - 2011/7
Y1 - 2011/7
N2 - The recent 29 September 2009 South Pacific and 27 February 2010 Chilean events are a graphic reminder that the tsunami hazard and risk for the Pacific Ocean region should not be forgotten. Pacific Islands Countries (PICs) generally have short (<150 years) historic records, which means that to understand their tsunami hazard and risk researchers must study evidence for prehistoric events. However, our current state of knowledge of palaeotsunamis in PICs as opposed to their circum-Pacific counterparts is minimal at best. We briefly outline the limited extent of our current knowledge and propose an innovative methodology for future research in the Pacific. Each PIC represents a point source of information in the Pacific Ocean and this would allow their palaeotsunami records to be treated akin to palaeo-DART® (Deep-ocean Assessment and Reporting of Tsunamis) buoys. Contemporaneous palaeotsunamis from local, regional and distant sources could be identified by using the spatial distribution of island records throughout the Pacific Ocean in conjunction with robust event chronologies. This would be highly innovative and, more importantly, would help provide the building blocks necessary to achieve more meaningful disaster risk reduction for PICs.
AB - The recent 29 September 2009 South Pacific and 27 February 2010 Chilean events are a graphic reminder that the tsunami hazard and risk for the Pacific Ocean region should not be forgotten. Pacific Islands Countries (PICs) generally have short (<150 years) historic records, which means that to understand their tsunami hazard and risk researchers must study evidence for prehistoric events. However, our current state of knowledge of palaeotsunamis in PICs as opposed to their circum-Pacific counterparts is minimal at best. We briefly outline the limited extent of our current knowledge and propose an innovative methodology for future research in the Pacific. Each PIC represents a point source of information in the Pacific Ocean and this would allow their palaeotsunami records to be treated akin to palaeo-DART® (Deep-ocean Assessment and Reporting of Tsunamis) buoys. Contemporaneous palaeotsunamis from local, regional and distant sources could be identified by using the spatial distribution of island records throughout the Pacific Ocean in conjunction with robust event chronologies. This would be highly innovative and, more importantly, would help provide the building blocks necessary to achieve more meaningful disaster risk reduction for PICs.
KW - Pacific Island Countries
KW - Palaeotsunami
KW - Risk
KW - Sources
UR - http://www.scopus.com/inward/record.url?scp=79958865981&partnerID=8YFLogxK
U2 - 10.1016/j.earscirev.2010.10.005
DO - 10.1016/j.earscirev.2010.10.005
M3 - Review article
AN - SCOPUS:79958865981
SN - 0012-8252
VL - 107
SP - 141
EP - 146
JO - Earth-Science Reviews
JF - Earth-Science Reviews
IS - 1-2
ER -