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Geological subsidence and sinking islands: the case of Manono (Samoa)

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dc.date.accessioned 2021-12-10T03:00:28Z
dc.date.available 2021-12-10T03:00:28Z
dc.date.issued 2016
dc.identifier.citation DOI: 10.1002/arco.5099 en_US
dc.identifier.uri ${sadil.baseUrl}/handle/123456789/1651
dc.description 10 pages : PDF en_US
dc.description.abstract W.R. Dickinson, as part of his wide study of the geological history of the Pacific islands, has linked the unique case of the deeply submerged Lapita site of Mulifanua in western Upolu (Samoa) to the slow subsidence of Upolu island. Recent archaeological research on the neighbouring small island of Manono has yielded new and detailed data on this geological process. A series of new dates has allowed us to define the speed of the subsidence and demonstrate the massive environmental changes to which the local population has had to adapt over the past 2000 years. en_US
dc.language.iso en en_US
dc.publisher Archaeology in Oceania, en_US
dc.relation.ispartofseries Volume 51;
dc.subject geological subsidence, Samoa, Manono island, Pagai, resilience, intensification en_US
dc.title Geological subsidence and sinking islands: the case of Manono (Samoa) en_US
dc.type Article en_US


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