TUTUILA ISLAND IS PART OF THE SAMOAN Archipelago (Figure 1), located in the South Pacific. On September 29, 2009 an 8.0-8.3 magnitude earthquake occurred close to 200 km SW of Tutuila in the Tonga Trench; it triggered a massive tsunami that killed more than 200 people. On Tutuila 34 people lost their lives, on ‘Upolu 183 died, and on Niuatoputapu 9 perished. Tutuila experienced at least three destructive waves, up to 17 m in height and reaching over 700 m inland in some areas. More than 20 villages on Tutuila sustained substantial damage. At least half of the houses were destroyed in villages located at the eastern and western ends of the islands, such as Tula, Poloa, ‘Aman-ave, Fagasā, Vatia and Āsili, among others. Beaches were heavily ...
International audienceThe pre-colonial history (i.e. before the 16th century) of Tonga and West Poly...
W.R. Dickinson, as part of his wide study of the geological history of the Pacific islands, has link...
Ocean-island flank collapses are amongst the most dangerous of all landslide related hazards in the ...
Multi-proxy studies of trench sediments from Futuna island, in the Wallis and Futuna archipelago, ha...
Multi-proxy studies of trench sediments from Futuna island, in the Wallis and Futuna archipelago, ha...
Tsunami investigation is a fundamental component of coastal hazard mitigation and risk reduction. Re...
The September 2009 South Pacific Tsunami (2009 SPT) in the Samoa Islands resulted in local public an...
International audienceExtensive bathymetric and two-dimensional seismic surveys have been carried ou...
Recent tsunamis worldwide have prompted significant efforts amongst scientific and disaster manageme...
An Mw ˜ 8.1 earthquake south of the Samoan Islands on 29 September 2009 generated a tsunami that kil...
The Komandorsky seismic gap has distinctive boundaries and a length of 650 km. Its period of “seismi...
The 1917 Samoa tsunamigenic earthquake is the largest historical event to impact this region. Over a...
International audienceThe pre-colonial history (i.e. before the 16th century) of Tonga and West Poly...
W.R. Dickinson, as part of his wide study of the geological history of the Pacific islands, has link...
Ocean-island flank collapses are amongst the most dangerous of all landslide related hazards in the ...
Multi-proxy studies of trench sediments from Futuna island, in the Wallis and Futuna archipelago, ha...
Multi-proxy studies of trench sediments from Futuna island, in the Wallis and Futuna archipelago, ha...
Tsunami investigation is a fundamental component of coastal hazard mitigation and risk reduction. Re...
The September 2009 South Pacific Tsunami (2009 SPT) in the Samoa Islands resulted in local public an...
International audienceExtensive bathymetric and two-dimensional seismic surveys have been carried ou...
Recent tsunamis worldwide have prompted significant efforts amongst scientific and disaster manageme...
An Mw ˜ 8.1 earthquake south of the Samoan Islands on 29 September 2009 generated a tsunami that kil...
The Komandorsky seismic gap has distinctive boundaries and a length of 650 km. Its period of “seismi...
The 1917 Samoa tsunamigenic earthquake is the largest historical event to impact this region. Over a...
International audienceThe pre-colonial history (i.e. before the 16th century) of Tonga and West Poly...
W.R. Dickinson, as part of his wide study of the geological history of the Pacific islands, has link...
Ocean-island flank collapses are amongst the most dangerous of all landslide related hazards in the ...