Penultimate predecessors of the 2004 Indian Ocean tsunami in Aceh, Sumatra: Stratigraphic, archeological, and historical evidence

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Kerry Sieh, Patrick Daly, E. Edwards McKinnon, Jessica E. Pilarczyk, Hong-Wei Chiang, Benjamin Horton, Charles M. Rubin, Chuan-Chou Shen, Nazli Ismail, Christopher H. Vane, R. Michael Feener

2015 Journal of Geophysical Research: Solid Earth Vol. 120 Issue 1 Article Cited by 58 SDG 13SDG 17 Quartile

Abstract

We present stratigraphic, archeological and historical evidence for two closely timed predecessors of the giant 2004 tsunami on the northern coast of Aceh, northern Sumatra. This is the first direct evidence that a tsunami played a role in a fifteenth century cultural hiatus along the northern Sumatran portion of the maritime silk route. One seacliff exposure on the eastern side of the Lambaro headlands reveals two beds of tsunamigenic coral rubble within a small alluvial fan. Radiocarbon and Uranium-Thorium disequilibrium dates indicate emplacement of the coral rubble after 1344 ± 3 C.E. Another seacliff exposure, on the western side of the peninsula, contains evidence of nearly continuous settlement from ∼1240 C.E. to soon after 1366 ± 3 C.E., terminated by tsunami destruction. At both sites, the tsunamis are likely coincident with sudden uplift of coral reefs above the Sunda megathrust 1394 ± 2 C.E., evidence for which has been published previously. The tsunami (or tsunami pair) appears to have destroyed a vibrant port community and led to the temporary recentering of marine trade dominance to more protected locations farther east. The reestablishment of vibrant communities along the devastated coast by about 1500 CE set the stage for the 2004 disaster. ©2014. The Authors.

Affiliations

Earth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore; National University of Singapore, University Town, Singapore, Singapore; Archaeology Unit, Institute of Southeast Asian Studies, Singapore, Singapore; Institute of Marine and Coastal Science, Rutgers University, New Brunswick, NJ, United States; Institute of Earth, Ocean, and Atmospheric Sciences, Rutgers University, New Brunswick, NJ, United States; Department of Geosciences, National Taiwan University, Taipei, Taiwan; Department of Physics/Geophysics, Faculty of Mathematic and Natural Sciences, Syiah Kuala University, Banda Aceh, Indonesia; Centre for Environmental Geochemistry, British Geological Survey, Nottingham, United Kingdom; Asia Research Institute, National University of Singapore, Singapore, Singapore

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