The Sunda megathrust : past, present and future

After lying dormant for about a thousand years, sudden slippage of a 1600-km long section of the Sunda megathrust fault caused uplift of the seafloor between Aceh and Myanmar, resulting in a great earthquake and the horrific Indian Ocean tsunami of 2004. Three months later and just to the s...

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Bibliographic Details
Main Author: Sieh, Kerry
Format: Journal Article
Language:English
Published: 2012
Subjects:
Online Access:https://hdl.handle.net/10356/94170
http://hdl.handle.net/10220/8663
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author Sieh, Kerry
author_facet Sieh, Kerry
author_sort Sieh, Kerry
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description After lying dormant for about a thousand years, sudden slippage of a 1600-km long section of the Sunda megathrust fault caused uplift of the seafloor between Aceh and Myanmar, resulting in a great earthquake and the horrific Indian Ocean tsunami of 2004. Three months later and just to the south, sudden slippage of a 350-km length of the megathrust beneath Simeulue and Nias islands caused another destructive great earthquake and lesser tsunami. Because it takes centuries for tectonic strains to build up again after such big earthquakes, these two events are unlikely to recur within the next hundred years. Farther south, however, offshore West Sumatra and Bengkulu provinces, another great earthquake and tsunami will likely occur within the next few decades. We are trying to characterize that future earthquake and tsunami, to encourage and to focus preparations for and mitigation of the coming disaster. Similar efforts need to be initiated throughout much of south and southeast Asia, if the disastrous effects of future large earthquakes and tsunamis are to be mitigated.
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spelling ntu-10356/941702020-03-07T12:45:24Z The Sunda megathrust : past, present and future Sieh, Kerry DRNTU::Science::Geology::Volcanoes and earthquakes After lying dormant for about a thousand years, sudden slippage of a 1600-km long section of the Sunda megathrust fault caused uplift of the seafloor between Aceh and Myanmar, resulting in a great earthquake and the horrific Indian Ocean tsunami of 2004. Three months later and just to the south, sudden slippage of a 350-km length of the megathrust beneath Simeulue and Nias islands caused another destructive great earthquake and lesser tsunami. Because it takes centuries for tectonic strains to build up again after such big earthquakes, these two events are unlikely to recur within the next hundred years. Farther south, however, offshore West Sumatra and Bengkulu provinces, another great earthquake and tsunami will likely occur within the next few decades. We are trying to characterize that future earthquake and tsunami, to encourage and to focus preparations for and mitigation of the coming disaster. Similar efforts need to be initiated throughout much of south and southeast Asia, if the disastrous effects of future large earthquakes and tsunamis are to be mitigated. 2012-09-28T03:44:49Z 2019-12-06T18:51:58Z 2012-09-28T03:44:49Z 2019-12-06T18:51:58Z 2007 2007 Journal Article Sieh, K. (2007). The Sunda megathrust : past, present and future. Journal of Earthquake and Tsunami, 01(01), 1-19. https://hdl.handle.net/10356/94170 http://hdl.handle.net/10220/8663 10.1142/S179343110700002X en Journal of earthquake and tsunami © 2007 World Scientific Publishing Company.
spellingShingle DRNTU::Science::Geology::Volcanoes and earthquakes
Sieh, Kerry
The Sunda megathrust : past, present and future
title The Sunda megathrust : past, present and future
title_full The Sunda megathrust : past, present and future
title_fullStr The Sunda megathrust : past, present and future
title_full_unstemmed The Sunda megathrust : past, present and future
title_short The Sunda megathrust : past, present and future
title_sort sunda megathrust past present and future
topic DRNTU::Science::Geology::Volcanoes and earthquakes
url https://hdl.handle.net/10356/94170
http://hdl.handle.net/10220/8663
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