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Publications tagged with [tsunami]

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<p>Thin coastal dykes typically found in developing countries may suddenly collapse due to rapid land subsidence, material ageing, sea-level rise, high wave attack, earthquakes, landslides, or a collision with vessels. Such a failure could trigger dam-break ...
Reference: Nat. Hazards Earth Syst. Sci., 16, 1629–1638, 2016
Tectonic deformation from the 2010 Maule (Chile) Mw 8.8 earthquakeincluded both uplift and subsidence along about 470 km of the central Chilean coast. In the south, deformation included as much as 3 m of uplift of the Arauco Peninsula, which produced emergent ...
Reference: Earthquake Spectra, Volume 28, No. S1, pages S39–S54, June 2012; 2012, Earthquake Engineering Research Institute
The seismic design criteria applied to siting commercial nuclear power plants operating in the United States received increased attention following the March 11, 2011, earthquake and tsunami that devastated Japan’s Fukushima Daiichi nuclear power station. ...
Reference: CRS Report for Congress, Prepared for Members and Committees of Congress
The main reason for the generation of tsunamis is the deformation of the bottom of the ocean caused by an underwater earthquake. Usually, only the vertical bottommotion is taken into account while the horizontal co-seismic displacements are neglected in the ...
Reference: arXiv:1011.1741v3 [physics.class-ph] 13 Feb 2012
A devastating earthquake hit the Tohoku and Kanto regions of Japan on 11 March 2011, causing extensive damage to life and property as a result of large-scale tsunami and damage to nuclear power plants. Many slope failures occurred in hilly areas, such as in ...
Reference: NZSEE Annual Technical Conference & AGM, 13-15 April 2012, Christchurch
We apply the recently developed "tsunami ball" method to construct a physics based simulation of the 1963 Vaiont reservoir landslide and flood disaster.
Reference: Ital. J. Geosci. (Boll. Soc. Geol. It), Vol 130, No 1 (2011)
<p>We conduct a comprehensive study of the Amorgos, Greece earthquake and tsunami of 1956 July 09, the largest such event in the Aegean Sea in the 20th century. Systematic relocation of the main shock and 34 associated events defines a rupture area measuring ...
Reference: Geophys. J. Int. (2009) 178, 1533–1554
<p>The primary objective of this study is to examine tsunami generation from the 2004 Sumatra-Andaman earthquake at different levels of parameterization for the purpose of forecasting and assessing future tsunamis.</p>
Reference: Bulletin of the Seismological Society of America, Vol. 97, No. 1A, pp. S249-S270, January 2007
Catastrophic rock slope failures have caused destructive tsunamis in Norwegian fjords. At the Åknes rock slope the tsunami generating potential is large due to the potential large volume involved in a possible catastrophic failure. Widening of the upper crack ...
Reference: The South African Institute of Mining and Metallurgy, International Symposium on Stability of Rock Slopes in Open Pit Mining and Civil Engineering
<p>Plate tectonics after the 26 December 2004 Great Sumatra earthquake resulted in major topological changes in the Andaman and Nicobar islands. Aerial and land reconnaissance surveys of those islands after the earthquake provide evidence of spectacular plate ...
Reference: Earthquake Spectra, Volume 22, No. S3, pages S43–S66, June 2006