2010
DOI: 10.1038/ngeo975
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High tsunami frequency as a result of combined strike-slip faulting and coastal landslides

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Cited by 86 publications
(59 citation statements)
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“…The destructive 2010 Haiti earthquake and the 1999 earthquakes in Turkey brought to the world's attention the need to investigate seafloor ruptures and earthquake recurrence intervals along submarine transform faults (e.g., Barka, 1999;Parsons et al, 2000;Reilinger et al, 2000;Calais et al, 2010;Hayes et al, 2010;Prentice et al, 2010). Many onshore-offshore continental transform boundaries exist near densely populated regions, and faulting at these transforms sometimes generates destructive earthquakes.…”
Section: Introductionmentioning
confidence: 99%
“…The destructive 2010 Haiti earthquake and the 1999 earthquakes in Turkey brought to the world's attention the need to investigate seafloor ruptures and earthquake recurrence intervals along submarine transform faults (e.g., Barka, 1999;Parsons et al, 2000;Reilinger et al, 2000;Calais et al, 2010;Hayes et al, 2010;Prentice et al, 2010). Many onshore-offshore continental transform boundaries exist near densely populated regions, and faulting at these transforms sometimes generates destructive earthquakes.…”
Section: Introductionmentioning
confidence: 99%
“…Reconnaissance fi eld observations also led to the suggestion of probable Holocene faulting along this valley within a possible restraining bend (Koehler and Mann, 2011). Based on our observations alone, it is not clear if this fault is a splay off a main trace offshore to the north or the principal trace of the EPGF within a restraining bend; evidence of EPGF-parallel young faults within Grand Goâve Bay (Hornbach et al, 2010) described in the following supports the former interpretation. The ridge at Tapion Du Petit Goâve appears to be an active northeast-vergent fold, based on its on September 12, 2012 geosphere.gsapubs.org Downloaded from morphology and oblique orientation relative to the overall trace of the EPGF (Fig.…”
Section: Fault Segmentation and Evidence Of Past Surface Rupturementioning
confidence: 61%
“…Although the fault appears to be both onshore and offshore between L'Acul and Port Royal, our observations are limited to onshore areas because we did not have high-resolution bathymetric data to merge with the LiDAR data at the time of analysis. Such data have subsequently revealed faults offshore (Hornbach et al, 2010 (Both applications are available from http:// keckcaves.org/software.) Because applications using the Vrui toolkit are written without a particular input environment in mind, we used LiDAR Viewer and Crusta on multiple different hardware environments including standard desktop computers, a 3D display, and the CAVE fully immersive visualization environment.…”
Section: Softwarementioning
confidence: 99%
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“…Nevertheless, coastal areas are vulnerable to natural disasters such as earthquakes, tsunamis, and hurricanes (e.g., Mallin and Corbett, 2006;Wang et al, 2006;Hornbach et al, 2010), as evidenced by the recent magnitude 9.0 Tohoku earthquake that devastated coastal areas in northeast Japan on March 11, 2011. In order to mitigate natural disasters, it is important to map and understand underground features in coastal areas, because liquefaction caused by earthquakes depends on geological settings (Hallier et al, 2008), tsunami generation is, to some extent, associated with underwater landslides caused by the instability of sediments (Tinti et al, 2006), and hurricanes are major factors which erode, transport and redeposit sediments in coastal areas (Miner et al, 2009).…”
Section: Introductionmentioning
confidence: 99%