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Mr. Clerie, who left Haiti in 1959 and did not return until after the 2010 earthquake called him for a life of community service, is light-skinned.
Because earthquake timings are unpredictable within our current understanding, the best method is time-invariant deterministic seismic hazard analysis (DHSA) to assess effects from the largest single earthquake called Maximum Credible Earthquake (MCEs) expected from seismogenic faults.
This earthquake, called the 2015 Gorkha earthquake, was followed by large aftershocks to the west and east of the mainshock rupture.
On 31 March 2002, an M w 7.1 (M L 6.8) earthquake, called the 331 Hualien offshore earthquake, occurred in this area.
On 31 March 2002, an M w 7.1 earthquake, called the 331 Hualien offshore earthquake, also occurred in this area (see Fig. 1).
"The satellite looks largely down, but also off to the side slightly, and this allows us to see lateral/horizontal motion - and in this type of earthquake, called a strike-slip, we see this effect as movement of the ground towards and away from the fault.
Similar(53)
BRRPs are intended to be used as stoppers, and when they are installed at the edges of girder-type bridges, they will act as stiff elastic bearings in small to moderate earthquakes (called "Level 1 earthquakes" in Japan) and as energy dissipating dampers in large earthquakes (called "Level 2 earthquakes" in Japan).
We first simulate ground motions for virtual middle-size earthquakes called Event 3 and Event 4 from the recorded waveforms of the real small earthquakes (Event 1 and Event 2).
A giant earthquake, the 2011 off the Pacific Coast of To-hoku earthquake (hereafter called the Tohoku earthquake), occurred at the subduction plate boundary east of northern Honshu on March 11 , 2011
Evidence of damages in previous earthquakes has shown that damage to structures is increased when structures become closer to earthquake faults called near-field earthquake effect.
The 2011 off the Pacific coast of Tohoku Earthquake (hereafter called the 2011 Tohoku earthquake) occurred at 1446 23 JST (Japan Standard Time = UT + 9 h) on 11 March 2011 with Mw 9.0 and at an epicenter of (38.32°N, 142.37° E) (U.S. Geological Survey, 2011).
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