";s:4:"text";s:2949:"Consider that an arbitrary spatial region and a range of magnitudes have The off-Kamaishi earthquake is one such example (Fig. a rate increase of 160%). Earthquake-triggered landslides are among the most destructive secondary hazards associated with strong seismicity, often resulting in damage to infrastruc-ture and loss of life (Keefer 1984). 5 demonstrates how coherence changes with inter-event distance for pairs of earthquakes in the earthquake cluster that contain repeater sequences. We also find that the 2016 Pedernales earthquake triggered a shallow slow slip event (SSE) ~100 km south of the seismic rupture . You can find out more about our use of cookies in About Cookies, including instructions on how to turn off cookies if you wish to do so. A tsunami event that occurred recently and received global news coverage was the catastrophic tsunami that was generated in the Indian Ocean on December 26, 2004. The balance of the slope before the earthquake, changeable ground water conditions, and total precipitation directly before or after an earthquake can be as important in the case of earthquake-triggered landsliding as they are in the case of meteorological triggers … One historical example of a mass flow event triggered by an earthquake in the proximity of the VDLS site is the rock avalanche caused by the second M w 6 earthquake of the 1946 earthquake sequence ( Moore et al., 2012 ). The epicenter of the earthquake that triggered the series of tsunami’s was located off the west coast of Sumatra, Indonesia. Here, the distances are normalized by the fault radius (inter-event distances are divided by the sum of the fault radii of the two earthquakes). 4a) and Fig. A remotely triggered slow slip event. The results will lead us to examine the distribution of waiting times conditioned to different values of the jumps; finally, we measure diffusion profiles for seismic occurrence. An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves.Earthquakes can range in size from those that are so weak that they cannot be felt to those violent enough to propel objects and people into the air, and wreak destruction across entire cities. 33 preceding 4 decades [Ammon et al., 2010]. By continuing to browse this site you agree to us using cookies as described in About Cookies . The slip took place close to the trench at a depth shallower than 10 km.