(2015, February 5). Pages in category "Megathrust earthquakes in Japan" The following 33 pages are in this category, out of 33 total. Yamanaka, Y., & Kikuchi, M. (2004). “Nankai megathrust earthquakes are great megathrust earthquakes that occur along the Nankai megathrust – the fault under the Nankai Trough – which forms the plate interface between the sub-ducting Philippine Sea Plate and the overriding Amurian Plate (part of the Eurasian Plate), which dips beneath southwestern Honshu, Japan. When the magnitude of the earthquake off Tohoku, Japan, was calculated to be 9.0, it joined the ranks of “megathrust” earthquakes — exceptionally large ruptures involving 5 to 10 meters of slip motion on fault zones more than 100 kilometers in length.These massive earthquakes occur along Earth’s subduction zones, that is, where two 150-kilometer thick plates of solid rock collide. 2012, 2015). The 2012 Sanriku earthquake (Japanese: 三陸沖地震) occurred near the city of Kamaishi, Japan, on December 7. Constraints on the recurrence times of subduction zone earthquakes are important for seismic hazard assessment and mitigation. Studies of older tsunami deposits suggest a recurrence interval for megathrust earthquakes of 500–800 years (Sawai et al. From the legend of Atlantis to the present day, this book casts new light on these deadly waves. The magnitude 9.0 Tohoku-Oki earthquake that struck Japan on 11 March 2011, killing more than 15,000 people and setting off a devastating tsunami that … Kimura H(1), Takeda T, Obara K, Kasahara K. Author information: (1)National Research Institute for Earth Science and Disaster Prevention (NIED), 3-1 Tennodai, Tsukuba, Ibaraki 305-0006, Japan. The magnitude 7.3 shock generated a small tsunami, with waves up to 1 m high, that hit Ishinomaki in Miyagi Prefecture. Earthquake distribution around Japan (1960-2011) Monitoring of Earthquakes and Provision of Information To monitor earthquakes, JMA operates an earthquake observation network comprised of about 200 seismographs and 600 seismic intensity meters. This book analyses these failings, and discusses what Japan, and other countries, can learn from these events. Magnitude 8 megathrust earthquakes that have generated large tsunamis with wave heights of >5 m in coastal areas of southwestern Japan have occurred every 100–150 years along the Nankai–Suruga Trough, which marks the convergent boundary between the … Found insideThis book contains a collection of different research activities that include the biodegradation compounds with contaminant characteristics and special products of different interests as an added value product or that allows following up ... extremely powerful seismic events triggered in subduction zones, where one tectonic plate plunges below another. Near-trench earthquake rupture and seafloor deformation. Found insideIn light of recent massive quakes in Haiti, Chile, and Mexico, Cascadia's Fault not only tells the story of this potentially devastating earthquake and the tsunamis it will spawn, it also warns us about an impending crisis almost ... The two megathrust earthquakes, the 2004 Sumatra-Andaman and the 2005 Nias-Simeulue events, are both among the 11 largest earthquakes ever recorded. To explain this mismatch between different periods, we modeled the entire megathrust earthquake cycle in the Northeast Japan arc using a simple dislocation model with a two-layered … In Japan, the Nankai megathrust under the Nankai Trough is responsible for Nankai … This volume attempts to answer such fundamental concerns as why some interplate subduction earthquakes are relatively modest in rupture length (greater than 100 km) while others, such as the great (M greater than 9) 1960 Chile, 1964 Alaska, ... The amount of shaking at a location depends on an earthquake's magnitude, the distance between the location and the earthquakes 's source, and local geology. Earlier earthquakes that took place in such zones include the devastating 2011 earthquake followed by tsunami in Japan that claimed lives of thousands of people and triggered the Fukushima nuclear disaster, as well as a 2004 Indonesia magnitude 9.0 earthquake that left as many as 250,000 people dead. Large interplate megathrust earthquakes occurred in the Nankai subduction zone off Southwest Japan with an interval of ~100 to 150 years. Found insideThis invaluable volume set of Advances in Geosciences continues the excellent tradition of the Asia-Oceania scientific community in providing the most up-to-date research results on a wide range of geosciences and environmental science. The recent Tōhoku quake that struck Japan on March 11th, is a devastating reminder of the sheer power and velocity of a magnitude 9 earthquake. The link between the Japan and Cascadia events was clinched. Mary Leitka, a tribal elder, is recounting a Hoh legend centuries older than the building she sits in. Vinyl tablecloths cover the counters, and disco hits bubble beneath the restaurant chatter. The damage pattern would be very different. New GPS data has helped scientists probe giant megathrust earthquakes, such as the one that hit Chile in 2010 and Japan in March. Given that we can now expect the recurrence of an earthquake with magnitude greater than M8, we should explore the tectonic implications in NE Japan of M9-class earthquake cycles. These interplate earthquakes are the planet's most powerful, with moment magnitudes ( Mw) that can exceed 9.0. The 23-meter-high tsunami wave triggered by the earthquake flooded over 500km² of the Japanese Pacific coastline. This book is devoted to different aspects of earthquake research. Depending on their magnitude and the placement of the hypocenter, earthquakes have the potential to be very destructive. Found insideKathryn Miles descends into mines in the Northwest, dissects Mississippi levee engineering studies, uncovers the horrific risks of an earthquake in the Northeast, and interviews the seismologists, structual engineers, and emergency managers ... Underplating Below the Megathrust Earthquake Zone in Japan Hisanori Kimura,1* Tetsuya Takeda,1 Kazushige Obara,1'2 Keiji Ka Sahara2 Determining the structure of subduction zones is important for understanding mechanisms for the generation of interplate phenomena such as megathrust earthquakes. Since 1900, all earthquakes of magnitude 9.0 or greater have been megathrust earthquakes. This megathrust earthquake ruptured part of the subduction interface near the Japan Trench, where the Pacific Plate dives underneath the Eurasian Plate. The nature of incoming sediments is a key controlling factor for the occurrence of megathrust earthquakes in subduction zones. The underlying fault, the Nankai megathrust, is the source of the devastating Nankai megathrust earthquakes, while the trough itself is potentially a major source of hydrocarbon fuel, in the form of methane clathrate. There have been few attempts at seismotectonic analysis at map scale. Based on the above issues, this paper analyzes the characteristics of potential migration intentions in the case of a massive earthquake in the Nankai Trough area. The epicenter was Moment magnitude scale was There was almost no damage from the earthquake itself, but the huge tsunami caused by this earthquake struck the coasts of Iwate Prefecture and other areas, causing enormous damage. Results presented here are intended to provide guidance to local emergency management agencies for tsunami inundation assessment, evacuation planning, and public education to mitigate future tsunami hazards. Abstract. The Routledge Companion to Media and Humanitarian Action explores the interconnections between media, old and new, and the humanitarian challenges that have come to define the twenty-first century. Real subduction zones display re- The massive Tohoku, Japan, earthquake in 2011 and Sumatra-Andaman superquake in 2004 stunned scientists because neither region was thought to be capable of producing a megathrust earthquake … The March 11, 2011, earthquake was much larger than other post-1900 plate boundary thrust fault earthquakes in the southern Japan Trench, none of which attained M 8. The tsunami killed about 22,000 people. In predicting ground motions for earthquakes larger than Mw 8.0, such as mega-thrust earthquakes along the Japan Trench and the Nankai Trough (where magnitudes could reach 9 and above), extrapolation inferred from ground motion data of smaller magnitudes was typically used. The Nankai trough has hosted ~M8 interplate earthquakes with the interval of 100-200 years. Among the set of tools are tsunami forecasting, educational experiments, early alerting systems, and design guidance for tsunami-resilient communities. Part of this book has already been published in a recent journal issue. It occurred at a depth of 36 km within the Pacific Plate and was the result of reverse faulting, about 20 kilometres (12 mi) east of the Japan Trench Randomness of megathrust earthquakes implied by rapid stress recovery after the Japan earthquake. 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