What was Genroku’s earthquake death toll: it may have been as high as 200,000. The Genroku Kanto earthquake occurred in southern Kanto, less than 100 km away from Tokyo, on December 31, 1703. Did you know... that uplift data and tsunami wave heights indicate that the 1703 Genroku earthquake was probably caused by the rupture of three separate segments of the Eurasian – Philippine Sea Plate boundary? A record of the entry may be seen at Wikipedia:Recent additions/2011/November. occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō Region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. Its magnitude is estimated to be 7.9-8.2 (Usami, 2003). Your email address will not be published. Kuril Islands earthquake, 2006. It was an ocean trough earthquake originating somewhere between Sagami Bay and the area off the southern shore of the Bōsō Peninsula. The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. [12] The 31 December 1703 M w 8.2 Genroku earthquake ruptured two fault segments of the Sagami Trough and was the largest historical earthquake on this fault system [Shishikura, 2003; Grunewald and Stein, 2006]. The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. Here, we examine the correlation between two great Japa-nese earthquakes, the 1703 M w 8.2 Genroku and 1707 M w 8.7 Hoei, and Mt. correlation between earthquakes and volcanic eruptions. Fuji’s explosive (VEI 5) Hoei eruption, 49days after the 1707 earthquake. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC). Furthermore, these reflectors revealed a topographic high (bump) beneath the southern coast of the Boso Peninsula where the source fault of the Genroku earthquake of 1703 is thought to … The earthquake triggered a major tsunami which caused many casualties, giving a total death toll of at least 5,233, possibly up to 10,000. The 1703 Genroku and 1923 (Taisho) Kanto earthquakes (M 8.2 and M 7.9, respectively) are known as typical ones, and cause severe damages in the metropolitan area. Genroku is a Japanese eraspanning from 1688 through … The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC). Previous modeling of the 1703 earthquake applied inversion analyses of the observed terrestrial crustal deformations along the coast of the southern Boso Peninsula and revealed that the tsunami was generated along the Sagami Trough. A total of 8,007 houses were destroyed by the shaking and a further 563 houses by the fires, causing 2,291 deaths. 1697 (Genroku 10): Great fire in Edo. [1], "Comments for the Significant Earthquake", "A new probabilistic seismic hazard assessment for greater Tokyo", "Cycle of Interplate Earthquake Along the Sagami Trough, Deduced from Tectonic Geomorphology", "Catalog of Damaging Earthquakes in the World", https://en.wikipedia.org/w/index.php?title=1703_Genroku_earthquake&oldid=1009457039, Articles containing Japanese-language text, Creative Commons Attribution-ShareAlike License, This page was last edited on 28 February 2021, at 18:16. On both the Bōsō Peninsula and Miura Peninsula a clear paleo shoreline has been identified, indicating up to 5 m of uplift near Mera (about 8 km south of Tateyama) and up to 1.2 m of uplift on Miura, increasing to the south. Required fields are marked *. The entire wiki with photo and video galleries for each article 1703 Genroku earthquake is similar to these topics: 1842 Cap-Haïtien earthquake, 1981 Sirch earthquake, 1906 Aleutian Islands earthquake and more. The Kantō Region lies at the complex triple junction, where the convergent boundaries between the subducting Pacific and Philippine Sea Plates and the overriding North American Plate meet. The recurrence periods of Genroku- and Taisho-type earthquakes inferred from studies of wave cut … [2] The 1703 earthquake is thought to have involved rupture of the interface between the Eurasian Plate and the Philippine Sea Plate. 1703 (Genroku 16, 5th month): First performance of Chikamatsu Monzaemon's play The Love Suicides at Sonezaki (Sonezaki shinjū). The Arica Tsunami of 1868. Genroku, 1703 (Genroku 16)/11/23 The M7.9–8.2 Genroku earthquake occurred at about 2 a.m. on December 31, 1703, resulting in over ten thousand deaths. Japan’s spectacular economic success story over the second half of the 20th century is the more remarkable when you consider the shaky foundations on which it has been constructed – quite literally, since the country is one of the most geologically unstable parts of the entire planet. The earthquake triggered a major tsunami which caused many … An estimated 2,300 people were killed by the shaking and subsequent fires. (adsbygoogle = window.adsbygoogle || []).push({}); Your email address will not be published. The islands are actually a row of peaks in an underwater mountain range which includes hundreds of volcanoes – most notably iconic Mount Fuji, one of some 40 which are active. When did the Genroku earthquake happen: December 31 1703, Where did the Genroku earthquake happen: Edo (Tokyo), Japan. Genroku is a Japanese era spanning from 1688 through 1704. Where did the Genroku earthquake happen: Edo (Tokyo), Japan. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC). We model the static stress changes and dilatational … (2)The Genroku Earthquake (December 31, 1703, M 7.9-8.2) Genroku Earthquake is thought to have been an interplate earthquake whose focal region extended from Sagami Bay to the tip of the Boso Peninsula as well as the area along the Sagami Trough in the open sea southeast of the Boso Peninsula. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin?) There was also a single death on the island of Hachijō-jima about 180 km south of the earthquake's epicentre, where the tsunami was 3 m high. The 1703 Genroku Kanto earthquake and the resulting tsunami caused catastrophic damage in the Kanto region of Japan. The earthquake triggered a major tsunami which caused many … In 2006, a … This Genroku map was corrected in 1719 (Kyōhō 4) by the mathematician Tatebe Katahiro (1644–1739), using high mountain peaks as points of reference, and was drawn to a scale of 1:21,600. An estimated 2,300 people were killed by the shaking and subsequent fires. What was Genroku’s earthquake death toll: … Great earthquakes along the Sagami trough have repeatedly occurred. The Taisho type is defined by the Kanto earthquake of 1923 and the Genroku type by the Genroku earthquake of 1703. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC). Fuji's explosive (VEI 5) Hoei eruption, 49 days after the 1707 earthquake. [11] 31 December 1703 ( Genroku 16, 23rd day of the 11th month ): The Great Genroku Earthquake shook Edo. Japan comprises more than 4,000 islands, though the vast majority of the population lives on the four largest. You should know: The earthquake occurred during the historical Genroku Era and the name is used to distinguish it from subsequent major quakes which struck the city in 1855 and 1923. Even so, it is not easy for those of us who take living on terra firma for granted to comprehend that on an average day in Japan some half-dozen tremors are recorded somewhere in the Japanese archipelago. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. Previous modeling of the 1703 earthquake applied inversion analyses of the observed terrestrial crustal deformations along the coast of the southern Boso Peninsula and revealed that the tsunami was generated along the Sagami Trough. An estimated 2,300 people were killed by the shaking and subsequent fires. [5], The area of greatest damage due to the earthquake shaking was in Kanagawa Prefecture, although Shizuoka Prefecture was also affected. Few parts of the country have been spared over the centuries, but it is incidents affecting the most heavily populated areas that have attracted the greatest attention. Intensity distribution of the 1703 Genroku earthquake (M8.1) and the 1923 Taisho Kanto earthquake (M7.9). Both earthquakes occurred along Sagami Trough. Fuji [1] Other estimates are higher, with 10,000 in total,[7] and one source that gives 200,000. Tohoku earthquake, 2011 Japan's largest quake struck on March 11, 2011. In addition, to analyze the various types of edge waves that could be expected three additional earthquake scenarios were considered, each of them with a different magnitude and epicenter: the 1896 Sanriku Earthquake, the 1677 Empo Boso-oki Earthquake, and the 1703 Genroku Kanto Earthquake. [4] This distribution of uplift, coupled with modelling of the tsunami, indicate that at least two and probably three fault segments ruptured during the earthquake. The Taisho type is defined by the Kanto earthquake of 1923 and the Genroku type by the Genroku earthquake of 1703. The 31 December 1703 M w 8.2 Genroku earthquake ruptured two fault segments (Figure 1) of the Sagami Trough and was the largest historical earthquake on this fault system [Shishikura, 2003;Grunewald and Stein, 2006]. Earthquakes along the Sagami trough, where the Philippine Sea slab is subducting, have repeatedly occurred. Here, we examine the correlation between two great Japanese earthquakes, the 1703 M w 8.2 Genroku and 1707 M w 8.7 Hoei, and Mt. The 1703 Genroku and 1923 (Taisho) Kanto earthquakes (M 8.2 and M 7.9, respectively) are known as typical ones, and cause severe damages in the metropolitan area. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. Two types of the earthquakes strike the southern Boso Peninsula, the Taisho and the Genroku types (Matsuda et al., 1978, Shishikura, 2000). The 1703 Genroku Kanto earthquake and the resulting tsunami caused catastrophic damage in the Kanto region of Japan. [3], The earthquake was associated with areas of both uplift and subsidence. It should not come as a surprise, then, that roughly one fifth of the world’s earthquakes occur here. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. The 1703 Genroku Kanto earthquake and the resulting tsunami caused catastrophic damage in the Kanto region of Japan. When did the Genroku earthquake happen: December 31 1703. An estimated 2,300 people were killed by the shaking and subsequent fires. The Genroku earthquake of 1703 measured 8.0 in magnitude, but the accompanying tsunami managed to kill more than 108,000 people. The earthquake triggered a major tsunami which caused many casualties, giving a total death toll of at least 5,233, possibly up to 10,000. The explanation for all this activity is that Japan lies on a fault line between two of the earth’s major tectonic plates. Genroku, 1703 (Genroku 16)/11/23 The M7.9–8.2 Genroku earthquake occurred at about 2 a.m. on December 31, 1703, resulting in over ten thousand deaths. The 1703 Genroku Kanto earthquake and the resulting tsunami caused catastrophic damage in the Kanto region of Japan. The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. Earthquakes with epicenters in the Kanto region may occur within the Eurasian Plate, at the Eurasian Plate/Philippine Sea Plate interface, within the Philippine Sea Plate, at the Philippine Sea Plate/Pacific Plate interface or within the Pacific Plate. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC). Wemodel the static stress changes and dilatational strain imparted on the Mt. An estimated 2,300 people were killed by the shaking and subsequent fires. The earthquake triggered a major tsunami which caused many … [1] Studies in magma‐tectonics point to a spatiotemporal correlation between earthquakes and volcanic eruptions. [5] The total number of casualties from earthquake, fires and tsunami has been reported as 5,233. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. Two types of the earthquakes strike the southern Boso Peninsula, the Taisho and the Genroku types (Matsuda et al., 1978, Shishikura, 2000). At the start of the 18th century Edo (as Tokyo was then known) was the world’s largest city, with a population of one million; on the last day of 1703, however, it was devastated by a massive earthquake. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin?) Genroku refers to the Japanese era spanning 1688 to 1704 – the quake actually struck in Sagami Bay, about 25 miles southwest of Tokyo. [3], The tsunami had run-up heights of 5 m or more over a wide area, with a maximum of 10.5 m at Wada and 10 m at both Izu Ōshima and Ainohama. Not all large earthquakes are deadly location matters. We propose a fault model of the 1703 Genroku Kanto earthquake by using recently imaged shape of Philippine Sea Plate, distributions of coseismic coastal movements, and tsunami inundation heights along the eastern Boso coast. The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. Earthquakes along the Sagami trough, where the Philippine Sea slab is subducting, have repeatedly occurred. Intensities in the west of the Izu Peninsula are apparently smaller than those of 1923. In addition to this set of major plates it has been suggested that there is also a separate 25 km thick, 100 km wide body, a fragment of Pacific Plate lithosphere. Intriguingly slow slip events have also repeatedly occurred in an area adjacent to the asperities of the great earthquakes, off Boso peninsula (e.g., Ozawa et al 2007). Most of the casualties were caused by the resulting fires which swept through the mainly wooden buildings, and by a tsunami which smashed into a wide coastal area around Sagami Bay and the Boso Peninsula. The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. In addition, to analyze the various types of edge waves that could be expected three additional earthquake scenarios were considered, each of them with a different magnitude and epicenter: the 1896 Sanriku Earthquake, the 1677 Empo Boso-oki Earthquake, and the 1703 Genroku Kanto Earthquake. occurred at 02:00 local time on December 31 (17:00 December 30 UTC).The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō Region, Japan.An estimated 2,300 people were killed by the shaking and subsequent fires. The earthquake triggered a major tsunami which caused many … The 1703 Genroku earthquake (元禄大地震, Genroku Daijishin) occurred at 02:00 local time on December 31 (17:00 December 30 UTC). Intensities of 1703 after Matsu’ura and Nakamura , and those of 1923 after JMA . An estimated 2,300 people were killed by the shaking and subsequent fires. The earthquake caused many large fires, particularly at Odawara, increasing both the degree of damage and the number of deaths. The 1703 Genroku and 1923 (Taisho) Kanto earthquakes caused severe damages in the Tokyo metropolitan area. About 400 km of coastline was severely affected by the tsunami,[6] with deaths being caused from Shimoda on the east coast of the Izu Peninsula in the west to Isumi on the east side of the Bōsō Peninsula to the east. 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