1943 tottori earthquake

1 EARTHQUAKE-RIDDEN JAPAN • Japan is prone to earthquakes. ^ "Interpretation of damage to houses and casualties relied on a precise evaluation of earthquake ground motions in the epicentral region: 1945 Mikawa earthquake". 2013 ). As the earthquake struck in the evening when most kitchens had fires lit in preparation for the evening meal, fires broke out in 16 locations around the city. The Tottori earthquake (鳥取地震, Tottori jishin) occurred in Tottori prefecture, Japan at 17:36 local time on September 10, 1943. Statistics of the damage caused by the earthquake are tabulated in Table 1. Thus, we can recognize the possible surface faulting event around the epicentral area based on recent understanding of tectonic geomorpholgy. Eventualaj ŝanĝoj en la angla originalo estos kaptitaj per regulaj retradukoj. Viscoelastic relaxation of a large earthquake generally continues for more than several decades. [2] The center of Tottori city, with many antiquated buildings was the hardest hit, with an estimated 80% of its structures damaged or destroyed. This observation probably means that the causative fault for Tottori earthquake is at the infant stage on its way of evolution based on the Wesnousky's fault evolution model (Wesnousky,1988). 2.1 Description of the 2000 Tottori earthquake mainshock and of its largest aftershock On 6 October 2000 at 13:30 UTC, the Western Tottori Earthquake (Mw 6.6-6.8) occurred on a left-lateral strike-slip fault in the western Honshu, Japan, where very few large earthquakes have occurred since the 1943 Tottori earth-quake of M 7.2 (Kanamori, 1972). The 2016 M w 6.2 Tottori earthquake bears several similarities to the previous 1943 M w 7.0 and 2000 M w 6.7 Tottori earthquakes, and also some significant differences. Covid-19. (2014) showed a zone of high strain rate observed by GNSS almost overlapped the seismic zone and proposed to call it “the San’in shear zone”. We also showed the slip distribution along the surface rupture (Fig.3).The trace of the 1943 surface rupture exhibited the large step and quite sinuous geometry compared with other strike-slip surface breaks. Edit Like Comment Share. For example, about 80 % earthquakes occur in a positive dCFF region in case of the 1943 Tottori earthquakes, though the aftershocks of the 2000 Western Tottori earthquake (MJMA = 7.3) are … Although the earthquake occurred during World War II, information about the disaster was surprisingly uncensored, and relief volunteers and supplies came from many parts of the Empire of Japan, including Manchukuo. 2. The records of the Tottori earthquake of 1943 (M = 7.4, 35.5° N, 134.2° E, depth 10 km) about by a low-magnification seismograph at a relatively short distance are used to determine dynamics fault parameters such as the particle velocity and the effective tectonic stress, in addition to static fault parameters such as the dislocation and the stress drop. 1948 Fukui (Japan) Earthquake Archive: In Memory of Prof. Masayuki Kikuchi (1948-2004) 1948 6/28 7:13 UTC 36.50N 136.00E 10km Mw=6.8, Fukui, Japan. Advertising. Although the earthquake occurred during World War II, information about the disaster was surprisingly uncensored, and relief volunteers and supplies came from many parts of the Japanese empire, including Manchukuo.. • A hazardous earthquake can occur anytime, anywhere. In 2000, the M w 6.7 Western Tottori earthquake occurred approximately 50 km to west of the 2016 Tottori earthquake (Figure 1). Function: _error_handler, Message: Invalid argument supplied for foreach(), File: /home/ah0ejbmyowku/public_html/application/views/user/popup_modal.php Line: 315 Distribution of the JMA seismic intensity and the peak ground acceleration together with the epicenter are presented in Figures 1 and 2, respectively. In this area the Tottori earthquake (M= 7.4) occurred in 1943. Ohmi et al., 2002), showing that the SSZ is seismotectonically active. Time in Baba is now 06:44 PM (Saturday) . 3). Although the earthquake occurred during World War II, information about the disaster was surprisingly uncensored, and relief volunteers and supplies came from many parts of the Japanese empire, including Manchukuo.. Pages 73-91, (compatible with EndNote, Reference Manager, ProCite, RefWorks). Volume 2002 The Tottori earthquake (鳥取地震, Tottori jishin) occurred in Tottori prefecture, Japan at 17:36 local time on September 10, 1943. The trace of the 1943 surface rupture exhibited the large step and quite sinuous geometry compared with other strike-slip surface breaks. The Tottori earthquake of 1943 The Tottori earthquake (M = 7.4) occurred on Sep- tember 10, 1943, in the vicinity of Tottori, Japan (see fig. In 2000, the M w 6.7 Western Tottori earthquake occurred approximately 50 km to west of the 2016 Tottori earthquake (Figure 1). ^ Paula Dunbar. This observation probably means that the causative fault for Tottori earthquake is at the infant stage on its way of evolution based on the Wesnousky's fault evolution model (Wesnousky,1988). Line: 24 Seismic intensity 6 in JMA scale was observed in Tottori City, and 5 in Okayama City . Before this earthquake, there were earthquakes frequently occurred since October 2015 in the area about 10 km east of the area where the 2016 earthquake occurred, and the east side is the western extension of the Kano and Yoshioka faults, the 1943 Tottori earthquake fault. Interactive map of Hogi. Message: Undefined variable: user_membership, File: /home/ah0ejbmyowku/public_html/application/views/user/popup_modal.php This is a list of earthquakes in 1943.Only magnitude 6.0 or greater earthquakes appear on … The severely damaged area was concentrated on the Tottori plain (Architectural Institute of Japan, 1944), whereas there was less damage in the western and southern parts of Tottori City. La ĉi-suba teksto estas aŭtomata traduko de la artikolo 1943 Tottori earthquake article en la angla Vikipedio, farita per la sistemo GramTrans on 2014-01-11 06:56:46. Line: 479 Line: 68 The epicenters may be uncertain 35*N 134"E 135*E Fig. III Earthquakes • Earthquakes in Japan (p.2 5 • Earthquake preparation (p.6 10 • What to do in the event of an earthquake (p.11 16 . past century several large earthquakes have occurred within the SSZ, such as the 1943 Tottori earthquake (M7.2) (e.g. Faulting was expressed in the trenches as conspicious flexures ofgeologic beds, abrupt termination of geologic units, and open tunnels that possibly formed duringfaulting. In 1943, the M w 7.0 Tottori earthquake occurred east of the 2016 hypocenter (yellow line, Figure 1) and ruptured the Shikano and Yoshioka faults (Kaneda & Okada, 2002; Omote, 1943; Tsuya, 1944). [1] The seismic intensity was recorded as 6 in Tottori city, and 5 as far away as Okayama on the Inland Sea. Although the earthquake occurred during World War II, information about the disaster was surprisingly uncensored, and relief volunteers and supplies came from many parts of the Japanese empire, including Manchukuo. Geophysical Review of the JMA). The particle velocity of the fault motion is … Wikipedia's 1943 Tottori earthquake as translated by GramTrans. This observation probably means that the causative fault for Tottori earthquake is at the infant stage on its way of evolution based on the Wesnousky's fault evolution model (Wesnousky,1988). Are you sure you want to cancel your membership with us? Another possibility to cause strain rate concentration in the SSZ is postseismic deformation of recent large earthquakes including the 1927 M JMA 7.3 Tango, the 1943 M JMA 7.2 Tottori, and the 2000 M JMA 7.3 western Tottori earthquake. Hogi in the region of Tottori is a place in Japan - some 315 mi or ( 507 km ) West of Edo , the country's capital city . If the apparent frictional coefficient is less than ~ 0.1, the coseismic \(\Delta {\text{CFS}}\) on the source faults of the 1943 M j 7.3 Tottori earthquake, 1596 M7.0 Keicho Iyo earthquake, and 1596 M7.5 Keicho Fushimi earthquake that occurred within 10 years before the megathrust earthquake along the Nankai trough is negative. 1943 Tottori earthquake. Time in Hogi is now 04:07 AM (Sunday) . Therefore, to explain the occurrence of these historical earthquakes, our … Surface rupture with maximum right-lateral displacement of 150cm and length of about 1 lkm was observed during the 1943 Tottori earthquake of Mw: 7.0, which struck the eastern Tottori prefecture, southwest Japan. is a Western-style French Renaissance style residence of the Ikeda clan located in Tottori, Tottori Prefecture, Japan. [3], File: /home/ah0ejbmyowku/public_html/application/views/user/popup_modal.php Line: 478 Function: _error_handler, File: /home/ah0ejbmyowku/public_html/application/views/page/index.php This event killed approximately 1000 people, injured more than 3000 people, and completely or partially destroyed more than 13,000 houses (Usami et al. We found that recent seismicity for the mainshock receiver faults is concentrated in the positive ΔCFF regions of four earthquakes (the 1927 Tango, 1943 Tottori, 1948 Fukui, and 2000 Tottori-Ken Seibu earthquakes), while no such correlations are recognizable for the other four earthquakes (the 1931 Nishi-Saitama, 1963 Wakasa Bay, 1969 Gifu-Ken Chubu, and 1984 Nagano-Ken Seibu earthquakes… Line: 107 Although the earthquake occurred during World War II, information about the disaster was surprisingly uncensored, and relief volunteers and supplies came from many parts of the Japanese empire, including Manchukuo.. Interactive map of Baba. Function: view, File: /home/ah0ejbmyowku/public_html/index.php In 1943, the M w 7.0 Tottori earthquake occurred east of the 2016 hypocenter (yellow line, Figure 1) and ruptured the Shikano and Yoshioka faults (Kaneda & Okada, 2002; Omote, 1943; Tsuya, 1944). events' taken from the March 1943 Tottori-Ken swarm initiated by the two mainshocks of Mj6.2 for the time span of about 190 days up until the 1943 Tottori earthquake of Mj7.2. Retrieved 15 April 2016. The Tottori earthquake (鳥取地震, Tottori jishin) occurred in Tottori prefecture, Japan at 17:36 local time on September 10, 1943. 1. For example, about 80 % earthquakes occur in a positive dCFF region in case of the 1943 Tottori earthquakes, though the aftershocks of the 2000 Western Tottori earthquake (MJMA = 7.3) are dominant in the western part of the study area. Function: view, File: /home/ah0ejbmyowku/public_html/application/controllers/Main.php Advertising. The horizontal projection of its fault plane derived by KANAMORI (1972) is represented by a broken line in the figure. As a result, the positive dCFF region caused by some historical large earthquakes (e.g., 1943 Tottori earthquake, 1948 Fukui earthquake) well agrees with epicentral distribution of recent seismicity. This article is within the scope of the WikiProject Japan, a collaborative effort to improve the coverage of Japan-related articles on Wikipedia. The death toll of this earthquake was over 3,700. The epicenter was 260 km (162 mi) from Ishigaki Island, Japan, 400 km (249 mi) from Basco, Philippines, and 425 km (264 mi) from Hualian, Taiwan. This aftershock activity is 1). 1943 Tottori earthquake. Three trenches were excavated across the Shikano fault which ruptured at the 1943 Tottoriearthquake (M=7.4). Oike, 1987), and the 2000 Western Tottori earthquake (e.g. earthquakes including the 1943 M7.2 Tottori and the 2000 M7.3 western Tottori earthquakes also occurred in this seismic zone. At the west end of this fault, inside a square area shown in the figure, a moderate-size earthquake (M= 6.2) occurred on Oct. 31, 1983. The method to estimate the lengt h Df the seismogenic fault must be reestablished. (2)The Tottori Earthquake (September 10, 1943, M 7.2) The Tottori Earthquake occurred in a shallow location on land, and its focal region was near the Tottori Plain. Function: _error_handler, File: /home/ah0ejbmyowku/public_html/application/views/user/popup_harry_book.php • Most communities are well equipped and prepared. The Tottori earthquake (鳥取地震, Tottori jishin) occurred in Tottori prefecture, Japan at 17:36 local time on September 10, 1943. Nishimura et al. 1943 Tottori earthquake Scan10029-2.JPG 647 × 498; 158 KB 1952 Tokachioki Earthquake.JPG 411 × 281; 28 KB 2000 Tottori earthquake shakemap.jpg 612 × 719; 148 KB 1943 Tottori-sismo. The Tottori plain in the Sanin area of Japan, the target area of this study, was severely damaged by the 1943 Tottori earthquake (M7.2). Two magnitude 6.2 earthquakes had occurred in the same area earlier that year on March 4 and 5, but did not do significant damage. Function: view, "Tottori 1943: M 7.0 - western Honshu, Japan", "The Tottori Earthquake (September 10, 1943, M 7.2)", https://en.wikipedia.org/w/index.php?title=1943_Tottori_earthquake&oldid=1011009411. We compiled all the previous reports and papers regarding the surface rupture associated with the earthquake as precise location maps (Appendix 1) and a data table (Appendix 2). September 10, 1943: Tottori Earthquake (7.2) 1,083: Compiled by Nippon.com based on the Central Disaster Management Council’s 1923 Great Kantō Earthquake Report, Volume 2. Baba in the region of Tottori is located in Japan - some 315 mi or ( 508 km ) West of Edo , the country's capital city . In particular, the 1943 Tottori earthquake caused crippling damage to Tottori City and its surroundings due to strong ground motions. However, the length of the subsurface seismogenic fault is underestimated by the presently proposed method (Odagiri and Shimazaki,2000) and this sh ould lead to crucial underestimation of the seismic moment and also strong ground motions. 1943 Tottori earthquake: part our commitment to scholarly and academic excellence, all articles receive editorial review.|||... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled. Updated on May 19, 2018. Function: require_once. 1943 Tottori earthquake, 1948 Fukui earthquake, 1961 Kita-Mino earthquake, 1969 Gihu-ken chubu earthquake, 1974 Izu-hanto Oki earthquake, 1978 off Izu Oshima earthquake, 1984 Nagano-ken seibu earthquake, and 1995 Hyogo-ken nabu earthquake (Fig. The local timezone is named " Asia/Tokyo " with a UTC offset of 9 hours. Line: 192 The records of the Tottori earthquake of 1943 (M = 7.4, 35.5° N, 134.2° E, depth 10 km) about by a low-magnification seismograph at a relatively short distance are used to determine dynamics fault parameters such as the particle velocity and the effective tectonic stress, in addition to static fault parameters such as the dislocation and the stress drop. The 1998 Ryukyu Islands earthquake (石垣島南方沖地震, Ishigakijima nanpō-oki jishin) occurred on May 4, 1998, at 08:30 local time (UTC+9) (on May 3 at 23:30 UTC) in the Philippine Sea region with M w 7.5 (USGS) and M7.7 (JMA). The latest faulting before the 1943 event was found in trenches A and B at Horakuji.The faulting before 1943 … Prefecture since the 1943 Eastern Tottori earthquake in which approximately one thousand people were dead. jor inland crustal earthquakes have occurred in central and western Japan: the 1891 Nobi (M=8), 1927 Tango (M=7.3), 1943 Tottori (M=7.2), and the 1948 Fukui (M=7.1) earthquakes. Surface rupture associated with the 1943 Tottori earthquake, compilation of previous reports and its tectonic geomorphological implications, Edited and published by : Japanese Society for Active fault Studies & The Research Group for Active Faults of Japan, geomorphologically detectable active fault, https://doi.org/10.11462/afr1985.2002.21_73. Although the earthquake occurred during World War II, information about the disaster was surprisingly uncensored, and reli… Line: 208 Sign in. The Headquarters for Earthquake Research Promotion. Most of the surface rupture during the earthquake occurred along the geomorphologically detectable active fault (Shikano-Yoshioka active fault system). The Tottori earthquake (鳥取地震, Tottori jishin) occurred in Tottori prefecture, Japan at 17:36 local time on September 10, 1943. Issue 21 The hypocenter coordinates are: latitude, 35.5; longitude, 134.2; depth, 10 km (JAPAN METEOROLOG- ICAL AGENCY, 1958). is located east of the epicenter of the 1943 Tottori earthquake, and compared them with previously reported results for a Quaternary-inactive fault. very few large earthquakes have occurred since the 1943 Tottori earthquake of M 7.4 (Kanamori, 1972) (Fig. ^ "The Tottori Earthquake (September 10, 1943, M 7.2)". Function: _error_handler, File: /home/ah0ejbmyowku/public_html/application/views/page/index.php The records of the Tottori earthquake of 1943 ( M = 7.4, 35.5° N, 134.2° E, depth 10 km) about by a low-magnification seismograph at a relatively short distance are used to determine dynamics fault parameters such as the particle velocity and the effective tectonic stress, in addition to static fault parameters such as the dislocation and the stress drop. These are roughly equivalent to earthquakes Mj2.0 or larger, and are listed in Kisho-Yoran (1943) (i.e. The Tottori earthquake (鳥取地震, Tottori jishin) occurred in Tottori prefecture, Japan at 17:36 local time on September 10, 1943. 1943 Tottori earthquake (M7.2). We use a layered viscoelastic half-space model (Wang et al. 1943 Tottori earthquake: part our commitment to scholarly and academic excellence, all articles receive editorial review.|||... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled. "Significant Earthquake". The Tottori plain, the target area for this study, is an important factor for the prevention or mitigation of earthquake disasters. The trace of the 1943 surface rupture exhibited the large step and quite sinuous geometry compared with other strike-slip surface breaks. Kanamori, 1972), the 1983 Central Tottori earthquake (M6.2) (e.g. This earthquake has been studied by many Japanese seismologists, especially by the late Prof. Masayuki Kikuchi. The records of the Tottori earthquake of 1943 (M = 7.4, 35.5° N, 134.2° E, depth 10 km) about by a low-magnification seismograph at a relatively short distance are used to determine dynamics fault parameters such as the particle velocity and the effective tectonic stress, in addition to static fault parameters such as the dislocation and the stress drop. The local timezone is named " Asia/Tokyo " with a UTC offset of 9 hours. Materials exposed in the trenches included silts, sands, gravels of mostlyalluvial deposits and soils. If you would like to participate, please visit the project page, where you can join the project, participate in relevant discussions, and see lists of open tasks.Current time in Japan: 21:43, March 15, 2021 (JST, Reiwa 3) The severely damaged area was concentrated on the Tottori plain (Architectural Institute of Japan, 1944), whereas there was less damage in the western and southern parts of Tottori City. The Tottori earthquake had its epicenter offshore from Ketaka District, now part of Tottori, and registered a magnitude of 7.0 on the Moment magnitude scale. 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