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1586 Tenshō earthquake

Coordinates: 36°00′N 136°54′E / 36.0°N 136.9°E / 36.0; 136.9
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1586 Tenshō earthquake
Local dateJanuary 18, 1586 (1586-01-18)
Local time23:00 JST
Magnitude7.9 MJMA
Epicenter36°00′N 136°54′E / 36.0°N 136.9°E / 36.0; 136.9[1]
Max. intensityJMA 7
Tsunami5 m (16 ft)
Casualties8,000 dead (est.)

The Tenshō earthquake (Japanese: 天正地震, Hepburn: Tenshō Jishin) occurred in Japan on January 18, 1586 at 23:00 local time. This earthquake had an estimated seismic magnitude (MJMA) of 7.9,[2] and an epicenter in Honshu's Chūbu region. It caused an estimated 8,000 fatalities and damaged 10,000 houses across the prefectures of Toyama, Hyōgo, Kyōto, Osaka, Nara, Mie, Aichi, Gifu, Fukui, Ishikawa and Shizuoka.[3] Historical documentation of this earthquake was limited because it occurred during the Sengoku period.

Tectonic setting

The island of Honshu is situated in a region of complex plate convergence between the Pacific, Amurian, Philippine Sea and Okhotsk Plates. While a large component of the convergence is accommodated by subduction along the Nankai and Japan Trenches, shallow intraplate deformation occur as well. The Japan Median Tectonic Line and Itoigawa-Shizuoka Tectonic Line are two major fault zones that accommodate this deformation. These faults are associated with strike-slip and dip-slip faulting.[4]

Earthquake

Landslide scars visible on Mount Sarugabanba.

The origin of the Tenshō earthquake is not known, but geologists have presented different faults to be the possible source. There is still debate about which fault zone caused the earthquake and even how did the earthquake unfold, through a single fault system rupture or even a multiple fault system rupture, given the massive death and destruction across wide areas of the Tōkai, Kinki, and Hokuriku regions.[2] An analysis of the meizoseismal area suggest the source area was approximately 180 km × 60 km (112 mi × 37 mi) extending north-northeast–south-southwest from Wakasa Bay to Ise Bay.[5] The same region was also the source area of the 1891 Mino–Owari earthquake.

Geology

The Atera Fault System that runs through the Chūbu region is a north-northeast–south-southwest-striking left-lateral fault with a length of 60–70 km (37–43 mi) that ruptured during the event.[6][7] Present data suggest seismicity on the fault is low, with long recurrence intervals between major earthquakes of ~1,800 years.[6] Soil surveys have found evidence that the fault ruptured in 1586.[8] The forested area in the region showed evidence of en-echelon fractures. A nearby sag pond is also thought to have formed from the earthquake that has now been converted into a paddy field. Paleoseismic trenching and radiocarbon dating revealed that the last seismic event on the fault occurred between 1400 and 1600.[9] This date corresponded to the 1586 earthquake as no other reports of a severe earthquake in the region occurred at around this time.[9] Further surveys revealed that another structure, the Miboro Fault, a northwest strand of the Atera Fault was also involved in the earthquake, bringing the estimated rupture length to 85 km (53 mi).[7] The suggested epicenter is located near the northwest part of Gifu Prefecture, based on analyzing the damage distribution.

An 1879 woodblock print in Yoshitoshi's Mirror of Famous Generals of Great Japan depicting Toyotomi Hideyoshi being rescued by Katō Kiyomasa during the 1596 earthquake.

Additional surveys and drilling found that the Yōrō-Kuwana-Yokkaichi Fault Zone to the west of the Nōbi Plain may have also ruptured, and corresponds to reports of severe damage in the vicinity.[10] There is also evidence that the last earthquake on that fault zone could have happened between the 13th and 16th century, and it hence corresponds to the time of the earthquake (1586). The Yōrō-Kuwana-Yokkaichi Fault Zone is a group of three reverse faults beneath the Nōbi Plain with a total length of 55 km (34 mi). Evidence of faults was further supported by the presence of vertical displacements reflected in the sedimentary layers of the plain. The fault zone was also responsible for an earthquake in 745 AD (ja), and ten additional events within the past 6,000 years.[11] The blind Yōrō Fault located along the eastern base of the Yōrō Mountains was also identified as a source of the quake. Fold scarps measuring up to 2 m (6 ft 7 in) high formed during the event was discovered to have extended 60 km (37 mi) in length.[12]

The disappearance of islands at the mouth of the Kiso River in Ise Bay was attributed to liquefaction and tsunami, caused by slip on the Ise Bay and Ise Bay Mouth Faults, located undersea.[4]

Foreshocks and aftershocks

A foreshock occurred on November 27, 1585 and is thought to have triggered the mainshock two months later.[13] The foreshock had an estimated magnitude of 6.6.[13][14] The earthquake caused aftershocks that were felt in Kyoto every day for two months. Two strong earthquakes rocked the region in 1589 and 1596 (ja), but were less destructive.[15] The latter event had a magnitude of 7.5 and resulted in at least 1,100 fatalities in Kyoto and Sakai.[16]

Tsunami

A tsunami was reported in Lake Biwa, Wakasa Bay and Ise Bay,[17] however these may have been seiches as the rupture did not extend offshore.[18] A run-up height of 3 m (9.8 ft) was recorded at Ise Bay, while at Wakasa Bay, the tsunami was estimated to be 4–5 m (13–16 ft).[5]

A wave was reported along the coast of Lake Biwa, slamming into homes and washing away many residents in Nagahama. The wave destroyed much of the city and flooded Nagahama Castle. There were over 8,000 fatalities in Ise Bay due to the tsunami.[19][20][21] Multiple fatalities was recorded in Toyama Bay and along the Shō River.[22] Analysis of sedimentary layers at Lake Suigetsu found no evidence of seawater entering the lake.[23] A 2015 study found tsunami deposits in a paddy field in Ōi District, Fukui Prefecture dating to between the 14th and 16th centuries which corresponds to the event.[24]

Records of the tsunami are sparse and it was misattributed to a destructive wave along the Sanriku coast in a tsunami catalog in 1586.[25][26][27] The 1586 Sanriku tsunami is regarded as a false event as there are no historical documentation of such an event in 1586.[28] The tsunami was also misattributed to a Peruvian earthquake the same year.[29] Historical records support the occurrence of a tsunami along the Sanriku coast in June 1585,[29] which has been attributed to a large earthquake in the Aleutian Islands.[30]

Damage

A monument of the Kaerikumo Castle, buried by an earthquake-triggered landslide. The landslide scar is visible in the background.

The earthquake had a maximum JMA intensity of Shindo 6–7 extending from the Noto Peninsula to Lake Biwa.[5][31] Extreme damage was reported between Nara, Osaka, Toyama and Shizouka. Large conflagrations broke out as a result. Large-scale landslides occurred in the northern part of the damage zone which was dominated by mountains. A fortress was completely wiped out by one of these landslides, while another collapsed during the tremors.[31] A triggered landslide on Kaerikumoyama buried the Kaerikumo Castle and 300 houses,[32] killing 500 people.[33] The Ōgaki Castle was destroyed by a fire.[34] The only daughter of Yamauchi Kazutoyo was killed in Nagahama.[35]

There were reports that a few small islands in the Kiso River vanished as a result of soil liquefaction and subsequent subsidence which caused water to submerge the islands while a tsunami was generated in Ise Bay, drowning thousands.[31] At the location of present-day Nagoya, extensive soil liquefaction took place. Sand volcanoes and dykes were recorded and discovered at locations in the plain.[31] Significant destruction was reported in Kyoto, but its temples sustained minor damage.[31] The Tō-ji temple in the city was seriously damaged and over 600 Buddha statues in Sanjūsangen-dō were destroyed.[36] A Christian missionary in the region reported that 60 homes were destroyed at Sakai.[3] Movement of faults and shaking severely deformed the Kiso Three Rivers, resulting in a drastic change in its course.[37]

See also

References

  1. ^ Miyazawa, Masatoshi; Mori, Jim (2006). "Historical Maximum Seismic Intensity Maps in Japan from 1586 to 2004: Construction of Database and Application" (PDF). Seismological Research Letters. 77 (2): 154–158. doi:10.1785/gssrl.77.2.154. Archived (PDF) from the original on 2022-05-31. Retrieved 2022-05-22.
  2. ^ a b Yamamura, Norika; Kano, Yasuyuki (2020). "1586年天正地震の震源断層推定の試み: 液状化履歴地点における液状化可能性の検討から" [Source Fault Estimation of the 1586 Tensho Earthquake by Evaluating the Possibility of Liquefaction]. Zisin (Journal of the Seismological Society of Japan). Second Series (in Japanese). 73. Seismological Society of Japan: 97–110. doi:10.4294/zisin.2019-7. S2CID 229523816. Archived from the original on 2022-05-22. Retrieved 2022-05-22.
  3. ^ a b National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K, archived from the original on 2021-11-29, retrieved 2021-02-11
  4. ^ a b Kanaori, Y. (2000). "Seismic risk assessment of an active fault system: the example of the Tsurugawan–Isewan tectonic line". Engineering Geology. 56 (1–2): 109–123. doi:10.1016/S0013-7952(99)00137-4. Archived from the original on 23 May 2022. Retrieved 23 May 2022.
  5. ^ a b c Hatori, Tokutaro (2015). "1586 年天正地震の震源域と津波" [Estimated Source Area of the 1586 Tensho Earthquake and Tsunami] (PDF). Historical Earthquake (in Japanese). 30: 75–80. Archived (PDF) from the original on 2022-04-23. Retrieved 2022-05-23.
  6. ^ a b Yabe, Yasuo; Yamamoto, Kiyohiko; Sato, Namiko; Omura, Kentaro (2010). "Comparison of stress state around the Atera fault, central Japan, estimated using boring core samples and by improved hydraulic fracture tests". Earth, Planets and Space. 62 (3): 257–268. Bibcode:2010EP&S...62..257Y. doi:10.5047/eps.2009.12.002. S2CID 55740982. Archived from the original on 2022-05-23. Retrieved 2022-05-23.
  7. ^ a b Eds. Y. Fujinawa and A. Yoshida (2002). "Rupturing History of Active Faults during the Last 1000 Years in the Central Japan" (PDF). Seismotectonics in Convergent Plate Boundary: 209–218. Archived from the original (PDF) on 2007-09-25. Retrieved 2021-02-03 – via Terra Scientific Publishing Company.
  8. ^ Headquarters for Earthquake Research Promotion Earthquake Research Committee (2004). "Long-term evaluation of the Atera fault zone" (PDF). The Headquarters for Earthquake Research Promotion (in Japanese). Archived (PDF) from the original on 2011-03-22. Retrieved 9 February 2021.
  9. ^ a b Yamashita, Futoshi; Mizoguchi, Kazuo; Fukuyama, Eiichi; Omura, Kentaro (2010). "Reexamination of the present stress state of the Atera fault system, central Japan, based on the calibrated crustal stress data of hydraulic fracturing tests obtained by measuring the tensile strength of rocks". Journal of Geophysical Research. 115 (B4). American Geophysical Union. Bibcode:2010JGRB..115.4409Y. doi:10.1029/2009JB006287.
  10. ^ Headquarters for Earthquake Research Promotion Earthquake Research Committee (2001). "Long-term evaluation of the Yōrō-Kuwana-Yokaichi fault zone" (PDF). The Headquarters for Earthquake Research Promotion (in Japanese). Archived (PDF) from the original on 2011-03-22. Retrieved 9 February 2021.
  11. ^ Niwa, Yuichi; Sugai, Toshihiko; Yasue, Ken-ichi (2012). "Activity of the Yoro Fault System Determined from Coseismic Subsidence Events Recorded in the Holocene Delta Sequence of the Nobi Plain, Central Japan". Bulletin of the Seismological Society of America. 102 (3): 1120–1134. Bibcode:2012BuSSA.102.1120N. CiteSeerX 10.1.1.901.1662. doi:10.1785/0120110211. Archived from the original on 22 May 2022.
  12. ^ Ishiyama, Tatsuya; Mueller, Karl; Sato, Hiroshi; Togo, Masami (2007). "Coseismic fault-related fold model, growth structure, and the historic multisegment blind thrust earthquake on the basement-involved Yoro thrust, central Japan". Journal of Geophysical Research. 112 (B3). American Geophysical Union. Bibcode:2007JGRB..112.3S07I. doi:10.1029/2006JB004377. Archived from the original on 2022-05-23. Retrieved 2022-05-23.
  13. ^ a b Iida, Kumizi (1987). 天正大地震誌 (in Japanese). Nagoya University Press. p. 560. ISBN 4930689597.
  14. ^ Muramatsu, Ikuei (1998). "天正地震の震源について" [Epicenter of the Tensho Earthquake]. Seismological Society of Japan Autumn Proceedings (in Japanese). C54.
  15. ^ Imamura, Akitune (1928). "Further Note on the Seismic Activity of the Northern Part of Central Japan". Proceedings of the Imperial Academy. 4 (8). University of Tokyo: 485–488. doi:10.2183/pjab1912.4.485. Archived from the original on 2022-05-23. Retrieved 2022-05-23.
  16. ^ "日本付近のおもな被害地震年代表" [Japan Historical Earthquakes Representative]. Seismological Society of Japan. Archived from the original on 2 June 2021. Retrieved 24 May 2022.
  17. ^ 外岡慎一郎 (2013). "越前・若狭の歴史地震・津波～年表と史料" (PDF). 敦賀論叢 (27号). Archived (PDF) from the original on 2017-08-09. Retrieved 2022-05-22.
  18. ^ Okada, Atsumasa (2011). "天正地震とこれを引き起こした活断層" [The Tensho earthquake and the active fault that caused it]. Active Fault Research (in Japanese). 35: 1–13. doi:10.11462/afr.2011.35_1. Archived from the original on 2022-05-22. Retrieved 2022-05-22.
  19. ^ National Geophysical Data Center / World Data Service (NGDC/WDS), Global Historical Tsunami Database (Data Set), NOAA National Centers for Environmental Information, archived from the original on 2022-05-31, retrieved 2022-05-22
  20. ^ 東京大学地震研究所 『日本地震史料 続補遺』 日本電気協会、1993年
  21. ^ 『長島町史』 1978年
  22. ^ （富山県）上市町史編纂委員会 (1970). 上市町史. 上市町. p. 1117.
  23. ^ Saito, Megumi; Yamada, Kazuyoshi; Staff, Richard; Nakagawa, Takeshi; Yonenobu, Hitoshi; Haraguchi, Tsuyoshi; Takemura, Keiji; Ramsey, Christopher (2013). "水月湖ボーリングコアを用いた天正地震（AD1586）前後の湖底堆積物の分析" [An assessment of the magnitude of the AD 1586 Tensho Tsunami inferred from Lake Suigetsu sediment cores]. Journal of Geography (Chigaku Zasshi). 122 (3): 493–501. doi:10.5026/jgeography.122.493. Archived from the original on 2022-05-23. Retrieved 2022-05-23.
  24. ^ Yamamoto, Hirofumi; Honjo, Sho; Sasaki, Naohiro; Urabe, Atsushi (2016). "若狭湾沿岸で見出された津波堆積物" [Tsunami deposits found along the coast of Wakasa Bay]. 123rd Academic Conference (2016 Tokyo Sakurajosui) (in Japanese). 2016. Tokyo, Japan: Geological Society of Japan. doi:10.14863/geosocabst.2016.0_035. Archived from the original on 2022-05-23. Retrieved 2022-05-23.
  25. ^ 天正13年5月14日にも三陸沿岸に津波が来襲したという
  26. ^ 吉村昭「三陸海岸大津波」文春文庫版p60(2)
  27. ^ "昭和八年三月三日 三陸沖強震及津波報告". Archived from the original on 2021-09-19. Retrieved 2022-05-23.
  28. ^ Yoshinobu Tsuji (2013). "Catalog of Distant Tsunamis Reaching Japan from Chile and Peru". Report of Tsunami Engineering. 30: 61–68. CiteSeerX 10.1.1.723.1716.
  29. ^ a b Kenji Satake; Mohammad Heidarzadeh; Marco Quiroz; Rodrigo Cienfuegos (2020). "History and features of trans-oceanic tsunamis and implications for paleo-tsunami studies". Earth-Science Reviews. 202 (103112): 103112. Bibcode:2020ESRv..20203112S. doi:10.1016/j.earscirev.2020.103112. S2CID 212778611. Archived from the original on 9 July 2021. Retrieved 8 July 2021.
  30. ^ Rhett Butler; David A. Burney; Kenneth H. Rubin; David Walsh (2017). "The orphan Sanriku tsunami of 1586: new evidence from coral dating on Kaua'i". Natural Hazards. 88 (2): 797–819. doi:10.1007/s11069-017-2902-7. S2CID 134237666.
  31. ^ a b c d e T. Moreno, S.R. Wallis, T. Kojima, W. Gibbons (2016). The Geology of Japan. London: The Geological Society. ISBN 9781862397439. Archived from the original on 2023-10-24. Retrieved 2021-12-14.{{cite book}}: CS1 maint: multiple names: authors list (link)
  32. ^ "帰雲城" (in Japanese). ニッポン旅マガジン. 4 May 2021. Archived from the original on 29 November 2022. Retrieved 28 May 2022.
  33. ^ "幻の帰雲城" (in Japanese). Shirakawa village. 2012. Archived from the original on 25 May 2022. Retrieved 22 May 2022.
  34. ^ Sangawa, Akira (2011). 地震の日本史―大地は何を語るのか [Japanese History of Earthquakes - What Does the Earth Tell?] (in Japanese). Tankobon. ISBN 978-4121919229.
  35. ^ Unkawa, Yuzu (9 August 2021). "戦国大名の運命を大きく変えた大災害「天正地震」秀吉は家康への総攻撃を中止に？". Japaaan Magazine (in Japanese). Archived from the original on 31 May 2022. Retrieved 22 May 2022.
  36. ^ Utsu, Tokuji; Shima, Etsuzo; Yoshii, Toshiyoshi; Yamashina, Kenichiro (2001). 地震の事典. Asakura Shoten.
  37. ^ Nishimura, Katsuhiro; Okuda, Masao; Kani, Yukihiko; Nakane, Yoji; Hayakawa, Kiyoshi (2015). "Midstream of Kiso river affected by Tensho mega-earthquake" (PDF). Christchurch, New Zealand: 6th International Conference on Earthquake Geotechnical Engineering. Archived (PDF) from the original on 31 May 2022. Retrieved 22 May 2022.
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