Menu
Home
Log in / Register
 
Home arrow Geography arrow Seismic Japan

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. It was an ocean trough earthquake originating somewhere between Sagami Bay and the area off the southern shore of the Bōsō Peninsula. It was the same type as the Great Kantō Earthquake of 1923, one of the M8 class earthquakes whose origins are the ocean troughs caused by the Philippine Sea Plate subducting beneath the Eurasian Plate and the North American Plate. These earthquakes typically are damaging in and of themselves, and they usually generate tsunamis. In the case of the Genroku earthquake, tsunamis of between 2 and 10.5 meters in height struck the coast between Shimoda and Inuboesaki, washing approximately six hundred to their deaths near Kamakura. The total death toll from the seismic sea waves probably numbered in the thousands. Shaking could be felt as far away as the Kinki region, and the earthquake and tsunami destroyed over twenty-eight thousand structures. This earthquake caused uplift in the southern part of the Bōsō Peninsula by as much as 5.5 meters.[1] Daimyō mansions on solid ground such as the Yamanote area suffered relatively light damage, whereas alluvial areas of Shitamachi suffered severe damage.[2] This earthquake prompted a change of era name from Genroku to Hōei.

Hoei, 1707 (Hoei 4)/10/4

The change of era names, however, did not mollify the cosmic forces. On October 28, 1707, nearly the entire Nankai Trough plate boundary ruptured at once. Until March 11, 2011, many specialists regarded the resulting M8.4 Hōei earthquake as the strongest seismic event to shake Japan. It caused at least five thousand deaths and possibly as many as fifteen thousand. It generated tsunamis from the Izu Peninsula to Kyushu, and the waves reached heights of five to eight meters in Shikoku. They washed away nearly eighteen thousand homes and destroyed some three thousand boats and ships. Uplift and subsidence were common throughout Shikoku. Tsuro and Murozu harbors in Murodozaki (Tosa) experienced about 1.8 meters of uplift, and a twenty-square-kilometer area near Kōchi sank by about 2 meters.[3]

Sanjo(Echigo), 1828 (Bunsei 11)/11/12

At about 7 a.m. on a market day, December 18, 1828, the earth around Sanjō in Echigo (Niigata Prefecture) began to shake. The M6.9 inland, shallow-focus earthquake caused liquefaction (many buildings sank about one meter into the earth), landslides, and fissures in the earth from which water and sand flowed. The earthquake caused 1,443 deaths, collapsed 9,808 structures, and burned 1,204 more. The shaking began just after many merchants in the marketplace had started their fires to prepare food, and many fled without extinguishing them. Soon the whole town was ablaze, and the cries of trapped victims mingled with cries of those chanting the
name of Amida Buddha.[4] One account mentioned the anguished sounds of horses and cows amidst smoke and people drowning in flooded pits that had opened in the ground.[5]

Kyoto, 1830 (Bunsei 13/Tenpo1)/7/2

At roughly 4 p.m. on August 19, 1830, an inland earthquake of approximately M6.5 shook Kyoto. The epicenter was slightly to the northwest of the city. Kyoto's death toll in 1830 was between two and three hundred. Heavy shaking was limited to the city itself, although some outlying areas experienced minor damage and the earthquake was felt in nearby cities such as Osaka. Destruction of storehouses was widespread, but destruction of houses was relatively modest. Nijō Castle suffered serious damage, and liquefaction was widespread throughout the city.[6] As was usual by this time, there were reports of light flashes in the sky and bursts of light issuing forth from the earth.[7]

  • [1] Okada, Jishin chizu, 86–87; Itō, Jishin to funka no Nihonshi, 80–91; Sangawa, Jishin no Nihonshi, 134–137; and Usami, Higai jishin, 65–70. For diaries, official chronicles, and other accounts of the earthquake and its damage, see DNJS, vol. 1 (kō), 281–307.
  • [2] Sangawa, Jishin no Nihonshi, 136. For a detailed account of damage to daimyō and hatamoto mansions, see “Kanrosō,” in DNJS, vol. 1 (kō), 290.
  • [3] Okada, Jishin chizu, 169–170; Sangawa, Jishin no Nihonshi, 138–141; Itō, Jishin to funka no Nihonshi, 81; and Usami, Higai jishin, 75–90.
  • [4] Okada, Jishin chizu, 56; Sangawa, Jishin no Nihonshi, 158–162; Usami, Higai jishin, 130–131; and Hashomoto Manpei, Jishingaku no kotohajime: kaituakusha Sekiya Seikei no shōgai (Asahi shinbunsha, 1983), 40.
  • [5] “Chōshin hiroku, jōkan,” in Usami Tatsuo, ed., “Nihon no rekishi jishin shiryō” shūi (hereafter NRJSS), vol. 3, 211.
  • [6] Sangawa, Jishin no Nihonshi, 162; Itō, Jishin to funka no Nihonshi, 187–190; Usami, Higai jishin, 131–132; and Miki Haruo, Kyōto daijishin (Shibunkaku shuppan, 1979), 4–48, 115–250. Miki argues that an accurate count of the dead is impossible. See also DNJS, vol. 1 (kō), 533–589.
  • [7] Musha kinkichi, Jishin namazu (Meiseki shoten, 1995, originally 1957), 55.
 
Found a mistake? Please highlight the word and press Shift + Enter  
< Prev   CONTENTS   Next >
 
Subjects
Accounting
Business & Finance
Communication
Computer Science
Economics
Education
Engineering
Environment
Geography
Health
History
Language & Literature
Law
Management
Marketing
Mathematics
Political science
Philosophy
Psychology
Religion
Sociology
Travel