2003 Tokachi earthquake
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   Kushiro Map showing the epicenter of the mainshock | |
| UTC time | 2003-09-25 19:50:06 |
|---|---|
| ISC event | 7134409 |
| USGS-ANSS | ComCat |
| Local date | 26 September 2003 |
| Local time | 04:50 |
| Magnitude | 8.3 Mw[1] |
| Depth | 27 km (17 mi) |
| Epicenter | 41°47′N 143°52′E / 41.78°N 143.86°E |
| Type | Megathrust |
| Areas affected | Japan |
| Total damage | ¥213 billion (US$1.9 billion)[2] (Damage to fishing ports, agriculture, and infrastructure) |
| Max. intensity | MMI IX (Violent)[3] JMA 6− |
| Peak acceleration | 1.11 g 1091 Gal |
| Tsunami | Yes (4.0 m) |
| Landslides | Yes |
| Aftershocks | 65+ (max 7.4 Mw) |
| Casualties | 1 dead (indirect), 849 injured, 2 missing[4] |
The 2003 Hokkaidō earthquake, scientifically named the 2003 Tokachi-Oki earthquake (十勝沖地震, 2003 Tokachi-Oki Jishin), occurred off the coast of Hokkaidō, Japan on 26 September at 04:50 local time (19:50 UTC 25 September). At a focal depth of 27 km (17 mi), this great undersea earthquake measured 8.3 on the moment magnitude scale, making it the most powerful earthquake of 2003, as well as one of the most intense earthquakes to hit Japan since modern record-keeping began in 1900.
The Hokkaido earthquake caused extensive damage, destroying roads all around Hokkaidō, and triggered power outages and extensive landslides.[1] Over 800 people were injured.[5] The earthquake also caused a tsunami reaching 4 meters in height.[6] The earthquake's presence was felt throughout Japan, stretching all the way to Honshu and Tokyo.[1]
Tectonic setting
The location and moment tensor solution of this earthquake are consistent with it being a result of thrust faulting between the North American Plate and the subducting Pacific Plate. In addition to experiencing large thrust earthquakes that originate on the interface between the plates, eastern Hokkaidō experiences great earthquakes that originate from the interior of the subducted Pacific plate.
The region experienced a catastrophic earthquake and tsunami with an estimated magnitude of 9 in 1667,[7] a magnitude 8.2 event in 1952,[8] a 1968 quake measuring 8.3 Mw , and one in 2008 measuring 7.1, all bearing the name Tokachi-Oki,[8] and a 1973 quake to the immediate north along the Kuril Trench plate boundary called the 1973 Nemuro earthquake.
Aftershocks
As of 3 October 2003, a total of 65 aftershocks were reported near the main shock epicenter. At least one major tremor occurred, measuring magnitude 7.0 on the Richter scale.[9] At the time, specialists assessed a 50% probability of an aftershock of magnitude 6.0 or greater to occur within the subsequent 72 hours, with a 20% chance of its magnitude exceeding 7.0.
Damage and casualties
Despite the earthquake's great intensity, structural damage to the region was comparatively light; the epicenter was located nearly a hundred kilometers offshore, with most structures in its vicinity reported to be resistant to earthquake shaking.[10] The majority of the destruction was confined to coastal areas, such as sea and fishing ports, mostly inflicted by subsequent tsunami waves. Although soil liquefaction was observed over a broad geological area, it occurred in localized areas almost exclusively limited to man-made embankments.[11] The earthquake affected a total of 36 local rivers, including the major Abashiri and Ishikari Rivers.[4] Many properties received considerable damage, two individuals remain missing and 849 people sustained injuries. Monetary losses in Hokkaido amounted to at least ¥213 billion (2003 JPY), or $1.9 billion (2003 USD[12]).[2] One person died after being hit by a car after cleaning up earthquake damage.[13]
Structures
The earthquake and its associated tsunami waves destroyed several oceanside home communities and damaged many others. Over 1,500 houses or buildings – the majority of which were in Kushiro city – suffered considerable damage, with of a total of 141 reported to be partially or completely destroyed.[2] Strong shaking affected many bridges in the region, some sustaining severe damage due to relative motion between spans in excess of design standards.[11] The center of the Rekifune Bridge, located in Taiki, Hiroo, was reported to have sunk about 0.12 m (0.39 ft) at the joint section following significant ground deformation. Some local schools were also damaged, ranging from shattered windows to severed expansion joints and columns. Two town halls in Kushiro and Taiku suffered partial collapses.[10]
At Kushiro Airport, the tremor caused the control tower ceiling to collapse, prompting officials to halt control work for several days. Small cracks were reported in the gates of the Takami Hokkaidō Dam, though no threat of dam failure existed.[4]
Harbour facilities
Several sea ports in the area sustained moderate damage – such as cracks and wall collapse – due to lateral ground spreading caused by liquefaction. Some 123 coastal fishing ports and facilities in eastern Hokkaidō reported significant damage, with an additional 25 ports damaged in Iwate.[4] At least three major ports were affected by the disaster; Kushiro Port sustained great damage to one of its piers as a result of ground displacement and sand boils.[14] Tsunami waves stranded several small boats onshore; various ship containers and oil tanks along coastlines sustained damage. The earthquake left marine oil spills in its wake, though the conditions were quickly normalized.[15]
See also
References
- ^ a b c "2003 Hokkaido earthquake". USGS. 3 October 2003. Archived from the original on 2008-08-28. Retrieved 2008-07-12.
- ^ a b c 被害の概要 (PDF) (in Japanese). Kiso-Joban Company. 2003. p. 1–2. Archived from the original (PDF) on 2012-03-24. Retrieved 2011-05-18.
- ^ Kenji Hirata; Yuichiro Tanioka; Kenji Satake; Shigeru Yamaki; Eric L. Geist (2004). "The tsunami source area of the 2003 Tokachi-oki earthquake estimated from tsunami travel times and its relationship to the 1952 Tokachi-oki earthquake". Earth, Planets and Space. 56 (3): 367–372. Bibcode:2004EP&S...56..367H. doi:10.1186/BF03353066. S2CID 55586940.
- ^ a b c d 平成１５年（２００３年）十勝沖地震について (PDF) (in Japanese). MLIT. 2003-10-03. p. 6–7. Retrieved 2011-05-17.
- ^ S. F. A. Rafeeqi and S. H. Lodi (April 2004). "Earthquakes Cause Damages in Pakistan, Iran, Japan and Morocco" (PDF). Cowasjee Earthquake Study Centre. Archived from the original (PDF) on October 4, 2006. Retrieved May 20, 2012.
- ^ "List of 2003 tsunamis". International Tsunami Information Center. 2005. Archived from the original on 2012-02-13. Retrieved 2008-07-12.
- ^ AIST (December 10, 2004). "Transient Uplift After a 17th-Century Giant Earthquake in Hokkaido" (Press release). Archived from the original on April 20, 2012. Retrieved May 20, 2012.
- ^ a b "かがくナビ > 読む > 科学よみもの > 地球科学現象の解明に役立つ地震研究". www.kagakunavi.jp. Archived from the original on 16 March 2012. Retrieved 15 January 2022.
- ^ Kitano, Masayuki (26 September 2003). "Quake in Japan Injures 270". Independent Online. Retrieved 24 June 2011.
- ^ a b EQE Japan Division (2003). "The 2003 Tokachi-oki Earthquake of September 26" (PDF). American Bureau of Shipping. pp. 1, 19. Archived from the original (PDF) on 2011-09-28. Retrieved 2011-05-18.
- ^ a b "EERI Newsletter Volume 37, Number 11" (PDF). EERI. November 2003. Retrieved 2011-06-01.
- ^ "Monthly exchange rate average (Japanese Yen, American Dollar) 2003". x-rates.com. Retrieved 2011-05-18.
- ^ "Strong quake hits north Japan". BBC News. 26 September 2003.
- ^ "Preliminary Observations on the Tokachi-Oki, Japan Earthquake of September 26, 2003" (PDF). EERI. December 2003. Retrieved 2011-06-01.
- ^ 釧路沖を震源とする地震について (PDF) (in Japanese). Cabinet Office, Government of Japan. 2003-09-26. p. 4. Archived from the original (PDF) on 2011-09-28. Retrieved 2011-05-18.
External links
- The International Seismological Centre has a bibliography and/or authoritative data for this event.
- ReliefWeb's main page for this event.