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2007 Noto earthquake

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2007 Noto earthquake
能登半島地震
2007 Noto earthquake
2007 Noto earthquake
UTC time2007-03-25 00:41:57
ISC event11703278
USGS-ANSSComCat
Local dateMarch 25, 2007 (2007-03-25)
Local time9:41:48 JST (UTC+09:00)
DurationAbout 30 seconds[1]
Magnitude6.9 Mj (6.7 Mw)[2]
Depth11 km (7 mi)
Epicenter37°18′N 136°30′E / 37.3°N 136.5°E / 37.3; 136.5Coordinates: 37°18′N 136°30′E / 37.3°N 136.5°E / 37.3; 136.5
TypeIntraplate
Areas affectedJapan
Max. intensityIX (Violent)[3]

JMA 6+
Peak acceleration0.96 g
TsunamiUp to 22 cm in Suzu
LandslidesYes
Aftershocks500~
Casualties1 dead, 356 injured[4]

The 2007 Noto earthquake (Japanese: 能登半島地震) is an earthquake that occurred on March 25, 2007 in Japan.

Overview

At 9:41:58 a.m. on March 25, 2007, a magnitude 6.9 earthquake struck the Hokuriku region of Japan, near the Noto Peninsula. The earthquake shook the city of Wajima, the city of Nanao, and the town of Anamizu with a seismic intensity of 6+ on Japan's shindo scale.[5] One death, in the city of Wajima, and at least 356 injuries have been reported.[4]

Geology

This earthquake was the result of oblique-slip faulting.[6] According to the Geospatial Information Authority of Japan, the fault was 21 km long, 14 km wide and shifted 1.4 m.[6] By using sound waves, the National Institute of Advanced Industrial Science and Technology also found a fault 18~ km long that is supposed to have caused this earthquake.[7]

This earthquake was an intraplate earthquake that occurred within the Eurasia Plate, near the boundary with the North American Plate. Noto Peninsula itself was created by pressure pushing up sediment from the south-east, and many folds and reverse faults are in the area. Some strike-slip faults are also found in the area. A 6.6 Mj earthquake also struck Ishikawa Prefecture on February 7, 1993.

Since the 1990s, the number of earthquakes with a magnitude of 6.0~ Mj are increasing. Some seismologists say that the seismic activity in West Japan is at its peak, and many earthquakes will occur, like the Great Hanshin earthquake. This earthquake is sometimes considered as one of those earthquakes.[citation needed]

Like the 2005 Fukuoka earthquake, it was announced that it "occurred in an area where seismic activity was relatively quiet", but earthquakes are possible anywhere in Japan and its surrounding areas. Also this earthquake's fault was out in sea, so it was not simulated in the seismic danger maps, since most of the faults simulated are inland faults. Some seismologists are trying to simulate these kind of earthquakes as well as inland earthquakes.[citation needed]

Frequency

This type of earthquake was estimated to have occurred 1~2 times in the last 20,000 years.[7]

Main shock

USGS ShakeMap for the event
USGS ShakeMap for the event

The Japan Meteorological Agency placed the earthquake at 37.3°N, 136.5°E, at a depth of 11 km. It estimated the magnitude at 7.1, but later revised its estimate to 6.9. The earthquake had a maximum three-component vector sum peak ground acceleration of 1,304 cm/s2 (1.33 g).[8] It occurred in a big seismic gap. Shaking in Wajima was very close to Shindo 7. It was the first time that Shindo 6- or more was observed in Ishikawa prefecture. It was also the 2nd time that Shindo 5- or more was observed in Toyama prefecture.

Geophysical effects

The earthquake moved Shika 25 cm southwest, and Anamizu 15 cm northwest.[6] It also shifted an erosion terrace formed in the ice age and the sediment on top by 10 cm.

Extent

Shaking was felt as far as Oshamanbe in the north, to Hiroshima in the west and Nahari in the south.[5]

Damage

According to the National Research Institute for Earth Science and Disaster Prevention, the pattern of the shaking was similar to the shaking in the Great Hanshin earthquake and the 1994 Northridge earthquake, called the "killer pulse": Pulse waves with a frequency of 1–2 seconds. This kind of shaking heavily damages buildings with around 2 floors. The shaking then got larger as it reached softer ground like alluvial plains, causing major damage.

Board that shows the damage and repairs made on the Noto Toll Road
Board that shows the damage and repairs made on the Noto Toll Road
Besshyo Service Area immediately after the earthquake
Besshyo Service Area immediately after the earthquake
  • A 52-year-old woman died after a tōrō (stone lantern) collapsed and hit her head in Wajima.[1][9]
  • 25 track ballasts on the Noto Line were shifted after the earthquake.
  • 22 cracks were found in the runway of Noto Airport. The runway was repaired by March 26.
  • Some parts of the Noto Toll Road collapsed, making people leave their cars on the road after they evacuated. The roads were completely repaired by November 30.
  • According to estimates about 110,000 houses had power outages, 13,250 houses had no water supply, and 260 houses' phones stopped working.
  • Many other houses had no gas supply after the earthquake.
  • Soil liquefaction was confirmed at the coasts near the epicenter and Himi port.
  • Some people were trapped in elevators that stopped after the earthquake.

Ishikawa Prefecture (as of July 17, 2007)

Casualties Structural
Damage
Evacuation
Centers
Shindo
Deaths Serious Injuries Minor Injuries Collapsed Half Collapsed Partially Damaged
Anamizu[note 1] 0 3 36 72 94 2,197 3 6+
Wajima 1 46 69 503 1,057 9,984 6
Nanao 0 17 110 50 252 6,493 0
Noto 0 2 10 1 10 1,018 0 6-
Nakanoto 0 3 0 3 7 1,524 0
Shika 0 10 27 14 217 3,385 1
Suzu 0 0 3 2 13 769 0 5+
Kahoku 0 0 0 3 2 18 0 5-
Hōdatsushimizu 0 0 0 0 3 25 0
Hakui 0 0 1 3 13 133 0
Hakusan 0 0 0 0 0 1 0 4
Tsubata 0 0 1 0 0 2 0
Kaga 0 0 0 0 0 6 0
Total 1 81 257 649 1,655 24,959 10 Max 6+

Toyama Prefecture (as of March 28, 2007)

Casualties Shindo
Serious Injuries Minor Injuries
Toyama 1 0 5-
Himi 0 1
Oyabe 0 1
Imizu 0 2
Takaoka 0 6 4
Uozu 0 2
Total 1 12 Max 5-

Effects

Evacuations

At least 1000 people in Wajima were evacuated to temporary shelters.[1]

Transportation

The train lines that were stopped after the earthquake were:

Noto Airport temporarily closed due to the fact that 22 cracks were found in the runway.

A part of the Noto Toll Road temporarily closed since many parts of it collapsed. It re-opened on April 27.

Tsunami

A tsunami advisory was immediately made for the Kaga coast and Noto coast, and a 22 cm wave[10] hit shore about 30 minutes later.[11]

Aftershocks

More than 500 perceptible aftershocks were observed.

Aftershocks with Shindo 4 or more[12][13]
Date
(YYYY-MM-DD)
Time
(UTC)
Magnitude Shindo
2007-03-25 09:45:50 4.7 (Mj) 4
2007-03-25 09:52:37 4.5 (Mj) 4
2007-03-25 15:43:34 4.5 (Mj) 4
2007-03-25 18:11:45 5.3 (Mj) 5-
2007-03-26 07:16:36 5.3 (Mj) 4
2007-03-26 14:46:35 4.8 (Mj) 5-
2007-03-26 18:02:53 4.6 (Mj) 4
2007-03-28 08:08:15 4.9 (Mj) 5-
2007-03-28 13:05:31 4.7 (Mj) 4
2007-04-06 15:18:18 4.3 (Mj) 4
2007-05-02 20:44:38 4.7 (Mj) 4
2007-06-11 03:45:14 5.0 (Mj) 4
2008-01-26 04:33:00 4.8 (Mj) 5-

Largest aftershocks are blue, and 4.8~ Mj earthquakes are light blue.

Response

The Cabinet Office

At 9:45, an emergency meeting for this earthquake was held at the Prime Minister's Official Residence. Government damage inspecting teams under command of Kensei Mizote were sent to the epicenter area from the 25th to the 26th.

Ishikawa Prefecture

At 10:45, an emergency disaster prevention meeting was held. 375 firefighters were summoned from Toyama Prefecture, Fukui Prefecture, Tokyo prefecture, Kyoto Prefecture, Osaka Prefecture, Shiga prefecture, and Hyogo Prefecture.[9] They were ordered to leave on 10:42 on the 26th, and left on 11:55.

Japan Self-Defense Forces

At 10:45, the Ministry of Defense held an emergency meeting. At 11:08, Masanori Tanimoto, the governor of Ishikawa Prefecture summoned 30 soldiers from the Ground forces from bases in Kanazawa, Sabae, Toyama, Kasugai, Nagoya, Hisai, and Takashima.[9] Helicopters from bases in Wajima and Komatsu were also used. Ground forces, maritime forces, and air forces all went to investigate damage.

Other

See also

References

  1. ^ a b c "Earthquakes rock Pacific nations". BBC News. 2007-03-25.
  2. ^ "Archived copy". Archived from the original on 2009-12-18. Retrieved 2012-12-16.CS1 maint: archived copy as title (link)
  3. ^ [1]
  4. ^ a b "Archived copy". Archived from the original on 2012-12-14. Retrieved 2013-01-05.CS1 maint: archived copy as title (link)
  5. ^ a b http://www.seisvol.kishou.go.jp/cgi-tmp/shindo_db/27680.html[permanent dead link]
  6. ^ a b c "石川県能登半島沖を震源とする地震に伴う地殻変動(第1報)|国土地理院". Gsi.go.jp. Retrieved 2017-06-08.
  7. ^ a b "産総研:能登半島地震の震源域で長さ18km以上の活断層と一部で海底に達する変動を確認". Aist.go.jp. 2007-07-30. Retrieved 2017-06-08.
  8. ^ Yamada, Masumi; Park, Sun-Cheon; Mori, Jim (2008). "The 2007 Noto Peninsula, Japan, Earthquake (Mw 6.7): Damage to Wooden Structures" (PDF). Seismological Research Letters. Seismological Society of America. 79 (1): 20–24. doi:10.1785/gssrl.79.1.20.
  9. ^ a b c "6.9 Magnitude Earthquake Kills 1, Injures 170 in Japan". Fox News. 2007-03-25.
  10. ^ "Archived copy". Archived from the original on 2013-01-20. Retrieved 2012-12-16.CS1 maint: archived copy as title (link)
  11. ^ "Hokuriku quake kills one, injures 170". The Japan Times. 2007-03-26. Retrieved 26 March 2007.
  12. ^ http://www.seisvol.kishou.go.jp/cgi-tmp/shindo_db/15560.html[permanent dead link]
  13. ^ http://www.seisvol.kishou.go.jp/cgi-tmp/shindo_db/16178.html[permanent dead link]

Notes

  1. ^ The seismometer that recorded the shaking in Anamizu reported shaking a little larger than it actually was, so the Shindo might have been 6-.

Sources

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2007 Noto earthquake
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