Very strong dangerous earthquake along the coast of Honshu (Aomori), Japan – minor damage reported

Last update: May 24, 2012 at 9:38 pm by By

Earthquake overview : A few minutes after midnight, a very strong earthquake hit the channel zone in between Hokkaido and Honshu, Japan. Epicenter in the Ocean approx. 50 km from the coast.
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Update 24/05 – 08:08 UTCAfter carefully examining the many sources we use to create this report, we are happy to inform that no additional damage has been found.


A video shop in Hachinoche after the earthquake - image courtesy toonippo.co.jp

Update 18:05 UTCNuclear facilities
- Tohoku Electric Power has reported that there were NO power outages.
- The Mutsu nuclear installations and the Ogawara Nuclear plant are reported to be operating normally.
- The shaking must have been serious as the picture of a video shop proves on the right
- trains have been halted for a while during and after the quake
- Aomori authorities have inspected various strategic buildings like airports, runways, etc and found no structural damage.

Update 18:05 UTCMinor damage
4 schools in Noheji have broken windows. Other damage has been reported in the museum of Noheji (damage to the ceiling).  Noheji is a city with 14,721 inhabitants.
We will keep you updated if new reports are published.

Update 16:57 UTC : FDMA Japan has issued a new report on 16:40 UTC – good news, still no sign of any damage.  ER expects that the highest intensity area will probably remain damage free.

Update 16:44 UTC : FDMA Japan (Fire brigade who also works as SAR and Emergency forces during earthquake are currently making an assessment of the situation. The heaviest shaking is in the Aomori prefecture. Until now no damage reported as yet. The report has been issued 1 hour ago.

Noheji town - composite image courtesy Kaznis

Purple line is subduction fault line - seismic hazard map courtesy USGS

Update 16:30 UTC : We have noticed and reported a very curious swarm of earthquakes more to the south.  A lot of these earthquakes had the same Magnitude than this one but due to the distance from the coast (150 to 200 km) we have only described the phenomenon in our daily lists.  This earthquake as well as all the other earlier ones and the great March 11 destructive one in 2011 are triggered by the same fault. The purple line at right is the subduction fault line where the pacific plate subducts the Eurasian plate. The depth today is a very good illustration of this subducting process. The pacific heavier plate glides below the Eurasian plate and hangs frequently.  When the pressure mounts, it suddenly breaks and generates an earthquake.  The friction points are mostly seen in a rather wide area (a few hundred km’s) along the subduction faults.

Update 16:20 UTC : The earthquake occurred just after midnight and a lot of people must have been already sleeping. Hard to get up this way.

Update 16:20 UTC : There are NO tsunami advisories in effect. In general earthquakes below M7 generate rarely stronger waves.

Update 16:17 UTC :  USGS I Have Felt It data are confirming the testimony report below. MMI V in Misawa.  The highest intensity values will have been felt along Cape Shinyazaki.

Update 16:13 UTC : The data below is a little confusing for some people as USGS indicates “only” a max. MMI V (moderate shaking) and JMA a 5+ (equivalent of MMI VII). JMA Japan is a highly specialized seismological agency and we always tend to believe the local agencies. The testimony below shows that JMA Japan is right. We do not expect a lot more Experience reports as there are very few English understanding people living in these areas. Our Experience reports in Japan are mostly coming from Expats working in the country.

Intensity map, courtesy JMA Japan (dark orange = strongest shaking)

Update 16:01 UTC : Other intensity values :
JMA5- : Noheji-machi Tabasamizawa*, Noheji-machi Noheji*, Higashidori-mura Odanosawa*
JMA 4 : Aomori-shi Hanazono, Goshogawara-shi Sakaemachi, Goshogawara-shi Shikishimacho*, Hiranai-machi Kominato, Hiranai-machi Higashi-tazawa*, Itayanagi-machi Itayanagi*, Sotogahama-machi Kanita*, Hachinohe-shi Minatomachi, Hachinohe-shi Uchimaru*, Hachinohe-shi Nangoku*, Towada-shi Nishi-nibancho*, Towada-shi Nishi-junibancho*, Misawa-shi Sakuracho*, Shichinohe-machi Shichinohe*, Shichinohe-machi Morinokami*, Rokunohe-machi Inuotose*, Tohoku-machi Tonosawayama*, Rokkasho-mura Obuchi, Gonohe-machi Furudate, Gonohe-machi Kuraishi-nakaichi*, Aomori Nambu-cho Taira*, Aomori Nambu-cho Tomabechi*, Hashikami-cho Dobutsu*, Oirase-cho Nakashimoda*, Oirase-cho Kamiakedo*, Mutsu-shi Kanamagari, Mutsu-shi Kanaya*, Mutsu-shi Ohatamachi-nakajima*, Mutsu-shi, awauchimachi*, Higashidori-mura Sunagomata*

Update 15:56 UTC : An ER reader living in Misawa, approx. 75 km from the epicenter wrote a few moments ago :

Woke me up, I think midnight.  I was so scared that I jumped up too quickly and ended up with a cramp in my leg.  It was long too and was getting stronger so husband and I stood under doorway of lodging until subsided a little then went outside. She described the shaking as a strong shaking. Misawa is labeled as a JMA 4 intensity. Some people must have felt it a lot stronger (see above)

Update 15:52 UTC : Based on JMA data (Japan Seismological Service), the max. shaking will be 5+ at Tohoku-machi Kamikita-minami*. 5+ is considered by Earthquake-Report.com as “moderately dangerous”. JMA uses a 0 to 7 scale.

Based on theoretical data from USGS, the max. shaking will be moderate and felt by 76,000 people.

Most important Earthquake Data:
Magnitude :  M6.0 (JMA Japan)
UTC Time : Wednesday, May 23, 2012 at 15:02:25 UTC
Local time at epicenter : Thursday, May 24, 2012 at 12:02:25 AM at epicenter
Depth (Hypocenter) : 50 km (JMA Japan)
Geo-location(s) :
Approx. 60 km from Mutsu, Honshu, Japan
107 km (66 miles) NNE of Hachinohe, Honshu, Japan
119 km (73 miles) ESE of Hakodate, Hokkaido, Japan
127 km (78 miles) ENE of Aomori, Honshu, Japan

Links to important maps
USGS Did You Feel It Map
Google satellite map showing the epicenter and the surrounding area
Historic earthquakes map
Seismic hazard map
Shaking map
Scientific parameters
Human impact map

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SRC Location UTC Date/time M D INFORMATION
USGS Near The East Coast Of Honshu, Japan May 23 23:15 PM 4.4 10 MAP I Felt It
EMSC Hokkaido, Japan Region May 23 15:02 PM 6.0 60 MAP I Felt It
USGS Hokkaido, Japan Region May 23 15:02 PM 6.0 71 MAP I Felt It
GEOFON Hokkaido, Japan Region May 23 15:02 PM 5.9 61 MAP I Felt It
  • Shinjuku - I was in my hotel, 6th floor. I woke up as my bed was shaking and I heard the sound of ground shaking, too. It was my first time to experience an earthquake (that was my first morning in Japan). I wasn't scared, though.
  • Misawa, Japan - Woke me up, I think midnight. I was so scared that I jumped up too quickly and ended up with a cramp in my leg. It was long too and was getting stronger so husband and I stood under doorway of lodging until subsided a little then went outside.
  • Misawa Japan - Moderate shaking reported
  • Ohma, Aomori-ken - Strong shaking reported
  • JMA Hokkaido - Honshu, Japan May 23 15:02 PM 6.0 50 MAP I Felt It
    EMSC Izu Islands, Japan Region May 23 13:55 PM 4.4 369 MAP I Felt It
    GEOFON Southeast Of Honshu, Japan May 23 13:55 PM 4.6 346 MAP I Felt It
    USGS Izu Islands, Japan Region May 23 13:55 PM 4.4 348 MAP I Felt It

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    SHARE YOUR EARTHQUAKE EXPERIENCE WITH US

    Enter Email (not compulsory)
    City/Village where you felt the earthquake
    MMI II (Very weak shaking) ?
    People :
    Felt by persons at rest, on upper floors or favorably placed.
    MMI III (Weak shaking) ?
    People :
    Felt indoors; hanging objects may swing, vibration similar to passing of light trucks, duration may be estimated, may not be recognized as an earthquake.
    MMI IV (Light shaking) ?
    People :
    Generally noticed indoors but not outside. Light sleepers may be awakened. Vibration may be likened to the passing of heavy traffic, or to the jolt of a heavy object falling or striking the building.
    Fittings :
    Doors and windows rattle. Glassware and crockery rattle. Liquids in open vessels may be slightly disturbed. Standing motorcars may rock.
    Structures :
    Walls and frames of buildings, and partitions and suspended ceilings in commercial buildings, may be heard to creak.
    MMI V (Moderate shaking) ?
    People :
    Generally felt outside, and by almost everyone indoors. Most sleepers awakened. A few people alarmed.
    Fittings :
    Small unstable objects are displaced or upset. Some glassware and crockery may be broken. Hanging pictures knock against the wall. Open doors may swing. Cupboard doors secured by magnetic catches may open. Pendulum clocks stop, start, or change rate.
    Structures :
    Some large display windows cracked. A few earthenware toilet fixtures cracked.
    MMI VI (Strong shaking) ?
    People Felt by all. People and animals alarmed. Many run outside. Difficulty experienced in walking steadily.
    Fittings :
    Objects fall from shelves. Pictures fall from walls. Some furniture moved on smooth floors, some unsecured free-standing fireplaces moved. Glassware and crockery broken. Very unstable furniture overturned. Small church and school bells ring. Appliances move on bench or table tops. Filing cabinets or "easy glide" drawers may open (or shut).
    Structures :
    Slight damage to buildings with low standard. Some stucco or cement plaster falls. Large display windows broken. Damage to a few weak domestic chimneys, some may fall.
    Environment :
    Trees and bushes shake, or are heard to rustle. Loose material may be dislodged from sloping ground, e.g. existing slides, talus slopes, shingle slides.
    MMI VII (Very strong shaking) ?
    People
    General alarm. Difficulty experienced in standing. Noticed by motorcar drivers who may stop.
    Fittings :
    Large bells ring. Furniture moves on smooth floors, may move on carpeted floors. Substantial damage to fragile contents of buildings.
    Structures :
    Unreinforced stone and brick walls cracked. Low standard buildings cracked with some minor masonry falls. A few instances of damage to buildings of ordinary workmanship. Unbraced parapets, unbraced brick gables, and architectural ornaments fall. Roofing tiles, especially ridge tiles may be dislodged. Many unreinforced domestic chimneys damaged, often falling from roof-line. Water tanks Type I burst. A few instances of damage to brick veneers and plaster or cement-based linings. Unrestrained water cylinders (hot-water cylinders) may move and leak. Some common windows cracked. Suspended ceilings damaged.
    Environment :
    Water made turbid by stirred up mud. Small slides such as falls of sand and gravel banks, and small rock-falls from steep slopes and cuttings. Instances of settlement of unconsolidated or wet, or weak soils. Some fine cracks appear in sloping ground. A few instances of liquefaction (i.e. small water and sand ejections).
    MMI VIII (Severe shaking) ?
    People Alarm may approach panic. Steering of motorcars greatly affected. Structures : Low standard buildings heavily damaged, some collapse. ordinary workmanship buildings damaged, some with partial collapse. Reinforced masonry or concrete buildings damaged in some cases. A few instances of damage to buildings and bridges designed and built to resist earthquakes. Monuments and pre-1976 elevated tanks and factory stacks twisted or brought down. Some pre-1965 infill masonry panels damaged. A few post-1980 brick veneers damaged. Decayed timber piles of houses damaged. Houses not secured to foundations may move. Most unreinforced domestic chimneys damaged, some below roof-line, many brought down. Environment : Cracks appear on steep slopes and in wet ground. Small to moderate slides in roadside cuttings and unsupported excavations. Small water and sand ejections and localized lateral spreading adjacent to streams, canals, lakes, etc.
    MMI IX (Violent shaking) ?
    Structures Many low standard buildings destroyed. Ordinary workmanship buildings heavily damaged, some collapse. Reinforced masonry or concrete buildings damaged, some with partial collapse. Buildings and bridges designed and built to resist earthquakes damaged in some cases, some with flexible frames seriously damaged. Damage or permanent distortion to some buildings and bridges, designed and built to normal use standards. Houses not secured to foundations shifted off. Brick veneers fall and expose frames. Environment : Cracking of ground conspicuous. Landsliding general on steep slopes. Liquefaction effects intensified and more widespread, with large lateral spreading and flow sliding adjacent to streams, canals, lakes, etc.
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