Earthquake — off Coast of Japan

February 29, 2012 – strong coastal earthquake close to Tokyo

Last update: February 29, 2012 at 2:57 pm by By 

 

Earthquake intensity image courtesy JMA Japan

M 5.8      2012/02/29 14:32    Depth 20.0 km     JAPAN
local time 23:32 – Epicenter location see below in list
70 km SE Choshi (pop 75,650) and 108 km SE Narita (pop 100,641) (Narita is one of the Tokyo airports)
Earlier report we wrote when we found out the earthquake occurred
Preliminary data are talking about a strong earthquake 20 km out in the sea near Tokyo
We are estimating that the epicenter is about 50 km out in the sea. Certainly NOT strong enough to generate a tsunami.
JMA Japan reports a magnitude of 5.8 at a depth of 20 km. Max. registered intensity by JMA : 4 at Isumi-shi Misakicho-choja* – Earthquake-Report.com considers 5+ as dangerous for eventual damage
Conclusion Earthquake-Report.com : NOT dangerous for damage or injuries

from:    http://earthquake-report.com/2012/02/28/earthquakes-list-february-29-2012/

Earthquake near Honshu, Japan

Strong shallow earthquake near Sado Island, Honshu, Japan

Last update: February 8, 2012 at 2:15 pm by By 

Earthquake overview : At 21:01 (09:01 PM) a strpng shallow earthquake occurred close to the coast of Sado Island, Honshu, Japan

Coastal village on Sado Island close to the epicenter – courtesy KatyGoat

Update 14:03 UTC
Fire Department of Japan has reported in his third report that as far as 2 hours after the earthquake,  no damage has been detected in the villages or cities and that the Kashiwazaki-Kariwa Nuclear Power Station has not been damaged neither.

Update 13:44 UTC
The strongest earthquake we could trace at Sado Island was a M 6.6 earthquake which occurred at December 9, 1802.

Update 13:34 UTC
Japan seismological agency, JMA is reporting a 5+ intensity, considered by Earthquake-report.com as moderately dangerous for damage.
5+    Sado-shi Aikawa-sanchome and Sado-shi Kawaharada-hommachi*
5-    Sado-shi Ogimachi*, Sado-shi Hamochi-hongo* and Sado-shi Akadomari*
   Sado-shi Iwayaguchi*, Sado-shi Ryotsu-minato*, Sado-shi Matsugasaki*, Sado-shi Chigusa*, Sado-shi Niibo-uryuya*, Sado-shi Mano-shimmachi*, Sado-shi Ryotsu-shisho* and Sado-shi Aikawa-sakaemachi*
Japan seismological intensity values are scaled from 0 to 7. 5+ JMA can be compared with 7 MMI (very strong shaking).

Sado Island earthquake – Intensity map courtesy JMA Japan

Update 13:32 UTC
Sado Province was a province of Japan until 1871; since then, it has been a part of Niigata Prefecture. It was sometimes called Sashū or Toshū. It lies on the eponymous Sado Island, off the coast of Niigata Prefecture (or in the past, Echigo Province).
Sado was famous for the silver and gold mined on the island. In the Kamakura Period, the province was granted to the Honma clan from Honshū, and they continued to dominate Sado until 1589, when Uesugi Kagekatsu of Echigo Province took over the island. The Tokugawa shoguns later made Sado a personal fief after Sekigahara, and assumed direct control of its mines.
Since 2004 Sado city has comprised the entire island.
Its rich history and relaxed rural atmosphere make Sado one of the major tourist destinations in Niigata Prefecture. The island has several temples and historical ruins, and offers possibilities for various outdoor activities, as well as fresh local food.
Sado is famous as the major breeding area for the Japanese Crested Ibis. The last known Japan-born Japanese Crested Ibis died in captivity in 2003 on the island. Currently, birds from China are being bred in a captive program in a facility in Niibo area. The Ibis, Toki in Japanese, is a major symbol of the Island and can be found on several tourist items. There are plans to release Ibis in the wild at the end of 2008. (source Wikipedia)

Update 13:31 UTC
The Island area does not seem to be particularly dangerous, although moderate earthquakes are fairly common.

The strong shallow and thus moderately dangerous earthquake occurred almost below Sado Island, an island approx. 50 km from the western Honshu coast.


Most important Earthquake Data:

Magnitude : 5.7
UTC Time : Wednesday, February 08, 2012 at 12:01:37 UTC
Local time at epicenter :  Wednesday, February 08, 2012 at 09:01:37 PM at epicenter
Depth (Hypocenter) : 10 km
Geo-location(s) :
10 km from Sawazakihana Light (Sado Island)
38 km SW Ryotsu (pop 16,359)
72 km NW Nagaoka (pop 195,318)

for more information and updates, go to:    http://earthquake-report.com/2012/02/08/strong-shallow-earthquake-near-sado-island-honshu-japan/

Analysis of Tokyo’s Earthquake Risk

Tokyo sees high quake probability, scientists warn

By Elizabeth Yuan, CNN
updated 7:17 AM EST, Tue January 24, 2012
Japan's highest mountain, Mount Fuji, rises behind Tokyo's skyscraper skyline, as the sun sets in this photo last year.
Japan’s highest mountain, Mount Fuji, rises behind Tokyo’s skyscraper skyline, as the sun sets in this photo last year.

STORY HIGHLIGHTS
  • Forty-two million people live in Tokyo metropolitan area
  • University researchers cited findings on increase in small tremors
  • Government put 70% probability of magnitude-7 quake in region within 30 years
  • March 11 quake and tsunami left more than 15,700 dead, government says

(CNN) — Tokyo faces the possibility of being hit by a massive earthquake within the next four years, according to Japanese researchers.

The University of Tokyo’s Earthquake Research Institute predicts there is a 70% probability that the capital’s metropolitan area will experience a magnitude-7 quake within four years and a 98% probability within the next 30 years.

Nearly one year ago, a magnitude 9.0 quake struck off Japan’s central Pacific coast, triggering a devastating tsunami and aftershocks that left more than 15,700 dead, according to a government report in December on Japan’s recovery from the catastrophe. About 4,500 were listed as missing.

Nearly 700 aftershocks registering magnitude 5 or greater followed last year’s quake, the government report said.

The March 11 earthquake — dubbed “Tohoku” after the region in which it occurred — also damaged the Fukushima Dai-ichi nuclear power station, where three reactors experienced full meltdowns, creating a nuclear crisis for a country already grappling with disaster.

Quake, tsunami debris threaten coastlines

The research institute cited for its findings the Gutenberg Richter Law, which states that an increase in small tremors will likely increase the number of larger earthquakes. According to another paper published in September, the institute concluded that the quake ruptured a fault area nearly 500 kilometers in length and 200 kilometers wide offshore.

The fourth strongest quake recorded in history, Tohoku caused abrupt stress changes in the upper plate and triggered widespread seismic activity throughout the Japanese island. The northern part of Ibaraki Prefecture, in particular, saw a significant increase of shallow seismicity after the quake compared with the extremely low rate eight years prior, the researchers said.

Should Tokyo’s inhabitants be worried?

The research institute’s findings carry great consequences for the 42 million people who live in the Tokyo metropolitan area. The Central Disaster Management Council has estimated that a large-scale earthquake in the next few decades could result in 11,000 deaths and an economic loss of 112 trillion yen (US$1 trillion). Its goal is to halve the estimated death toll and reduce the estimated economic loss.

How precise are seismic forecasts?

Gary Gibson, a seismologist at Australia’s Seismology Research Centre Seismology Research Centre, called the Earthquake Research Institute’s findings “not at all unexpected,” given the level of seismic activity and their model.

“Seismologists cannot predict with certainty when, where and how large the next big earthquake will be,” he wrote in an e-mail to CNN. “However, it is possible to forecast the probability of an earthquake in a particular time range (e.g. the next four years), location area (e.g. the Tokyo region), and magnitude range (e.g. greater than magnitude 7.0).

“Long-term forecasts use average activity levels from past earthquakes, geological data from fault displacements, and data about plate movement and deformation from very precise GPS measurements and other methods to determine these probabilities.”

What is the government saying?

The government’s Headquarters for Earthquake Research Promotion had put a 70% probability of a magnitude-7 quake in Kanto region, which encompasses Tokyo and Yokohama, within 30 years, based on long-term seismicity and hazard studies.

Scientists have already dubbed as “Tokai” an expected 8.0 quake near Suruga Bay, where large quakes have historically struck every 100-150 years, according to the Japan Meteorological Agency. The last one, a magnitude-8.4 quake, occurred in 1854 — nearly 160 years ago.

According to Gibson, the seismologist, the enhanced seismicity in the area affected by the Tohoku quake may fall towards normal levels and could affect the research institute’s findings. Results for the six-month period after the quake would become available after this coming March 11, the quake’s anniversary, he noted.

Why is Japan so prone to earthquakes?

The Japanese archipelago and neighboring areas rest on or around four tectonic plates — the Pacific, Philippine Sea, North American and Eurasian plates — whose movements account for one of the most seismically active places on earth.

Can Tokyo withstand a 7.0 quake?

Gibson said that while the area is a very active one seismically, building standards are high, therefore reducing the damage caused by earthquakes. Buildings in Tokyo held up well in the face of the “Tohoku” quake. Reinforced concrete and anti-seismic systems in buildings are among features that have helped absorb shocks when earthquakes occur.

Watch Tokyo’s quake-proof communities

“A magnitude 7.0 earthquake is very much smaller than the magnitude 9.0 Tohoku earthquake,” he wrote. “It would need 1,000 magnitude-7.0 earthquakes to release as much strain energy as the magnitude 9.0. The fault rupture size is tens of kilometers, rather than hundreds of kilometers, and the fault displacement two to three meters rather than 20 to 30 meters.”

Serious damage could be limited, if it occurs offshore, he added. And the shallower the quake, such as within 10 kilometers of the surface, the more localized the damage.

CNN’s Junko Ogura contributed to this report.

this story comes from:    http://www.cnn.com/2012/01/24/world/asia/tokyo-quake-forecast/index.html?hpt=hp_t3

Massive earthquake Shakes Japan

Massive deep earthquake sends a vibration all over Japan

Last update: January 1, 2012 at 1:45 pm by By

Earthquake overview : A massive earthquake occurred in the hot solid mantle of the earth.  Due to the focal depth of 370 km this earthquake has been felt all over Japan. The earthquake was however harmless due to the weakened impact.

Intensity map courtesy JMA Japan

Update : The hypocenter of this earthquake was far too deep to generate a tsunami.

Update :  Values of other seismological agencies
EMSC : 7.0 at 365 km
GEOFON : 6.7 at 361 km
CEN : 7.0 at 360 km

The earthquake must have been felt by millions of people.

A little bit to our surprise the shaking was strongest in the greater Tokyo area (see yellow bullets on the JMA map) , although other areas in Japan felt it as a weak shaking and were located closer to the epicenter. Part of the reason will certainly be the propagation of the wave.

The earthquake was calculated to be felt as a weak shaking based on the USGS Data, however the Japanese seismological agency JMA reported a V MMI (moderate shaking). These values are approx.  4 JMA (Japanese use another seismic intensity scale)

Very strong but very deep earthquake with an hypocenter (focal depth) in the hot solid mantle of the earth. Based on calculations of the seismological centers, only a weak shaking will have been felt in a very wide area. The epicenter was located in between a lot of submarine volcanoes .

Most important Earthquake Data:
Magnitude : 7.0 (JMA) 6.8 (USGS)
UTC Time : Sunday, January 01, 2012 at 05:27:54 UTC
Local time at epicenter :  Sunday, January 01, 2012 at 02:27:54 PM at epicenter
Depth (Hypocenter) : 370 km (JMA) 349 km (USGS)
Geo-location(s) :
242 km (150 miles) SW of Hachijo-jima, Izu Islands, Japan
365 km (226 miles) S of Hamamatsu, Honshu, Japan
393 km (244 miles) S of Shizuoka, Honshu, Japan
495 km (307 miles) SSW of TOKYO, Japan

for more information and updates go to:    http://earthquake-report.com/2012/01/01/massive-deep-earthquake-sends-a-vibration-all-over-japan/

 

SakuraJima Volcano Erupts

Explosive eruptions and information on SakuraJima volcano, Japan + video’s

Last update: October 3, 2011 at 3:52 pm by By 

The webcam videos below are from October 1 and October 3, 2011. They show a couple of explosive eruptions.
Sakurajima’s activity became prominent in 1955, and the volcano has been erupting almost constantly ever sinceThousands of small explosions occur each year, throwing ash to heights of up to a few kilometers above the mountain.
The Sakurajima Volcano Observatory was set up in 1960 to monitor these eruptions.

(to see the current videos, go to:    http://earthquake-report.com/2011/10/03/explosive-eruptions-and-information-on-sakurajima-volcano-japan-videos/)

1914 eruption of Sakurajima

 

Image courtesy TANAKA Juuyoh – CC-By-3.0

The 1914 eruption was the most powerful in twentieth-century JapanLava flows filled the narrow strait between the island and the mainland, turning it into a peninsula. The volcano had been dormant for over a century until1914.The 1914 eruption began on January 11.Almost all residents had left the island in the previous days, in response to several large earthquakes that warned them that an eruption was imminent. Initially, the eruption was very explosive, generating eruption columns and pyroclastic flows, but after a very large earthquake on January 13, 1914 which killed 35 people, it became effusive, generating a large lava flow.  Lava flows are rare in Japan—the high silica content of the magmas there mean that explosive eruptions are far more common but the lava flows at Sakurajima continued for months.

 

Pre-eruption earthquakes killed at least 35 people; caused an evacuation and significant changes to the local topology.

The island grew, engulfing several smaller islands nearby, and eventually becoming connected to the mainland by a narrow isthmus. Parts of Kagoshima bay became significantly shallower, and tides were affected, becoming higher as a result.

During the final stages of the eruption, the centre of the Aira Caldera sank by about 60 centimetres (24 in), due to subsidence caused by the emptying out of the underlying magma chamber. The fact that the subsidence occurred at the centre of the caldera rather than directly underneath Sakurajima showed that the volcano draws its magma from the same reservoir that fed the ancient caldera-forming eruption. The eruption partly inspired a 1914 movie, Wrath of the Gods, centering around a family curse that ostensibly causes the eruption.

to read more on this, see the videos, etc., go to:    http://earthquake-report.com/2011/10/03/explosive-eruptions-and-information-on-sakurajima-volcano-japan-videos/

Typhoon & Tropical Storm Update fr/Dr. Masters

Typhoon Roke batters Japan; Ophelia forms in the Central Atlantic
Posted by: JeffMasters, 1:28 PM GMT on September 21, 2011 +9
Typhoon Roke hit Japan near Hamamatsu at 14:00 JST Wednesday as a Category 1 typhoon with 80 mph winds. Roke brought sustained winds of 62 mph, gusting to 83 mph to the Tokyo airport at 5:25 pm local time, and a wind gust of 89 mph was reported at Shizuhama Airbase. Roke has dumped heavy rains of 155 mm (6.20″) at Hamamatsu and 125 mm (4.86″) at Tokyo. Damage due to flooding from Roke’s heavy rains will likely be the main problem from Roke, as the soils over much of Japan are saturated from the passage of Tropical Storm Talas during the first week of September. Talas was a very slow moving storm, and brought extreme rainfall amounts of over six feet to some portions of Japan. Roke brought winds less than 25 mph to the damaged Fukishima-Dai-Iche nuclear plant northeast of Tokyo, and heavy rains of 189 mm (7.50″) toHirono, located 8 miles south of the plant.


Figure 1. Radar image of Typhoon Roke as it made landfall at 14:00 JST on September 21, 2011. The typhoon brought a large area of rainfall of 50 mm/hr (2″/hr) to Japan. Image credit: Japan Meteorological Agency.


Figure 2. MODIS image of Typhoon Roke taken at 3:55 UTC on Wednesday, September 21, 2011. At the time, Roke was a Category 1 storm with 80 mph winds. Image credit: NASA.

Tropical Storm Ophelia forms in the Atlantic
Tropical Storm Ophelia formed last night in the Central Atlantic from the tropical wave (Invest 98L) we’ve been tracking this week. Satellite imagery shows that Ophelia is suffering the classic symptoms of high wind shear, with the low level center of circulation exposed to view, and the storm’s heavy thunderstorms pushed to the northeast side of the center of circulation. An analysis of wind shear from the University of Wisconsin CIMMS group shows a high 20 – 30 knots of wind shear due to strong upper level west-southwesterly winds affecting Ophelia. We don’t have any ship, buoy, or hurricane hunter observations of Ophelia’s winds, but an ASCAT pass from 7:27 pm EDT last night found top winds of 45 mph in the northeast quadrant of the storm. Ophelia will be passing south of buoy 41041 late tonight. Water vapor satellite imagesshow dry air to the the west of Ophelia, and the strong upper level west-southwesterly winds bringing high wind shear to the storm are also injecting dry air into the storm’s core, interfering with development.


Figure 3. Morning satellite image of Ophelia showing the low-level center exposed to view, with all the storm’s heavy thunderstorms pushed to the northeast side.

Forecast for Ophelia
The latest SHIPS model forecast predicts that Ophelia will experience moderate to high wind shear of 10 – 25 knots over the next five days, and will move into a region with drier air. The combination of shear and dry air should keep Ophelia from strengthening, and could dissipate the storm, as predicted by the ECMWF and HWRF models. The Northern Lesser Antilles could see some wind gusts of 30 – 40 mph and heavy rain squalls from Ophelia on Saturday and Sunday, but right now it looks unlikely that the islands would see sustained tropical storm force winds of 39+ mph, since they are likely to be on Ophelia’s weaker (dry) side. At longer ranges, Bermuda will have to keep an eye on Ophelia, since a large cut-off low pressure system over the Eastern U.S. should turn Ophelia to the northwest and then north early next week. Ophelia may eventually be a threat to Canada, but it is too early to assess the odds of this happening.

Ophelia is the 15th named storm this year, putting 2011 in 10th place for the most number of named storms in a year. Ophelia’s formation date of September 21 puts 2011 in 4th place for earliest date of arrival of the season’s 15th storm. Only20051936, and 1933 had an earlier 15th storm. With only three of this year’s fifteen storms reaching hurricane strength, though, this year has been near average for destructive potential. Atlantic hurricane records go back to 1851.

Jeff Masters

U of Tokyo Professor Speaks Out on Fukushima

Professor’s anger at lawmakers creates buzz on Internet

SHUKAN ASAHI WEEKLY MAGAZINE

photoTatsuhiko Kodama, right, a University of Tokyo professor, shows residents in Minami-Soma, Fukushima Prefecture, how to reduce radiation contamination in the soil. (Takeshi Kawasaki)

An exasperated University of Tokyo professor who launched an angry tirade at lawmakers over the Fukushima nuclear crisis has become a hero to many on the Internet.

Tatsuhiko Kodama, 58, who heads the Radioisotope Center at Todai, was called to provide expert testimony before the Lower House Health, Labor and Welfare Committee on July 27.

Facing a panel of lawmakers, Kodama said, “At a time when 70,000 people have left their homes and have no idea where to go, what is the Diet doing?”

Video footage of Kodama’s testimony was soon posted on YouTube, and within a few days, the video had been viewed more than 200,000 times.

Responses to the footage were generally favorable.

“I was deeply moved that Todai has a professor like him,” said one post.

“I understand the scary truth. I understand the inaction of the central government,” said another.

Besides being a doctor of internal medicine, Kodama is also an expert on internal radiation exposure. His background made even more shocking the testimony he provided in the Diet.

to read more, go to:     http://www.asahi.com/english/TKY201108120245.html

Antarctic Icebergs Effected by Japanese Tsunami

Japan Tsunami has been cutting off parts of Antarctic Icebergs

Last update: August 9, 2011 at 10:47 pm by By Armand Vervaeck

Using satellite radar data, scientists recently observed the calving of several large icebergs from the Sulzberger Ice Shelf along the Antarctic coast as a result of the March 2011 tsunami half a world away in Japan.
Scientists have long speculated that ocean waves could cause an ice shelf to flex and break, but this is the first time researchers have observed a tsunami having this effect.

The images above were acquired by the Advanced Synthetic Aperture Radar (ASAR) on the European Space Agency’s Envisat satellite on March 11 and 16, 2011. The top image was taken just before the arrival of the tsunami at the front of the Sulzberger Ice Shelf, while the bottom image shows the chunks of ice well out to sea just five days later.
This time-lapse series of images shows the progression of the ice breakup. In each radar image—which allows researchers to see through cloud cover—land ice, ice shelves, and the new bergs are brighter white, while grayer areas have smaller bits of sea ice. Open water is black.

to see the photographs and read more, go to:    http://earthquake-report.com/2011/08/09/japan-tsunami-has-been-cutting-off-parts-of-antarctic-icebergs/

 

 

 

 

 

Earthquake – Iwaki Japan

Very strong aftershock near Iwaki (Japan) – at least 7 people injured

Last update: July 30, 2011 at 11:27 pm by By Armand Vervaeck and James Daniell

Earthquake Overview : A very strong coastal earthquake at an intermediate depth and with an epicenter only 18 km from Iwaki occurred in the night of July 31 2011.  NO tsunami advisories or warnings have been published for this earthquake. Today’s earthquake is a very strong aftershock of the March 11 earthquake

Shaking map (yellow = MMI VI) – courtesy USGS

UPDATE 23:21 UTC : Official reports are indicating that at least 7 people were injured during this earthquake (1 person in Sendai, 2 in Koriyama, 2 in Mito, 1 in Hitachi Omiyma and 1 in Chikusei. No reports on damage yet.

UPDATE 21:48 UTC : As reported earlier in this article, Earthquake-Report.com fears the combination of the TORRENTIAL RAINS, overflowed rivers ( in Niigata and Fukushima prefectures) and the shaking of this aftershock.

to read more, go to:  http://earthquake-report.com/2011/07/30/very-strong-moderately-dangerous-aftershock-near-iwaki-japan/

Japan Strong Aftershock

Very strong coastal earthquake / aftershock near Ofunato, Japan

Last update: July 25, 2011 at 5:58 am by By Armand Vervaeck and James Daniell

Earthquake overview : At 1.34 PM (13:34), a very strong aftershock has shaken the Ofunato coastal area. Theearthquake had a magnitude of 6.4 following USGS.  The Ofunato coast was severely damaged during the March 11 earthquake and tsunami.

Intensity map courtesy JMA Japan – Orange: 5+ Yellow: 5-

FINAL UPDATE 25/07 05:49 UTC :
There has been 2 buildings damaged in Tono, in the Iwate Prefecture.
6 non-dwelling buildings have also been partially damaged.
In addition, one educational facility was damaged and also a cleaning facility.
No damage to nuclear facilities has occurred.
The damage denotes CATDAT ORANGE.

07:15 UTC : JMA has revised its earthquake parameters to a magnitude of 6.4 @ a depth of 47 km.

to read more, go to:   http://earthquake-report.com/2011/07/25/very-strong-coastal-earthquake-near-ofunato-japan/