Showing posts with label Nagano Prefecture. Show all posts
Showing posts with label Nagano Prefecture. Show all posts

Monday, 24 November 2014

Magnitude 6.8 Earthquake in Nagano Prefecture, Japan.

The Japan Meteorological Agency (which also monitors seismic activity) recorded a Magnitude 6.8 Earthquake at a depth of 10 km in Nagano Prefecture on Honshū Island, slightly before 10.10 pm Japan Standard Time (slightly before 1.10 pm GMT) on Saturday 22 November 2014. Over 40 people are reported to have been injured, seven of them seriously, in the incident, which was felt across most of central Honshū, and over 50 homes have been destroyed. A series of aftershocks have been reported since the event, and rescue teams are still searching the remains of many buildings for further survivors.

A collapsed home in Nagano Prefecture following the 22 November 2014 Earthquake. Associated Press/Kyodo News/Japan Out.

Japan has a complex tectonic situation, with parts of the country on four different tectonic plates. Eastern Honshu area lies on the boundary between the Pacific, Eurasian and Philipine Plates, where the Pacific Plate is passing beneath the Eurasian and Philipine Plates as it is subducted into the Earth. This is not a smooth process; the rocks of the two plates constantly stick together, only to break apart again as the pressure builds up, causing Earthquakes in the process. 

 The movement of the Pacific and Philippine Plates beneath eastern Honshu. Laurent Jolivet/Institut des Sciences de la Terre d'Orléans/Sciences de la Terre et de l'Environnement.

See also...

Ten people have been confirmed dead and 63 have been injured following an unpredicted eruption of Mount Ontake on central Honshū on Saturday 27 September 2014. At least 26 people remain...

The Japan Meteorological Agency recorded a Magnitude 5.5 Earthquake at a depth of 90 km in eastern Iwate Prefecture on northern Honshū Island, Japan, slightly...

The Japan Meteorological Agency recorded a Magnitude 6.2 Earthquake at a depth of 160 km, off the south coast of the Kantō Region of Honshu Island, slightly before 5.20 am Japan Standard Time on Sunday 4 May 2014...


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Friday, 6 June 2014

A fossil Filefish from the Middle Miocene of Nagano Prefecture in central Japan.

Filefish (Monacanthidae) are  Tetraodontiform Fish related to Triggerfish, Pufferfish and Trunkfish. They are found throughout shallow tropical and temperate waters in the Atlantic, Pacific and Indian Oceans. They get their name from their rough skins which was supposedly once used for finishing surfaces by by boatmakers. Despite being a widely distributed and specious group, they have a relatively short fossil record, with the oldest known specimens coming from the Miocene of North America, with later specimens being known from the Pliocene of North America, Italy and Greece, and the Pleistocene of Italy.

In a paper published in the journal Zootaxa on 10 April 2014, Yusuke Miyajima of Department of Geology and Mineralogy at Kyoto University, Fumio Ohe of Harayamadai in Seto City, Hakuichi Koike of the Shinshushinmachi Fossil Museum and Hiroshige Matsouka, also of the Department of Geology and Mineralogy at Kyoto University, describe a fossil Filefish from the in an outcrop of the Tazawa black mudstone Member of the Bessho Formation in the riverbed of the Hofukuji River at Sorimachi in Matsumoto City, Nagano Prefecture, central Japan. This locality has previously produced a variety of Fish fossils, as well as Molluscs (Scallops and Argonauts), Goose Barnacles and a Sperm Whale.

The specimen is placed in the extant genus Aluterus, which contains four living species found in tropical and temperate waters at depths of as great as 150 m. These are widely distributed across the globe, including in the waters off Japan. It is given the specific name shigensis, meaning ‘from Shiga’ the specimen being found close to the village of Shiga-Mura. It is preserved as a partial axial skeleton, lacking the head or pelvic girdle, as part and counterpart on a split slab of black siltstone.

Aluterus shigensis from the Bessho Formation at Sorimachi, Matsumoto City, Nagano prefecture. Photograph (A) and drawing (B) of the part of the specimen. Abbreviations: 1DBP, basal pterygiophore of the spiny dorsal fin; 2DP, pterygiophore of the soft dorsal fin; 2DP1, first pterygiophore of the soft dorsal fin; AF, anal-fin ray; AV1-7, first-seventh abdominal vertebrae; CF, caudal fin; C–H, compound terminal centrum; CV1-13, first-thirteenth caudal vertebrae; DS I, first dorsal spine; DS II, second dorsal spine; HS, haemal spine; LAF, last anal-fin ray; NS, neural spine; PH, parhypural. l shows the length of skeleton from second abdominal vertebra to caudal-fin base. Dotted area anterior to caudal fin shows the preservation of scales. Scale bars are 50 mm. Miyajima et al. (2014).

Aluterus shigensis. Photograph (A) and drawing (B) of the counterpart of the specimen. Abbreviations: 2DF, soft dorsal-fin ray; 2DP2, second pterygiophore of the soft dorsal fin; 2DPX, pterygiophore of the soft dorsal fin between neural spines of the ninth and tenth caudal vertebrae; AP, pterygiophore of anal fin; AP1, first pterygiophore of anal fin; PP, parapophysis. Other abbreviations as in Figure 3. Dotted area shows the preservation of scales. Square shows the area observed using SEM in Figures 7A and 7B. Scale bars are 50 mm. Miyajima et al. (2014).

Aluterus shigensis closely resembles the extant Aluterus scriptus, which has a global distribution in tropical and subtropical waters, where it lives on reefs and in lagoons, and has been reported living in temperate waters in areas where warm current flows are present. The Bessho Formation is thought to have been laid down in temperate waters, but contains significant numbers of formaminifera from warmer zones, implying the input of warm currents. This suggests that Aluterus shigensis could have pursued a lifestyle essentially similar to that of the modern Aluterus scriptus, implying that Filefish were not only reasonably widely distributed by the Middle Miocene (Japan and North America), but that they were already living similar lives to the modern Fish.

Scanning electronic microscope images of scales of the fossil, Aluterus shigensis (A and B) and the modern Aluterus scriptus (C). Note the close resemblance of the shape and size of scales of the fossil to those of extant Aluterus species. Scale bars are 100 μm. Miyajima et al. (2014).

Soft radiograph of a dried specimen of Aluterus scriptus. Miyajima et al. (2014).

Reconstruction of Aluterus shigensis. Scale bar is 50 mm. Miyajima et al. (2014).

A living specimen of the extant Filefish Aluterus scriptus in Aquarium Paris. 

See also…

 A new species of Pufferfish form French Polynesia.

Pufferfish of the genus Canthigaster (Sharp Nosed Puffers or...


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Friday, 1 July 2011

The Nagano Earthquake of 30 June 2011

At 8.16 am on the 30th June 2011 the Japanese Prefecture of Nagano was hit by an earthquake with a magnitude of 5.5 on the Richter scale, at a depth of about 4 km. This was followed by aftershocks at 8.20, 13.54 and 14.11. Earthquakes are surprisingly common in Japan, on the same day an earthquake with a magnitude of 3.7 hit the Iwate Prefecture and one of 5.3 hit Fukushima. However the Nagano earthquake and its aftershocks were very close to the surface (by contrast the Iwate earthquake was at a depth of 10 km and that in Fukushima was 20 km deep), so that much of the power of the quake was felt by the inhabitants of the prefecture. This lead to at least eight injuries and some damage to the historic Matsumoto Castle.

Map of Japan, showing the epicentre of the earthquake (red cross) and the intensity felt at the surface, measured on the JMA intensity scale.
Japan uses the Japan Meteorological Agency (JMA) scale to measure the effects of Earthquakes. This is similar to the Mercalli Scale, in that it records ground acceleration at the surface rather that worrying about the energy output at the actual hypocenter of the quake. This enables then to map the effects on the surface, as shown in the map above, where the area around the epicenter experienced a JMA scale 5 quake, and an area to the north a scale 3 quake. It also enables comparison of how earthquakes actually impact on people. Thus on the 30th June Japan had two earthquakes with a magnitude of greater then 5 on the Richter scale, in Nagano and Fukushima, but while the shallow Nagano earthquake achieved a JMA scale of 5, the 20 km deep earthquake at Fukushima only produced a JMA reading of 3.


Map of Japan showing the epicenter of the June 30 Fukushima Earthquake, and intensity experienced on the shore.
Japan lies on the Pacific Ring of Fire, that is to say the ring of subduction zones that surounds the Pacific Ocean causing earthquakes an volcanicity. Two subdution zones pass under Japan, as the Philippine Plate to the south and the Pacific Plate to the east are forced under the Asian Plate to the northwest. Japan has over a hundred active volcanoes, caused by melted material from the subducting plates rising to the surface, and, as noted above, is extremely prone to earthquakes.

There have been five major earthquakes in Japan so far this year.

On the 9th of March an earthquake with a magnitude of 7.2 on the Richter Scale hit Tōhoku, on the northeast of Honshu Island, at a depth of 32 km. This is 12 km deeper than the Fukushima earthquake of 30 June, but the Richter Scale is logarithmic, each point on the scale being ten times as great as the previous point, to a magnitude 7 quake is a hundred times as strong as a magnitude 5 quake - more than enough to offset a 50% increase in depth.

At 14.46 local time on the 11th of March a second earthquake (though they were clearly connected) hit Tōhoku, this time with a magnitude of 9.0 on the Richter Scale and at a depth of only 24.4 km. This is one of the largest earthquakes ever recorded, and caused a tsunami which lead to widespread devastation. Several towns were completely destroyed, 15 500 people are known to have been killed, and at least 7000 more are missing. The earthquake and tsunami also caused a meltdown at the Fukushima Nuclear Reactor, which is still causing Japan serious problems.


The aftermath of the deadly Tōhoku Earthquake & Tsunami.

45 minutes later a second earthquake (though again this was clearly related) hit the same area, with a magnitude of 7.1 0n the Richer Scale, and at a depth of 19.7 km. This clearly contributed to the chaos and devastation caused by the earlier quake, though the two were to close together to produce accurate separate casualty statistics.

On April the 7th an Earthquake hit Miyagi (southeast Tōhoku) at a depth of 49 km and with a magnitude of 7.1 on the Richter Scale. This was almost certainly related to the earlier Tōhoku earthquakes. This quake caused the loss of four lives and 141 minor injuries. It also caused some damage to roads and houses, and a power outage which in places lasted over two days.

On the 11th of April an Earthquake measuring 6.6 on the Richter Scale hit Fukushima (also southeast Tōhoku) at a depth of 10 km, causing the loss of three lives, with another three people being critically injured, and seven more sustaining minor injuries. The quake also caused several fires, widespread power outages, and a mudslide that closed several roads. Again this was almost certainly connected to the earlier Tōhoku quakes.

See also The Christchurch Earthquakes,
Rethinking Energy and Earthquakes on Sciency Thoughts YouTube.