Friday, 8 July 2011

Earthquake in the Kermadec Islands triggers tsunami alert.

The Kermadec Islands are the northernmost outpost of New Zealand, situated 650 km northeast of North Island, and 550 km southwest of Tonga. They are a Volcanic Island Arc, which is to say a group of islands that sits on a convergent plate margin (in this case the one where the Pacific Plate is being subducted beneath the Australian) and are formed entirely by volcanic activity. This volcanic activity occurs when rocks from the subducted plate melt as they are drawn into the earth's (hot) interior, then rise up through the overlying plate.


The Kermadec Islands.

The islands host four volcanoes, two of which, Raoul and Curtis, and a number of volcanic seamounts (marine volcanoes which do not poke above the surface) the most notable of which is Monowai Seamount, 120 m below the surface, and lies halfway between Raoul Island and Tonga - another island arc on the same convergent plate margin. To the south of the Kermadec Islands the South Kermadec Ridge Seamounts stretch most of the way to New Zealand; the most southerly, the Rumble IV Seamount, is only 150 km north of North Island, which itself lies on the Australian/Pacific margin.

The islands were settled by polynesians in the 14th century (and possibly separately in the 10th), but these settlements were long abandoned when the first Europeans arrived in the eighteenth century. Today only Raoul Island is inhabited, by a small group of meteorologists and conservationists.

At about 7.00 am on the 7th July (local time) a magnitude 7.6 earthquake was recorded 20 km beneath the Kermadec Islands. The earthquake was associated with the Kermadec Trench (i.e. the trench formed by the Pacific Plate being forced down beneath the Australian) rather than any volcanic activity. This triggered a Tsunami warning from the New Zealand Ministry of Civil Defence and Emergencty Management, but this was cancelled when no tsunami was forthcoming.

See also The Christchurch Earthquakes and Earthquakes on Sciency Thoughts YouTube.

Thursday, 7 July 2011

The Hekla Volcano - is the Gateway to Hell about to open?

Hekla is one of Iceland's largest and most active volcanoes. It has a recorded history of eruptions dating back to 1104, 130 years after the date most commonly given for the initial colonization of Iceland (historians and archaeologists argue about this, but that's another story), and geological evidence of eruptions dating back over seven thousand years. The volcano is thought to have produces about five cubic kilometers of tephra (volcanic ejecta) in the last thousand years; about 10% of all the tephra produced in Iceland during this time. Hekla is unique among Icelandic volcanoes in that it produces calc-alkaline lavas, more typical of subduction zones than the mid-oceanic rift on which Iceland sits. This makes ash beds caused by Hekla's activity distinctive, enabling geologists to say with some confidence that ash layers as far away as Scotland and Scandinavia originate from Hekla.


Mount Hekla.

The volcano takes the form of a stratovolcano (classic volcanic cone) at the end of a volcanic ridge. In major eruptions a fissure up to 5 km long can open along the ridge.

In addition to being calc-alkaline, ash from Mount Helka is unusually rich in fluorine, which has led to a number of mass poisoning incidents associated with ash falls from Hekla. The volcano has also been known to throw lava bombs for over a kilometer, with one in 1947 being recorded as falling 32 km away.

Ash fall deposits associated with Hekla in Europe have been dated to 5050 BC, 2310 BC and 950 BC. In 1846 an eruption caused ash falls in the Faroes, Shetlands and Orkneys that were associated with widespread livestock deaths. In 1947 an eruption caused ashfalls as far away as Helsinki.

The prospect of an eruption from Helka is clearly a worrying prospect, particularly after the recent eruptions from Eyjafyallajokull and Grimsvötn volcanos in Iceland caused major disruption to air traffic in Europe. Hekla has a track record of sudden eruptions, not proceeded by earthquakes.

On the 7th of July 2011 the media contained a number of reports of an imminent eruption on Hekla. Icelandic geophysicists Pall Einarsson of the Faculty of Earth Sciences at the University of Iceland, and Ari Trausti Guđmundsson, a geoscientist and science writer, were quoted as saying that there had been some activity around Mount Hekla and that the volcano was due an eruption.


Unfortunately 'due an eruption' means slightly different things to a journalist and a geologist. To a journalist this implies within the next week, to a geologist, the next decade or so. Einarsson and Guđmundsson found themselves trying to retract the story, and becoming frustrated with the press. Einarsson went as far as telling English language website IceNews that British journalists had disgraced their profession by the way the story had been reported (although he may not have fully realized what else the UK press has been up to lately).

Hekla is situated on, and fed by the Mid-Atlantic ridge. Eruptions on Hekla follow a pattern; when the volcano has been quiet for a long time, pressure will have built up for a long time, leading to a massive eruption. The devastating 1947-8 occurred after a century of inactivity. The last eruption was in 2000, which was not particularly notable - before then Hekla had erupted in 1991, 1981, 1980 and 1971. So it is likely that if Hekla does erupt in the near future then it will not be a major eruption. But that doesn't make a very good story.

See also The Grímsvötn Volcano and Volcanoes on Sciency Thoughts YouTube.

Wednesday, 6 July 2011

Walking with Giant Wombats.

This week scientists in Australia unveiled a new specimen of Diprotodon optatum, an extinct rhinoceros sized marsupial widely referred to in the press as a 'Giant Wombat'. Diprotodon is a fairly well documented animal, but this specimen is one of the most complete and well preserved found to date, as well as being the most northerly specimen yet discovered.
A specimen of Diprotodon from Natural History Museum in London.

The specimen was uncovered at Floraville Station by the Liechardt River in the Gulf of Carpentaria, between the towns of Burketown and Normanton. The dig was lead by Mike Archer and Henk Godthelp of the University of New South Wales, Scott Hucknell of the Queensland Museum and Gilbert Price of the University of Queensland. The excavation formed part of a wider Australian Research Council Linkage Project into climate change in Northern Australia, led by Sue Hand, also of the University of New South Wales, and including scientists from the Australian Nuclear Science and Technology Organisation, the University of Melborne, the University of Wollongong, and Outback at Isa.

Diprotodon was found across Australia from about 2.5 million years ago, until sometime after 55 000 years ago, the date of the most youngest specimen yet dated (bone tissue from the Floraville Station specimen has been taken for dating, but no results are yet in). It is suspected that Diprotodon died out, along with other members of the Australian megafauna, at roughly the time the first humans arrived in Australia. The earliest known human remains in Australia are a pair of skeletons from Lake Mungo in New South Wales, imaginatively dubbed 'Mungo Man' and 'Mungo Woman', dated at 40 000. Humans had clearly lived in Australia some time before this, as Lake Mungo is not near any probable site for the first arrivals.

The excavation of Mungo Man.


Australia underwent a change in climate at roughly the same time that the first humans settled the continent. Palaeoclimatologists argue as to whether this climate change was due to natural causes, or human activity, in particular the practice of burning vegetation. In addition archaeologists argue as to whether this climate change was the cause of the loss of the Australian megafauna, or whether humans were more directly involved in the extinctions, hunting animals to extinctions. The same debate occurs on other continents, particularly North America, where human arrival coincided with megafauna extinctions.

The dating of the Floraville Station Diprotodon, and other megafauna components from the same site, such as giant kangaroos and lizards, combined with studies of the climatic conditions at the site, could potentially shed light on this debate.

The scientists also hope to see how the skeleton differed from animals from further south. There were once eight named species of Diprotodon across Australia, but a review of the specimens by Gilbert Price, one of the scientists on the Floraville Station dig, suggested that there were only actually two different body plans, and that most large Australian marsupials showed a strong degree of sexual dimorphism, which lead him to the conclusion that there was only a single species, Diprotodon optatum, the original species described in 1838 by the British zoologist Richard Owen. Many Australian animals show variation between the tropical north and the subtropical south, even within species.

See also Out of Africa(?), An Australian Spinosaurid and Mammals on Sciency Thoughts YouTube.

Monday, 4 July 2011

LH PV18, a New Mini-Tyranosaur, or an Immature Tarbosaur?

The Tyranosuarids are iconic dinosaurs, large bipedal predators with reduced forelimbs and powerful jaws. No dinosaur movie would be complete without an appearance by Tyranosaurus rex, the most famous member of the group, and species which gives the group its name. Tyranosaurids are relatively well known, there are quite a few good specimens, but almost all of these are from the Late Cretaceous; the earlier history of the group remains obscure.

In September 2009 a team lead by Paul Sereno of the Department of Organismal Biology and Anatomy at the University of Chicago published a paper in the journal Science in which they described a possible Early Cretaceous Tyranosaurid from northeastern China. This description was based upon a single specimen, LH PV18, given the Latin binomial Raptorex kriegsteini.


Specimen LH PV18, Raptorex kriegsteini.

Specimen LH PV18 had a dubious provenance. The specimen was purchased at the Tuscon Gem, Mineral and Fossil Showcase by Henry Kriegstein, an ophthalmologist and amateur fossil hunter (after who's father the specimen was named), who then donated it to Sereno's laboratory. Kriegstein bought the fossil from Hollis Butts, a Japan based dealer specializing in fossils from the Far East. Butts apparently sold the specimen as being from Mongolia, but there were persistent rumors that the fossil really came from China (it is illegal to export such specimens from China, so it is hardly surprising that Butts would deny this).

Sereno et al. examined the matrix in which the fossil was set for other fossils in an attempt to verify the provenance of the specimen. They claim to have found numerous smaller fossils, including 'fish bones, turtles, clam shells and other fauna', and on the basis of these concluded that the fossil originally came from the Lujiatun Beds of the Lower Cretaceous Yixian Formation in Liaoning Province, north-east China. Sereno was sufficiently convinced of this diagnosis to donate the specimen to the Long Hao Institute of Geology and Paleontology at Hohhot in Inner Mongolia, China.

Using small fossils to date rocks (or biostratigraphy) is very much the meat of palaeontology. Many small, shelly groups of creatures have very high rates of species turnover and palaeontologists can use this to date sediments very accurately - within hundreds of thousands of years on sediments hundreds of millions of years old. This information can be used to build up detailed models of the structure of sedimentary beds. These stratigraphic models are vital for the oil industry, as well as for engineering projects such as the Channel Tunnel.


A biostratigraphic section of part of the Neuqué Basin in the Argentine Andes, using nanofossils, ammonites and bivalves.

The actual specimen is a nearly complete skeleton roughly 2.5 m long, that probably came from a living animal 3 m long. The specimen was clearly not fully mature, as not all of its bones were fully ossified and fused, however several bones had fused which Sereno et al. interpreted to indicate that the animal was close to maturity.

This was two speculative jumps in a single paper; the dating and location of the original fossil, plus the age of the specimen, so it was unsurprising that the paper was duly challenged.

Peter Larson is co-owner of the Black Hills Institute of Geological Research, a private fossil hunting company based in Hill City, South Dakota. The Institute specializes in finding and preparing museum grade fossils; it was responsible for the discovery of 'Sue' the most complete Tyranosaurus specimen ever found, now housed in The Field Museum, Chicago.

Jørn Hurum is an associate professor of Paleontology at the University of Oslo. He specializes in Mesozoic Mammals and Dinosaurs, though recently he has been most famous for his description of Ida, an Eocene lemur.

In October 2010 Larson and Hurum spoke to the journal Nature about their concerns. To them LH PV18 looked like a juvenile specimen of Tarbosaurus, a well documented tyranosaurid dinosaur from Mongolia. Furthermore the provided supporting evidence for the age of the specimen didn't seem good enough. Despite having claimed numerous smaller fossils were found in the matrix, Sereno et al. provided images of only two, a pelycepod and a fish vertabrae which resembled one from a fish of the genus Lycoptera.

Pelycepod is another word for bivalve; the term is itself of little significance. Sereno et al. published a picture of a bivalve shell in their supporting material, without any description, and noted that pelycepods were common in the Lower Cretaceous Jehol fauna. To Larson & Hurum the specimen appeared to be a freshwater clam, a widespread and long surviving group, of little stratigraphic significance. To me it looks like a unionoid, or freshwater mussel, a group that appeared in the Triassic, and haven't changed much since. The fish vertebrae Sereno et al. described as probably from a fish of the genera Lycoptera, a fish abundant in the Jehol fauna, but with a fossil record dating from the Jurassic to the present. Thus even if the bone could be confirmed as coming from Lycoptera, this would be of no particular significance. Larson suggested that for a confident date far more reliable fossils would be needed, and suggested that the matrix material be analyzed for pollen, an excellent stratigraphic fossil.

In Jun this year (2011) a team lead by Denver W. Fowler of the Museum of the Rockies and the Department of Earth Sciences at Montana State University, published a more detailed review of LH PV18 in the journal PLoS One. Like Larson and Hurum they could not see any significance in the bivalve shell. They examined the fish vertebrae, and came to the conclusion that it did not come from Lycoptera, but was most probably from a ellimmichthyform fish, a group which survived from the Early Cretaceous till the Eocene. Fowler et al. suggest that in the absence of any stratigraphicly significant fossils it might be possible to date the sample using volcanic zircons in the matrix, or to analyze the bones for rare earth element content and try to correlate this with the rare earth content of bones from known localities.

In addition they performed an analysis of the osteology of the specimen and compared this to that of immature Tyranosaurus specimens from North America. From this they concluded that the level of development indicated a much younger animal than Sereno et al. implied. Tyranosaurus is very similar to Tarbosaurus, to the extent that some experts do not consider them to be separate species. If the two follow similar developmental patterns (which seems a reasonable conclusion), and LH PV18 really is a Tarbosaurus, then the pattern of development implies quite a young animal.

From this Fowler et al. conclude that there is no reason to conclude that LH PV18 is not an immature Tarbosaurus, and the name Raptorex is erroneous.

It is unlikely that Sereno, who is one of the world's leading dinosaur specialists, intended to deceive. Potentially a young palaeontologist striving to make a name for himself could be tempted to deliberately inflate the importance of their discoveries, but someone of Sereno's experience and reputation would have more to lose than to gain. It seems more likely that he allowed himself to be taken in by the romance of the apparently smuggled dinosaur, though Butts always claimed that the specimen came from Mongolia and was sold by him as an immature Tarbosaurus. This in itself would not be a bad discovery; no immature Tarbosuarus specimen has previously been described.

and Dinosaurs on Sciency thoughts YouTube.

Sunday, 3 July 2011

Mount Soputan, Sulawesi, erupts.

At about 6.00 am local time, on the 2nd of July 2011, Mount Soputan, on the northern arm of Sulawesi Island in Indonesia began to erupt, for the first time since October 2008. The volcano produced a column of ash and smoke which initially reached 5 km in height, then grew slowly throughout the day, eventually reaching 14 km, before suddenly subsiding at about midnight. This ash-cloud was been drifting steadily westward covering several hundred km. It continues to produce isolated bursts of ash. The Indonesian government has ordered local people not to go within 8 km of the sight, though since the volcano is in a fairy remote location it is unlikely that anybody would do this anyway. It is unclear what the volcano will do in the near future, though it is unlikely to prove hazardous to human life. Soputan is a fairly active volcano, but has not caused any recorded fatalities, due to its remote location. It is possible that it might become a hazard to aviation.


Soputan Volcano, Northern Sulawesi.

Mount Soputan is a stratocone volcano (a classic cone shaped volcano of the sort you would expect to see in a Hollywood movie) which forms part of the Tondano Caldera, a 20 x 30 km complex of volcanoes fed from a single source. In addition to Soputan the caldera contains the Sempu, Lokon-Empung, and Mahawu stratovolcanoes, the Batu Kolok and Sarangson Hot Springs, the Tampusu Cindercone (a cindercone is a cone of ashes which forms downwind of a volcanic vent) and the Lahendong Maar (a volcanic crater caused by an explosion when lava comes into contact with groundwater).

Soputan is an active volcano, having most previously erupted in 2008, then before that in 2007, 2006, 2005, 2004, 2003, 2002, 2000, 1996 and so on. In 1906 a vent opened in the north-east flank of Soputan. This vent, given the name Aeseput periodically produced lava flows until 1924, but has been inactive since.

Of the other volcanoes in the caldera, Lokon-Empung is also fairly active, Mahawu last erupted in 1789 and there have been no recorded eruptions on Mount Sempu, which hosts a sulphur mine.


An eruption on Mount Soputan.

Suluwesi forms part of the Pacific Ring-of-Fire. It lies on the border between the Pacific, Eurasian and Australian plates. The Australian plate is moving northward, butting into the Eurasian plate, which is moving south-eastward. Eventually this collision, may turn what is now Indonesia into an extension of the Himalayas, with Australia attached to South-East Asia. This is made more complex by the Pacific plate moving eastward, being forced under the other two plates and subducted into the Earth's mantle. As this happens waterlogged sediments are melted by the heat of the Earth's interior and rise up through the overlying plates to form volcanoes. Sulewesi has 13 active volcanoes, and there are hundreds more scattered throughout Indonesia.

Saturday, 2 July 2011

Out of Africa(?)

There are currently two main theories about the evolution and global migration of modern man.

The Out of Africa Hypothesis postulates that modern man evolved in Africa, with the first true members of our species appearing in Africa between 500 000 and 200 000 years ago, and then migrating out of the continent some time after 125 000 years ago, replacing all other species of humans.


The Out of Africa Model.


The Muli-Regional Hypothesis postulates that various species of humans spread around the globe about 2 million years ago, and that these separate species evolved into modern races of humans.

Different theories are part of the normal run of science, but when human origins are involved they can become very political. The two theories have very different implications as to how closely related we all are. Either we all share a common ancestry within the last half a million years and racial differences are merely superficial local adaptations to climate, or the different modern races are so distantly related they are nearly different species. However we cannot dismiss a scientific theory because we do not like its implications, but should consider the evidence for and against rival theories and try to make decisions based upon this.

The Out of Africa theory has the backing of the majority of palaeoanthropologists (scientists who study human origins). It was initially proposed by Charles Darwin in his 1871 book Descent of Man; a single human origin fitted with his theory of natural selection so this part of the theory is not overly surprising, what is surprising is that he postulated an African origin for mankind. At the time most scholars placed the origin of man in the Middle East, based upon biblical scholarship, the best evidence they were aware of (fossil humans were more-or-less unknown at this time). Darwin based his ideas on the African origin of man upon his (new and controversial) idea that we are descended from African apes. This was still at best a guess; the natural world was not as well documented in the eighteenth century as it is now, so it would not have been a great surprise if more human-like apes had subsequently been found somewhere in the jungles of Asia.

Charles Darwin, who's controversial views on the origin of man have stood the test of time.


The Multi-Regional Hypothesis as we currently know it did not exist in the eighteenth century, but it had its parallels. In the eighteenth century it was generally assumed that the different races of men were different species. When Linnaeus described humans he gave the different races different specific names; Homo sapiens (the thinking man) only applied to Europeans. This was convenient politically. It could be assumed that the biblical tales were about white people, when Jesus spoke of love for ones fellow man he obviously meant white men. Scholars seriously argued that Africans did not actually have souls; whatever the case it was clearly OK to enslave them; either they were animals, or an inferior sort of humans placed on Earth by god to do manual labour for white people. When Jean-Baptiste LaMark proposed his theory of evolution in 2009 he did not go as far as to say that different humans were different species, but his theories could definitely be read that way. LaMark thought that animals evolved by striving to improve themselves, actively trying to evolve towards a platonic ideal. Obviously in this scheme of things humans (and European humans at that) were the pinnacle of evolution, to which all other animals would strive. This could be interpreted to mean that different groups of humans had completely different origins. This theory did not even imply that apes were more closely related to humans than clams; species were more similar to humans because they were more strong willed than other species.


Jean-Baptiste LaMark's ideas on evolution seem ridiculous now, but were advanced for his time.

Since Darwin's time many fossil humans have been found, and a variety of human species named and placed in a number of genera. Most of these have been restricted entirely to Africa, but other members of the modern genus Homo have also been found in Asia and Europe. Nobody any longer disputes that the first humans arose in Africa, but it is disputed how long ago the ancestors of modern humans left Africa and diverged from one another.

Scientists have studied the genes and chromosomes of modern humans and come to some remarkable conclusions. Chromosomes have large chunks of non-coding DNA (sometimes called junk DNA). This DNA does not produce any proteins, so if it undergoes mutations this does not have any effect, good or bad. So while coding DNA (the DNA which codes for proteins) is subject to natural selection - beneficial mutations will quickly spread through a population, harmful ones will quickly be eliminated - non-coding DNA is not. Mutations can therefore accumulate at a steady rate, and this rate can be used to judge the time since different lineages diverged. This is known as the molecular clock.

Chromosomes come in pairs, and in each generation the genes on those pairs are recombined, forming a new chromosome with a combination of DNA from each parent, this can make the molecular clock method hard to interpret. However humans (and all mammals) have two sets of DNA which do not recombine; the male sex chromosomes Y, which is passed from father to son and never recombines with its partner the X chromosome (X chromosomes do recombine in women, so these are less useful), and mitochondrial DNA; DNA found outside the nucleus in organelles called mitochondria, and which are always inherited through the female line. It is therefore easy to assess the rate at which these chromosomes have accumulated mutations, making them a prime target for scientists interested in tracing the divergence of human populations.

When scientists examined the X chromosome they came to the conclusion that all humans had a common female ancestor approximately 160 000 years ago. This hypothetical female ancestor is sometimes known as the 'Mitochondrial Eve'. The Y-chromosomal DNA yielded even more surprising evidence, all male humans apparently shared a single male ancestor 60 000 years ago, sometimes called the 'Y-chromosomal Adam'.

This was not the end of the DNA story. Scientists were also able to analyze the entire human genome to look for diversity within different groups. By analyzing the DNA of thousands of volunteers from around the world it was possible to build up a rough family tree for humanity. This suggested that the greatest human diversity was found within African populations - all non-African populations, no matter what they look like - are comparatively closely related to one-another.


A family tree for the human race, based upon mitochondrial DNA

Evidence for the Multi-regional hypothesis is less solid. Some palaeoanthropologists claim that they can discern features on the skulls of ancient humans which resemble modern humans living in the same areas, and there have been claims (dubious) claims of recovered DNA from Neanderthals which suggests they might share some genes with modern Europeans which other ethnic groups lack.

Nevertheless the popular press has taken quite a liking to the Multi-Regional Hypothesis, and it is often reported as being of equal merit too, or even favored over, the Out of Africa Hypothesis. So when stories started appearing in the British media this week of a new paper being published that cast further doubts upon the Out of Africa Hypothesis, I was immediately suspicious.

Doubts over 'out of Africa' theory, Yahoo News, 29 June 2011.
'Out of Africa' theory thrown into doubt, Sunday Mercury, 30 June 2011.

The paper in question appeared in the journal Plos One and was by a team lead by Etty Indriati of the Laboratory of Bio- and Paleoanthropology at the Faculty of Medicine at Gadjah Mada University in Yogyakarta, Indonesia.

It does not actually make any reference to either the Out of Africa Hypothesis, or the Multi-Regional Hypothesis, but provides a re-evaluation of the date of the 20 Meter Solo River Terrace, one of the 'Java Man' sites, where remains of the the presumed human ancestor Homo erectus was found. Homo erectus has been found in eastern Africa, Georgia in southeast Europe, Turkey, India, China, Vietnam and Java, though not all scientists accept that all these specimens belonged to the same species. Most of these finds are over a million years old, but a much younger date, possibly as recent as 35 000 years ago, has been suggested for the Solo River site.


A reconstruction of 'Java Man'; the dark part on the skull was actually discovered, everything else is speculation.

What Indriati et al. did was to re-date the sight of the Solo River finds using isotope analysis of ash layers. This works something like this:

Mineral crystals are formed in volcanoes as liquid magma cools and solidifies. Each mineral forms at a range of temperatures, and (importantly) contains known elements. Some of these elements are mildly radio-active; they decay over time to form new elements. Since these new elements have different chemical properties, they would not have been present in the original minerals. Thus, since the rate at which these elements decay is constant, it is possible to compare the ratio of the original element to the product element within a mineral crystal and produce a date for the rock.

The Solo River site is on a floodplane, the material which makes it up has been deposited by rivers, and shows some mixing of material. However horizons of volcanic material exist within it that are unmixed, they give a constant date reading, implying they were deposited by discrete volcanic episodes. Using these horizons Indriati et al. were able to come up with a date of slightly over half a million years for the sight.


A reconstruction of the Solo River site.

What this tells us is that Java man was not a contemporary, or near contemporary, of the earliest modern humans in the area, or of Neanderthal man in Europe, as has been suggested, but rather lived and died long before the earliest anatomically modern humans appeared in Africa (or anywhere else). This does not preclude the possibility of Homo erectus having lived in the area until much more recently, but it does leave us with no evidence of this. As such it tends to support, rather than cast doubt upon, the Out of Africa theory.

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.