Tag Archives: fault lines

Kyushu Earthquake, Mt Aso and the Relationship between Volcanoes and Earthquakes.

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In the past week the Japanese Island of Kysushu has be ravaged by earthquakes.

2016-04-16Japan is a highly seismic area with noticeable quakes in some areas occurring nearly daily.  But things began to escalate for the Kyushu region on Thursday night when a magnitude 6.5 quake brought several buildings down. As rescue efforts began the region had two more huge after shocks during the night, one over Mg 6 and the other > Mg 5. By midday Friday the death toll stood at 9 with over 800 injured and although the aftershocks kept coming many >Mg 4 people were still being pulled from the rubble. Sadly these events were quite possibly a precursor to something larger.

At 01.25 local time (15.25 GMT) a Mg 7.3 struck just north of Kumamoto just kilometers from the large earthquakes which had already occurred. Much of the seismicity in the Kyushu region is related to the subduction of the Philippine Sea plate at great depth. However this series of earthquakes have occurred at very shallow depths several hundred kilometers northwest of the Ryukyu Trench. They have been cause by strike-slip faulting within the Eurasian plate.

Quake damaged houses in Kumamoto, Japan (16 April 2016)So far 22 more people have been reported dead but this is expected to rise in the coming days with at least 80 people known to betrapped in rubble. 11 of which are trapped in a Tokai university apartment in the town of Minami Aso.

 

The shallowness of the earthquakes means damage to the surface is high and it is not just collapsing building which are a hazard. People have fled the area down stream of a dam which collapsed soon after the earthquake. Landslides in the area have taken out roads and power lines and with heavy rain anticipated over the coming days JMA have advised mudslides will be a huge problem for rescuers.

 

 

 

 

 

 

The seismic problems of Kyushu may have also set in motion another geohazard in the form of Mt Aso. Yesterday one of my favorite volcanology bloggers Eric Klemetti tweeted “Quite a few volcanoes on Kyushu and these earthquakes have been centered near Unzen, Aso, Kirishima. This is NOT to say these earthquakes will trigger any eruptions, but could be worth watching over the next year.” Several hours late JMA reported a small scale eruption at Aso. Smoke plumes have migrated 100 meters above the summit and it is not yet clear if the activity is magmatic (caused by movement of magma towards the surface) or phreatic (steam explosion caused by heating of groundwater).

Eruptions and earthquakes do not always come hand in hand but each one can contribute to the other or not at all depending on the circumstances. One indication a volcano is about to erupt is volcanic tremors; these low frequency earthquakes are usually caused by the migration of magma or changes to magma chamber. Although they are rarely higher than a magnitude 4. On the other side large earth quakes can cause faulting in bed rock which allows magma to exploit a new weakness and find a path to the surface it previously could not intrude on. The same can happen for ground water with faulting caused by a quake allowing it to seep in to geothermal areas it previously did not have access to due to the impermeability of the rock. When earthquakes hit volcanic regions volcano observatories always keep a closer eye on vulnerable or highly active volcanoes as a precaution but it is not always needed.

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The Aso Caldera complex has one of the world’s largest calderas. It is comprised of a 25 km north-south by 18 km east-west Caldera and a central cone group comprised of Mt. Neko, Mt. Taka, Mt. Naka, Mt. Eboshi, and Mt. Kishima. Mt Naka where the eruption has just taken place is the most active with its most recent eruption taking place last October. Although much of Aso’s activity in the past century has been relatively small it has had a violent history with at least 4 VEI 7 events in the past 300,000 years.

It’s is not clear whether the earthquakes in the past few days did trigger the current current eruption but JMA are keeping a close eye on the situation and I will update this page as I know more.

 

 

Figure 1. http://earthquake.usgs.gov/earthquakes/map/

Figure 2; http://www.bbc.co.uk/news/world-asia-36061657

Figure 3; http://www.independent.co.uk/news/world/asia/japan-earthquakes-dozens-reported-dead-injured-second-quake-two-days-a6986931.html

Figure 4; http://mashable.com/2016/04/15/japan-earthquake-landslide-photos/

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Today in Geological History – March 27th; The Great Alaskan Earthquake

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The second strongest earthquake ever recorded occurred at 5.36 pm AST (3.46 am 28/03 UTC) on Good Friday in Prince William Sound, Alaska. Registering a massive 9.2 on the moment magnitude scale, it shook the region for 4 and a half minutes and generating a tsunami which propagated through out the Pacific Ocean.

The Pacific Plate moves northward and subducts under the North American plate along the northern edge of the Pacific Ocean creating a highly seismic zone and the explosive volcanics of the Aleutian Islands. On March 27th 1964 the Pacific Plate jolted forward in a megathrust earthquake causing major vertical and horizontal displacement in an area spanning over 250,000  km

At the time of the earthquake Alfred Wegener’s theory of plate tectonics was only just being proven by surveys of the worlds oceans. Although the study of seismology and the several large subduction earthquakes which happened in this era helped prove the theory it meant little was understood about the mechanics of megathrust earthquakes (a termed created in the wake of the Great Alaskan Quake). Earthquake resilient building standards where  at the time and all where unprepared for  the events of the Easter weekend.

At a depth of just 23 km the focus was just 125 km northwest of the states capital Anchorage which took most of the damage.It hit a high of XI on the Mercalli Intensity scale, the second highest mark, indicating the intensity of the shaking experienced in the area. The shaking tore apart buildings and subsidence ripped apart roads. Anchorage was built on sandy bluffs and clay, the earthquake caused a landslide which buried 75 homes. The control tower at Anchorage International airport was reduced to rubble.

139 people lost there lives, mainly due to the tsunami which badly hit much of the Alaskan coastline but also claimed lives as far away as Crescent City, California where 12 were killed. At its maximum the tsunami reached as high as 220 ft in Shoup Bay, but most were much smaller. Alaska was actually hit by multiple tsunami, one caused by the earthquake itself and then several local smaller waves up to hours later prolonging the suffering and hampering rescue operations.

The Great Alaskan Earthquake changed much of our understanding of the sheer power of our planet, which rang like a bell with vibrations for days after. Waterways as far south as Texas sloshed from side to side as the seismic waves where felt throughout the continent.

USGS worked quickly to collect data, recording the subsidence and uplift in the region. They began to see how secondary faults accommodated the erratic displacement. They also began to form a much clearer picture of the Aleutian Trench where the Pacific Plate subducts cementing the idea of plate tectonics. It also shone light on the major part soil liquefaction had in the destruction of the area. Core samples taken along the Copper River indicated that the Good Friday was not the first megathrust event in the area. Analyzing just 50 ft cores scientists revealed evidence of 9 megathrust earthquakes in the past 5,500 years.

The events of March 27th lead to the USGS beginning installation of an extensive earthquake-monitoring network across Alaska as part of the Advanced National Seismic System. In 1966 the National Earthquake Information Center was established as apart of the US Coast and Geodetic Survey and was transferred to USGS control in 1973. By 1977 Congress passed the Earthquake Hazards Reduction Act, the world was beginning to take the threat seriously.

Figure 1; https://www.google.co.uk/url?sa=i&rct=j&q=&esrc=s&source=images&cd=&ved=&url=http%3A%2F%2Fwww.theoildrum.com%2Fnode%2F8573&psig=AFQjCNHCK3Uk0lxyjJZhA8t2fmQn_Kq8iQ&ust=1459094529661721

Figure 2; http://earthquake.usgs.gov/earthquakes/events/alaska1964/

Figure 3; http://www.wired.com/2009/07/tsunami/

 

Today in Geological History; March 11th – Tōhoku Earthquake & Tsunami

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article-0-0D924D9F000005DC-785_964x591.jpgI am pretty sure I have covered this event before but seeing as today marks the 5 year anniversary of one of the worst natural disasters in the past decade I thought it deserves a much more in depth look. The events of March 11th destroyed the lives of hundreds of thousands of people and claimed the lives of nearly 20,000. For me, it opened my eyes to a world of geohazards and mad me realized this was something I wanted to study and understand so such loss of life would not happen again.

There are three elements to the events of March 11th that I am going to look at here; the earthquake, the tsunami and the Fukushima power plant. Each aspect a huge disaster in on there own but interlinked as they were caused devastation for Japan. 

The Earthquake

Instrumental Intensity Image

Japan is a volcanic island which stretches along where the North American, Pacific, Eurasian and Philippine plates all collide at different points. It is a part of the Pacific Ring of Fire, the world’s most tectonically active area. Practically all of our planets largest and most destructive earthquakes occur along the ring, one of which rocked the east coast of Japan at 2.46 pm JST (5.46am UTC) on March 11th 2011.

The magnitude 9 quake struck at the shallow depth of just 32 km roughly 70 km off the Oshika Peninsular. The area was already alert to seismic activity as several large foreshocks had occurred in the run up including a Mg 7.2 on March 9th and followed by three more above a Mg 6. Of course no one knew these were precursors to something much larger…

Initial reports from JMA and USGS put the March 11th quake at a 7.9 but this had risen first to a 8.8 and then to a 9 before most of the seismic waves had even hit Tokyo 373 km away. Luckily thanks to Japans intense seismic network the countries capital had at least 80 seconds warning before they felt the strong shaking.

The megathrust earthquake occurred where the Pacific Plate subducts beneath the North America Plate. The Pacific Plate moves at a relative speed of roughly 9 mm per year but it is not a smooth decent, tension can build and release in a large snap causing an earthquake. On March 11th this happened in epic style causing over ~50 meters of displacement near the Japan Trench which caused the tsunami which swept across the Sendai planes. The earthquake was so powerful that up to 1.69 meters of co-seismic deformation has permanently altered our planet and affected the Earths tilt shaving 1.8 microseconds of the day (not that we would ever notice!)

It was the forth largest earthquake ever recorded and the largest ever to strike Japan.

The Tsunami 

The displacement on the sea bed in turn caused a huge displacement of water in the Pacific ocean its self. Across a 180 km stretch there was recorded up thrust of 6-8 meters. Above the rupture the tsunami waves would have looked like no more than ripples on the surface radiating out across the ocean. It is as the waves reach the continental shelf and the water is forced upwards that they begin to take on their characteristic ‘wall of water’ appearance.
At its maximum height (recorded at Miyako, Iwate) the waves hit 40.5 m high (133 ft). The Pacific has the most comprehensive tsunami warning systems in the world but even this gave only about 15 minutes warning from the earthquake to waves hitting the coast line. Travelling at speeds up to 500 mph the water surged up to 6 miles (10 km) inland.

Honshu earthquake tsunami travel times

It was not just Japan which felt the repercussions of the event. Tsunami waves propagated out through out the entire Pacific. 11,000 miles away the coast of Chile experienced waves in excess of 2 meters along with most of the America west coast right up through to the Aleutian Islands and as far south as Antarctica where it broke chunks off the Sulzberger Ice Shelf

An estimated 5 million tonnes of debris began washing up on shore lines across the Pacific in the months and even years after the initial Earthquake. In April 2013 a 20 ft boat ran aground in California and was later identified as belonging to the marine sciences program at Takata High School, Japan. NOAA have kept tracks and aimed to clear as much of the debris as possible to minimize risk to ships and wild life but the operation can take more than a decade.

Fukushima

The melt down at the Fukushima was the worst nuclear disaster the world has seen since Chernobyl in 1986.

The plant ran by TEPCO had 3 of its 6 units shut down for inspection when the earthquake struck. Units 1, 2 and 3 then under went automatic shutdown cutting off power. 50 minutes later the waves up to 15 meters high breached the measly 5.7 meters seawalls and flooded the basements of the turbine buildings and disabling the emergency generators. The lack of power meant the cooling systems of the 3 active reactors failed and eventually the heat caused by decay caused the containers to burst leaking radioactive material.

It was classified a Level 7 on the International Nuclear Event Scale (INES) and its was the way the event was handled from the very beginning my TEPCO which saw the escalation in the threat. Approximately 15 PBq of caesium-137 was released along with some 500 PBq of iodine-131, luckily all the failed reactors were in concrete containment vessels, which limited the release of strontium-90, americium-241 and plutonium.

Dozens of vehicles lie abandoned and covered in overgrown bushes along what was once a stretch of road near the power plantNo deaths were caused by the events or short term radiation exposure but it is thought people in the area worst hit will have a slightly higher risk of developing certain cancers in the future. Now 5 years on there is still a 12.5 km is still in place with thousands of people still exiled from their homes. The wild has reclaimed the land making it look like a scene from an apocalyptic film.

It could be centuries before the area is truly deemed safe to live on again.

Pre-Warning; This has happened before

Japan is no stranger to tsunamis; the 1896 and 1933 Sanriku earthquakes (Mg 8.5 and 8.4 respectively) also brought deadly waves. For this reason tsunami barriers have been constructed both on and off shore, trees were planted along the coastline, vertical evacuation buildings were built to the highest standards and regular evacuation training was introduced. But none of these were built to with stand the sheer force of a tsunami of this magnitude.

In 2001 a team from Tohoku University published an article in Journal of Natural Disaster predicting such an event occurring every 800-1100 years. Within the Sendai Plain there is evidence of at least 3 major tsunami deposits all left within the past 3000 years. On July 9th 869 BC what is believed to be a magnitude 8-9 earthquake occurred off the coast of Sanriku causing a major tsunami which left deposits up to 4 km inland. So given that we knew an event like this had occurred before, why was Japan not better prepared for March 11th?

Sadly human nature does not always listen to the reason of science. It is often easier to believe ‘it won’t happen in my life time’ and then brush the threat under the carpet for future generations. The problem is it does not matter how much we study the mechanics of our planet we are still no where near being able to predict these disasters with any degree of accuracy meaning preparation is our best defence.

Aftermath

A report issued by the Japanese government in May 2015 claimed the events of March 11th 2011 caused $300 billion dollars. A confirmed 15,894 people lost their lives, 2,562 people are still unaccounted for.

5 years on the area is yet to recover. An estimated 174,000 are still displaced mainly due to the exclusion zone still heavily in place around the Fukushima plant. Soon as the initial rescue operation was completed the Tohoku Earthquake Tsunami Joint Survey Group was assembled. A team of natural scientists and engineers from 63 universities world wide set out to understand what made this tsunami so powerful and how we can protect our selves from further events. By the end of 2011 the Japanese government had passed laws to establish “tsunami-safe cities” and pledged billions of dollars to an intense 5 year clean up operation. It was clearly a bigger job than they originally thought….

Today there are still over 60,000 people living in temporary accommodation.For residents once living near the Fukushima power plant they will probably never return to there own homes. Sendai is still trying to recover from the tragic events but also now living in fear that this could occur again.

It is for this reason I choose to go in to studying geoscience. We all live at the mercy of our planet and most of us never even consider the risk the land beneath our feet poses. Prediction, preparation and knowledge can save lives and this is what I one day want to help with.

 

Figure 1; http://www.dailymail.co.uk/news/article-1365318/Japan-earthquake-tsunami-The-moment-mother-nature-engulfed-nation.html

Figure 2; http://earthquake.usgs.gov/earthquakes/shakemap/global/shake/c0001xgp/

Figure 3; http://minookatap.com/2011/08/22/japan-book-club-the-big-wave-5/

Figure 4; http://www.livescience.com/39110-japan-2011-earthquake-tsunami-facts.html

Figure 5; https://7plaguesofgod.wordpress.com/2011-tsunami-japan/

Figure6; http://vassarchronicle.com/section/politics/foreign-affairs/lack-of-regulation-fukushima-meltdown/

Figure 7; http://www.dailymail.co.uk/news/article-3263714/Destroyed-man-reclaimed-nature-Amazing-images-reveal-exclusion-zone-Fukushima-abandoned-overgrown-wilderness.html

 

 

 

What Makes an Earthquake ‘Significant’?

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If you google “What is the definition of a significant earthquake?” you are met with Michigan Tech’s* response; Major – magnitude 7-7.9. However when looking at ‘significant’ earthquakes on the USGS** web page there are ones as low as magnitude 3.3. So to different people (and/or institutions) how we classify earthquakes seems to vary greatly and this occurs from top seismologists right through to media reporting and how we perceive the threat.

 

At 11.23 UTC on May 30th a Mg 7.8 earthquake struck off the coast of Japan. This is the same magnitude as that of Nepal’s April 25th quake but one managed to devastate an entire region and the other barely shook a few skyscrapers. Unless, like my self you concern your selves with the rumblings of our planet, or you live in Japan or the surrounding area you probably did not ever know last Saturdays earthquake even happened.

1. Aftermath of Nepal earthquake April 25th 2015.

The main difference between the two is the location of their foci. The focus of an earthquake (sometimes called the hyprocenter) is often confused with the epicentre, however the epicentre is the surface area directly over where the earthquake takes place, whereas the focus is the actual point at depth where the snap of energy takes place. With the Nepal earthquake the focus was just 15 km under a heavily populated region. The buildings on the surface were poorly built and unable to with stand the violent shaking, bringing them crumbling to the ground killing over 8000 people.

2. Displacement by Japan’s March 11th 2011 earthquake.

The Japan earthquake in contrast occurred off the coast, below the Pacific Ocean, although the some shaking was felt onshore. Many may assume this is safer than an earthquake under an urban area but several of the most deadly earthquakes occur at sea as they can induce tsunamis like that of March 11th 2011 which killed nearly 30,000 in Japan or the infamous Boxing Day Tsunami which killed as many as 230,000! Luckily on Saturday no tsunami alert was even issued, as the biggest difference between these two 7.8 earth quakes is depth.

Occurring at 677 km beneath the surface, this deep-focus (below 300 km) earthquake happened so deep its distance from focus to surface is only slightly shorter than travelling from London to Berlin (690 km)!!! As seismic waves travel they dissipate, loosing energy so are never as intense as what they are closer to the source.

3. Diagram of an earthquake, highlighting its focus and Epicenter.the waves lighten in colour with distance from the focus to show their loss of strength.

 

So so far we have magnitude, depth and location which impact on the devastation potential, but is there any thing else? Well we can expand on the last, location, to highlight other potential threats posed by an earthquake. A moderate sized earthquake in the heart of Los Angeles or Tokyo may stop the subway and send food flying off shop shelves but casualties should be low. The same earthquake in a country like Nepal or Haiti can kill thousands. Earthquakes don’t kill people per say, I have never heard of some on being shaken to death by a quake.What kills people is poorly constructed buildings collapsing, bridges failing, gas mains bursting causing fires. After past disasters such as San Fransisco’s great earthquake of 1906, wealthy countries which sit along active fault lines have put in place strict building codes and pumped millions in to disaster management programs and construction.   Obviously earthquake-proof is not always a possibility by earthquake-resistant definitely is and has saved the lives of many of the past few decades. Sadly not all at risk areas have that luxury of these safe guards at the expense of hundreds of lives.

4. Damage and fires caused by the Greath San Fransisco earthquake in 1906.

Seismology is a tricky business. With so much to take in to consideration when classify earthquakes, it is easy to see where there is often conflicting statements. Things are complicated further by the multitude of scales actually used to quantify them. When asked what scale is used, I can guarantee most will say the Richter scale (or local magnitude, ML), that is even what I was taught in school. Charles Richter first put his scale to use in 1935 to give a more scientific quantification for earthquakes than the previously used Mercalli scale which was solely based of human perspective and building damage (this is still used today but not as often). The Richter scale was limited in many ways being primed for nearby, mid-sized earthquakes (M 3-7). Seismologist Beno Gutenberg expanded on Richter’s work greatly enabling the scale to factor in greater distances and separated scales for surface waves (MS) and body waves (Mb).The revised scales still had difficulties and were particularly ineffective when looking at earthquakes which spanned great lengths of fault lines such the Aleutian Fox Island quake of 1952. The Richter scale was finally replaced by the Moment magnitude scale (MW) back in 1979 and this is the scale used by most institutes today including USGS.

Moment magnitude was born from elastic dislocation theory put forward in 1972 which suggests that energy release from a quake is proportional to the surface area that breaks free, the average distance that the fault is displaced, and the rigidity of the material adjacent to the fault. It is based on a similar logarithmic scale to the Richter scale with each step equating to an increase in the amount of energy released 101.5 ≈ 32 more than the previous. Earthquakes usually have similar Richter and moment magnitude numbers but rarely exactly the same and this can be one way one earthquake can be reported at different levels across the media if their sources used different scales. Another way which causes different figures  is precision; the more seismic stations used to calculate magnitude the more precise the result. When an earthquake is first recorded institutes are likely to only use their own data but as soon as they have access to the global seismic network they can give a more accurate classification. This happen with Japan’s earthquake on May 30th, initial reports put it over a magnitude 8 but this was quickly downgraded to 7.8.

As you can see an earthquakes significance is a matter for debate and in many cases personal opinion. Magnitude and location (not just geographically but also politically) are the main factors but it tends to vary earthquake to earthquake.

Station VRI seismogram

5. Example of a seismograph.

 

Nepal Earthquake

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I sat in a bar last Thursday night discussing the rarity of large-scale natural disasters with several of my non-geologically minded friends. They were shocked to hear just how common certain hazards actually were. I explained that media coverage is scarce depending on fatalities or area of the occurrence, but we have actually been lucky not to have seen any particularly deadly events in a while. Sadly I spoke to soon…

Figure 1. Remains of the Bhaktapur temple, once a UNESCO world heritage site

At 11.56 am local time (06.11 UTC) Saturday, Nepal was rocked by its strongest earthquake in decades. The Mg 7.8 quake was intensified by its shallow depth, just 11 km below the surface, meaning waves had less time to dissipate and disperse leaving the region to feel its full force. This morning officials have raised the estimated death toll again to just under 4000 but it could be weeks before we have real figures. The rescue operation has been hindered by hundreds of aftershocks many over a Mg 5 and even several over a Mg 6 making them devastating events in their own right.

The effects where far-reaching with all neighbouring countries feeling the tremor. India has so far reported 67 deaths and China and Bangladesh 20 and 8 respectively. 19 people lost their lives on Mount Everest as the quake induced avalanches across the snowy region. It is the mountains highest fatality since explorers began ascending its flanks in 1953, scores of hikers are still believed to be stranded.

Figure 2. South Base camp was struck by an avalanche soon after the earthquake killing 12

Why has this earthquake been so devastating?
The answer is a combination of two factors;

Firstly the region is extremely tectonically active. The processes that caused this earthquake are the same that have given rise to the highest mountain range on the planet, the Himalayas. The Indian plate is moving north-northwest towards the Eurasia plate at a rate of 40-50 mm per year. The thick continental crust of the Indian plate instead of simply subducting under the Eurasian plate in to the mantle, like oceanic crust would, actually lifts the opposing plate creating the Himalayan mountain range. Large scale earthquake are relatively common along the subducting surface of the Indian plate as it sticks to the overriding plate, there have been 4 in the last century including Saturdays event. The largest was a Mg 8.0 back in 1934 roughly 240 km southwest of the recent quake; over 17,000 lost their lives. The last was back in 1988 claimed nearly 1500.

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Figure 3.

Secondly despite all this knowledge the country and many of its neighbours are grossly unprepared for such events. Nepal is one of Asia’s poorest countries, many of its residents live in extremely poorly constructed buildings and in many cases shacks. Building codes and regulations in place in richer at risk regions, say San Francisco, are simple non-existent in the Himalayan region. The epicenter was just 77 km north-west of the countries densely populated capital Kathmandu, were it’s believed at least 800 have lost their lives. Surrounding villages have seen complete devastation with no building and very few people surviving.

Figure 4. Huge displacement due to the quake.

Only last month at the UN World Conference on Disaster Risk Reduction identified the potential threat in the region but no further measures were put in place. Hopefully when the rebuilding process begins steps will be taken to limit the threat of future earthquakes.

Figure 1; http://www.theguardian.com/world/live/2015/apr/26/nepal-earthquake-death-toll-exceeds-1500-rolling-report

Figure 2; http://unofficialnetworks.com/2014/04/12-confirmed-dead-everest-avalanche

Figure 3;

Figure 4; http://www.cidi.org/disaster-responses/nepal/#.VT5EMpMYGuQ

Tsunami Awareness Week 2015

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March 22nd – 28th marks international Tsunami Awareness week. In the past decade humanity have witnessed to devastating tsunamis; Boxing day 2004 and Sendi March 11th 2011, both giving the world the bleak reminder of waters destructive power. But what actually is a tsunami and why are they so destructive?

Cars, trees and even buildings can be swept away as if they are mere toys. Japan March 11th 2011

tsunami

tsuːˈnɑːmi/
noun
noun: tsunami; plural noun: tsunami; plural noun: tsunamis
  1. a long, high sea wave caused by an earthquake or other disturbance.

The literal translation of ‘tsunami’ is ‘Harbour Wave’. This comes from the fact in open water a series of tsunami can travel thousands of mile visibly undetectable until they reach shallower waters causing them to rise up to the walls of water we know them to be.

They are caused by a large displacement of water most commonly by an earthquake or landslide, and are by far one of the most deadliest types of natural disaster. If you are in a coastal area and feel an earthquake it is often best to head to higher ground even if a tsunami alert has not been given, although most areas prone to tsunamis have quiet good warning systems waves still travel at speeds of up 500 km per hour, so even a few minutes warning may not always be sufficient.

The first warning of an income tsunami is often what is known as draw back. As water is displaced is often pulls water out to sea, so if you were sat on the beach it would appear as if the sea was withdrawing like at low tide but very quickly. Again if you see this, always best to get to high ground as quickly and calmly as possible.

A common misconception is that a tsunami is one wave, it is actually a series of waves. Also the first is often not the most powerful. This is why it can seem as the water just keeps coming as it gets further inland, its being forced by further waves.

Subduction zone earthquakes tend to cause the most powerful and deadly tsunamis such as the Boxing day or Sendi however the largest ever wave ever recorded was from a landslide induced tsunami at Lituya Bay, Alaska in 1958. Waves reached over 500 meters tall all this is in part the the shape of the bay as opposed to a landslide going in to open waters. Over 80% of tsunamis occur in the Pacific Ocean, the ring of fire.

If you are on a coast line in a at risk area, especially if holidaying and not too familiar with the area, make sure you check for evacuation routes and either easy access to high ground or strong, stable buildings which you can take shelter on high floors (wooden or unstable structures can be washed away!).

If you would like to know more here is a list of Tsunami Awareness Week links;

Mg 6.9 Iwate and Tsunami warning

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At 8.06 am local time a magnitude 6.9 submarinal earthquake occurred of the coast of Iwate, Japan. JMA have claimed it is an after shock from the mg 9, March 11th megathrust quake in 2011.

The following tsunami alert was released although this was played up by some media stations to a full blown warning.

This Tsunami Warning/Advisory was issued in the past
Occurred at 08:06 JST 17 Feb 2015
Region name Sanriku Oki
Depth about 10 km
Magnitude 6.9
Click the map to zoom in

Tsunami Forecast Region Category of Tsunami Warning/Advisory
IWATE PREF. TSUNAMI ADVISORY

Tsunami Warnings / Tsunami Advisories

Issued at 08:09 JST 17 Feb 2015

******************Headline******************
Tsunami Advisories have been issued for the following coastal regions of Japan:
IWATE PREF.

*******************Text********************
Tsunami Advisories have been issued for the following coastal regions of Japan:
<Tsunami Advisory>
IWATE PREF.

***********About Tsunami Forecast************
<Tunami Advisory>
Marine threat is in place.
Get out of the water and leave the coast immediately.
As the strong current will continue, do not get in the sea or approach coasts until the advisory is cleared.

<Tsunami Forecast (Slight Sea Level Change)>
Though there may be slight sea-level change in coastal regions, no tsunami damage is expected.

******* Earthquake Information ********
Occurred at 08:06 JST 17 Feb 2015
Region name SANRIKU OKI
Latitude 39.9N
Longitude 144.5E
Depth about 10 km
Magnitude 6.9

The following arrival times were issued;

Tsunami Forecast Region/
Tsunami Observation Site
High Tide Time Estimated Initial
Tsunami Arrival Time
<Tsunami Advisory>
  IWATE PREF. ( Area where tsunami is
expected to arrive first )
08:30 JST 17 Feb
    Miyako 13:28 JST 17 Feb 08:40 JST 17 Feb
    Ofunato 13:36 JST 17 Feb 08:40 JST 17 Feb
    Kamaishi 13:36 JST 17 Feb 08:40 JST 17 Feb
    Kuji-ko 13:23 JST 17 Feb 08:50 JST 17 Feb

The warning was then terminated at 10.21 local time.