An earthquake simulator in Tokyo, Japan shows off what a Magnitude 9 earthquake feels like. Scary stuff!
An earthquake simulator in Tokyo, Japan shows off what a Magnitude 9 earthquake feels like. Scary stuff!
by Huw Goodall
Half awake, half asleep. The room is shaking. You realise you are not at home. You are in central Italy. Now the room is really shaking, you sprint over to hide under the desk as the floor moves under your feet, grabbing clothes as you go. The shaking continues, you put on the random assortment of clothes, pulling the bag you packed the night before, with the essentials to survive, close to you, wondering when the shaking will stop. Preparing mentally to be buried under the roof and hunker under the desk until the rescue team gets to you, you listen as the doors and windows rattle and bang. Then there is silence.
Pulling your shoes on (why didn’t you untie them last night!) you run into the corridor, your colleagues are out there, everyone is unhurt. Down the gloomy hotel corridor you all hurry out into the square, where slowly but surely the population of Ascoli Piceno gathers in the beautiful early morning sun. After an hour or so delay, including dashing back into the ancient building to grab field kit, interviews with the BBC and a delayed breakfast, you escape from the medieval town towards the epicentre of the earthquake.
Driving up the winding mountain roads, dodging between boulders that have been dislodged by the shaking, your team of 4 make their way towards the centre of the earthquake. As you approach, the tiny villages that dot the route show increasing signs of damage. Then you see it. The rupture. This is where the earth has been cut by the quake. The work begins. High precision surveys are taken from this site, after a brief discussion it is decided to return to where you were working the previous day and see if the fault has moved in the earthquake there too.
This involves driving through the isolated town of Castellucio, a stunning hilltop village, famous for its lentils. As you drive up the hill, the residents are in the street. Your Italian is only good enough to order food, but you can tell they are scared, confused and don’t know why you are there. You are probably the second car at most that has passed this way since the earthquake that morning. The destruction is clear, walls collapsed a pancaked building along the road, other houses simply gone. There is a helicopter landing in the street. People are everywhere.
Eventually the situation is explained in a hash of Italian and English and you are allowed to pass through, to continue to do your work as the people of the village continue to take stock. The next two weeks are non-stop field work, police checkpoints, late dinners and early starts. You measure how the fault has ruptured the surface, using a high-tech laser scanner, GPS, cameras and the good old fashioned ruler and notebook.
We spent the fortnight mapping new parts of the rupture as well as repeating measurements at some sites, to generate a picture of how the fault is moving in the days after the earthquake. This data set will be unlike any other in existence and hopefully will give us an insight into why earthquakes happen the way they do.
Huw is a PhD student in the School of Earth and Environment at the University of Leeds. His work involves using precise chemical analysis of earthquake faults to understand how they have moved in the past.
Bangladesh is one of the most disaster-prone countries in the world. In addition to frequent cyclones and drought, large areas of the country are at risk of earthquakes.
With densely populated cities, even a relatively small earthquake could have catastrophic consequences. Amrai Pari (Together We Can Do It) is harnessing the power of animation to help people be better prepared. Find out more about the project: http://bbc.in/2gsG8Tx
Since 1900, 35 earthquakes worldwide have each killed at least 10,000 people. Of these, 26 were in the Alpine-Himalayan seismic belt – a broad “crumple zone” where the African, Arabian and Indian tectonic plates collide with Europe and Asia. Most of these deadly earthquakes were caused by the rupture of faults that had not previously been identified.
Tim Wright is Professor of Satellite Geodesy at the University of Leeds and Director of the Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET). His work has been at the forefront of developing the use of satellite radar for measuring tectonic and volcanic deformation.
Below is a lecture presented by Tim at the Geological Society talking about his work trying to understand the nature of seismic hazard within the Alpine-Himalayan region.
A megathrust fault could be lurking underneath Bangladesh, India and Myanmar, exposing one of the most densely populated regions in the world to the risk of a large earthquake, according to new research published in Nature Geoscience.
A new GPS study measuring tiny ground movements since 2003 in the south Asia region has found strong evidence suggesting that a large tectonic fault beneath Bangladesh and east India is seismically active.
The team, consisting of scientists from the USA, Singapore and Bangladesh, calculate that the megathrust fault could be accumulating strain energy at rates of about 15 mm per year.
Importantly, the researchers believe that the fault is “stuck” and has been storing energy for more than 400 years without a major earthquake; since the Mughal conquest of Bengal and the establishment of Dhaka as the Bangladeshi capital in the 1600s.
An earthquake occurs when the stresses become large enough that it causes the fault to break and releases all the stored energy. The 400 years of energy accumulation at 15 mm per year could result in a devastating magnitude 9 earthquake, similar in size to the Japanese quake that destroyed huge sections of the country’s northeastern coast in 2011. Such an event would have enormous consequences for more than 140 million people living within 100 km of the megathrust in Bangladesh and India.
The tectonic activity of south Asia is a consequence of the collision of the Indian subcontinent with Asia, a process that began nearly 50 million years ago and is still occurring today. This monumental collision resulted in the uplifting of Tibet and the formation of the Himalayan mountain range. Over millions of years these mountains have been slowly eroded and deposited their rich soils onto the Bangladeshi plains by a network of giant rivers. The thick sediments have made the Bangladeshi plains some of the most agriculturally productive in the world.
While the sediments can take up some of the energy along the newly proposed fault, they’re not especially stable, particularly around the rapidly developed eastern outskirts of Dhaka. If a major earthquake strikes, the sediments could even amplify the seismic waves, causing further destruction.
“Dhaka’s basically like building a city on a bowl of Jell-O [jelly],” says Steckler, lead author of the new study, implying that even small earthquake shaking could be amplified by the sediments.
The Savar building collapse in 2013, which resulted in over 1100 deaths, showed the world that building codes in Bangladesh are not strictly enforced. If buildings are collapsing on their own, it is a terrifying prospect to consider what would happen during an earthquake. The lack of preparedness is clear and it is essential for the Bangladeshi government to make long-term changes to promote greater seismic awareness and stricter enforcement of building codes.
 The original paper: http://www.nature.com/ngeo/journal/vaop/ncurrent/full/ngeo2760.html
by Camilla Watson
An earthquake of magnitude 7.8 occurred in Ecuador on the 16th April this year. With the current death toll at 654 and another 58 still missing, this is one of the most devastating disasters South America has seen in modern times. Although the earthquake epicentre was in a relatively sparsely populated area, according to the US Geological Survey the focus was shallow at 19.2km (12 miles) and located 27km (17 miles) from Muisne off the west coast of northern Ecuador, meaning the effects were stronger than expected upon the Earth’s surface.
The main initiator of earthquakes is tectonic plate movement. This particular earthquake was caused by a shallow thrust fault on or near the boundary between the Nazca and South American tectonic plates (USGS, 2016). In real terms, this means the Nazca plate is sliding beneath the South American plate, and the build-up of energy due to friction is realised in one sudden slip, causing the earthquake and its aftershocks (Wald, 2009). Similar systems have caused some of the strongest earthquakes in the world, including the 1960 Chile earthquake of magnitude 9.5 – the largest ever recorded. Due to the presence of the subduction zone, this particular area within Ecuador is known to be prone to earthquakes, with many of the quakes occurring at 0-70km depths beneath the Earth’s surface. This often causes the consequences to be more devastating. The subduction system is also responsible for the formation of the Andes, the longest mountain chain in the world, and the high levels of volcanism within the area (USGS, 2016).
Scientists have been speculating as to whether the 2016 Ecuador earthquake was linked to the magnitude 7.0 Japan earthquake that occurred the day before, on the 15th April, with a shallow focus at 10km depth (Byrd, 2016). The idea behind this is something known as ‘remote triggering’, whereby a magnitude 6.5 earthquake in Japan would have caused slip along the boundaries of the tectonic plates on the other side of the Pacific Ocean, which triggered the tremors that made up the earthquake (Brown, 2016). However, this may also be chance due to both localities being situated on the Ring of Fire, an area known to be extremely tectonically active. Research so far shows no evidence for remotely triggered earthquakes to reach magnitudes above 5, making this particular situation between Ecuador and Japan either the first recorded case of its kind, or a coincidence. However, there has not yet been enough time for thorough research, but many earth scientists will now be focusing on the possibilities of using this information to help us to forecast and prepare for earthquakes in the future.
 D. Byrd, (2016), Powerful earthquakes in Japan and Ecuador, EarthSky, [Online], Accessed 25/04/2016: http://earthsky.org/earth/powerful-earthquakes-japan-ecuador-april-2016
 E.K. Brown, (2016), Are the Japanese and Ecuador earthquakes related?, The Conversation, [Online], Accessed 25/04/2016: http://phys.org/news/2016-04-japanese-ecuador-earthquakes.html
 Fox News, (2016), Death toll in the powerful Ecuador Earthquake rises to 654, Fox News, [Online], Accessed 25/04/2016: http://www.foxnews.com/world/2016/04/24/death-toll-in-powerful-ecuador-earthquake-rises-to-654.html
 L. Wald (2009), The Science of Earthquakes, The Green Frog News, USGS, [Online], Accessed 25/04/2016: http://earthquake.usgs.gov/learn/kids/eqscience.php
 USGS, (2016), M7.8 – 27km SSE of Muisne, Ecaudor, United States Geological Survey (USGS), [Online], Accessed 25/04/2016: http://earthquake.usgs.gov/earthquakes/eventpage/us20005j32#general
Camilla is a 3rd year undergraduate student in the School of Earth and Environment at the University of Leeds. She likes to combine her passion for travel with her love of geology. Check out her blog at: www.geologyandme.weebly.com
Istanbul is an ancient and beautiful city with a long history at the centre of major empires including the Roman, Byzantine, Latin and Ottoman. It is a city inundated with rich culture and history. In 2010 it was named a European Capital of Culture, which helped make it the world’s tenth most popular tourist destination. Home to over 11 million people, it is also one of the most populated cities in the world.
But this thriving and seemingly indestructible metropolis sits on a loaded spring: The North Anatolian Fault. The most active and earthquake prone fault system in Turkey, and the source of the 1999 magnitude 7.4 earthquake that killed nearly 18,00 people in the city of Izmit.
The North Anatolian Fault is about 1300km long running along the entire length of northern Turkey, from the Aegean Sea in the west to Lake Van in eastern Turkey.
Curiously, large earthquakes on the fault have tended to follow a successive sequence, i.e. an earthquake will often occur on the section of the fault adjacent to the last rupture. The current sequence started in 1939 with the magnitude 7.9 Erzincan earthquake, which killed over 30,000 people, and has been progressing to the west in a series of 8 large events.
Researchers in 1997 used this observation to successfully predict the location of the 1999 Izmit earthquake (if not the exact time). Worryingly the Izmit earthquake ruptured less than 100km to the east of Istanbul. Further work has led other researchers to predict a major earthquake, possibly another large magnitude 7.4, in the Istanbul region within the next 20 years!
So what can we do? Firstly, we need to better understand the science behind the cause of earthquakes in this region. The FaultLab project based at the University of Leeds involves research on the the ground movements around the North Anatolian Fault during various stages of the earthquake cycle. A greater understanding of the fault system can be used in forecasting models to give a better idea of the seismic risk.
Secondly, more engineering work needs to be done to reinforce vulnerable buildings that would collapse in the event of ground shaking. In May 2012 the Turkish government passed a new Urban Transformation Law requiring all buildings that do not conform to current earthquake hazard and risk criteria to be demolished.
This effectively means nearly 6 million buildings throughout Turkey will be demolished over the next two decades! This massive project is expected to generate over USD 500 billion worth of construction industry over the next decade.
A new rail line that runs beneath the Bosphorus Straits and links the east and western parts of the city will be able to withstand shaking from a magnitude 9 earthquake.
The new airport terminal for the Sabiha Gokcen international airport that serves the city of Istanbul has also been built to withstand shaking from a magnitude 8 earthquake and importantly, remain operational afterwards. This is critical, as when a disaster does strike the airport will be one of the main entry points for international relief and aid.
But the key question is: will Turkey and Istanbul in particular be able to finish all its ambitious redevelopment plans before the next major earthquake?
I certainly hope so!
 Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering, 1997, Geophysical Journal International, v 128, pp 594-604
 Parsons, T., Shinji, T., Stein, R. S., Barka, A. A., Dietrich, J. H.; Heightened Odds of Large Earthquakes Near Istanbul: An Interaction-Based Probability Calculation, 2000, Science, v 288, pp 661-665
Lying on the floodplains of the mighty Ganges, Brahmaputra and Meghna rivers Bangladesh is a rich, fertile land. These giant river systems meet in the centre of the country and flow together into the Bay of Bengal which, at over 1600km wide, is the largest delta in the world.
Rising Sea Level
Bangladesh is often cited as one of the countries that will be most negatively affected by rising sea levels from human induced climate change. Two thirds of the country lies less than 5m above of sea level. With vast regions to the south much less than a 1m above sea level. The Intergovernmental Panel on Climate Change (IPCC) claims that just 1m rise in sea level could directly expose nearly 14 million people and result in potentially 17% land loss in southern Bangladesh.
Most of the country receives on average more than 2.5m of rainfall a year, 80% of which falls in about 4 months during the peak monsoon season, resulting in large annual floods. The flood waters bring nutrient rich clays and silts from the high Himalayas and deposit them on the river floodplains. These rich soils produce bountiful harvests of rice and other crops. Unsurprisingly, farming is the most common profession.
However floods, once welcomed by farmers and their families are now harbingers of disaster. Human induced climate change has resulted in more erratic monsoon weather patterns with often larger than normal volumes of water being delivered in shorter time intervals. The resulting floods have had devastating effects on the Bangladeshi people. In 2012 three large floods hit the country in swift succession between the months of July and September directly affecting more than 5 million people. These are now a common annual occurrence.
Bangladesh is also subject to annual tropical cyclones, storm surges and tornadoes. Some of the worst natural disasters in recorded history were results of cyclonic storms in the Bengal region. Among them, the 1970 Bhola cyclone which claimed over 500,000 lives! Worryingly new research into the impacts of climate change has shown that large cyclonic storms will become a more common occurrence in the years and decades to come.
The foothills of the great Himalayan mountain belt has historically been the location of many large earthquakes. Earthquakes in the continent tend to be more infrequent compared to regions such as Japan and California. However this makes them more unpredictable and often unexpected. But when one does occur it can result in significant ground shaking. The 1897 magnitude 8.1 and 1950 magnitude 8.7 Assam earthquakes were two of the biggest to hit the region in recent times. The current building stock in Bangladesh is poorly built and most are not built to withstand ground shaking in an earthquake. The collapse of poorly built buildings is the greatest hazard during an earthquake.
So what can we as earth scientists do?
Bangladesh has a population of over 160 million and among the highest population density of any country in the world. With the majority of the country built on river floodplains combined with widespread corruption and ignorance a large earthquake could quite possibly result in the greatest natural calamity to have ever hit the country!
Bangladesh needs to increase its resilience if its people are to survive the multitude of natural hazards they face. Earth scientists are well placed to understand the risks involved from these hazards and can play a key role in all aspects of building a resilient infrastructure.
Climate science research is ongoing and needs to continue to better understand the affect human induced climate is having and will have on the annual monsoon. This knowledge needs to be translated into rainfall variation and flooding potentials and communicated with the people who need this information. The socio-economic issues of a rising sea level needs to be addressed and plans put in place to allow big cities to efficiently absorb and cater for migrants moving away from hazard prone coastal regions. Hydro-geologists and geochemists are helping to find sustainable clean, arsenic free water sources for drinking and farming. Seismologists and earthquake scientists are working to better understand the seismic risk in the Himalayan foothills; produce more accurate hazard maps and importantly identify the active faults within the region.
These are to name but a few of the ways earth scientists can get involved. I believe it is our moral duty to translate the practical aspects of our science into real benefits for people.
North Korea’s nuclear test today created a magnitude 5.1 earthquake equivalent seismic signal and has been measured on seismographs around the world.
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