2011 Japanese tsunami Flashcards

1
Q

what was the magnitude of the earthquake

A

9.1

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2
Q

what was the date that the earthquake hit

A

March 11, 2011

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3
Q

where did the earthquake hit

A

off the northwest coast of Honshu on the japan trench.

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4
Q

how long did the earthquake last for

A

6 minutes

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5
Q

how long did it take for the tsunami to arrive at the coast

A

30 minutes

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6
Q

how many tsunami occur in the pacific ocean

A

90%

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7
Q

how rare was the 2011 tsunami

A

a one in a thousand year chance

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8
Q

where do most earthquakes occur in relation to japan

A

eastern part of Hokkaido, as well as the Pacific side of the Kanto region, Tokai region and Kinki and Shikoku regions.

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9
Q

what was the spatial impact of the tsunami

A

561 km2 along the Pacific coast of Japan

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10
Q

what is the area around the pacific where earthquakes and tsunami are always occurring

A

the ring of fire

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11
Q

what caused the 2011 tsunami

A

The Tohoku earthquake and tsunami were caused by centuries of build-up stress that was released in the convergent tectonic plate margin between the Pacific and the Eurasian plates. This is a common cause of earthquakes as the Pacific tectonic plate is being subducted below the Eurasian plate.

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12
Q

how far did the plant slip

A

50 metres

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13
Q

what did the government call the tsunami

A

the great east Japan earthquake

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14
Q

what were the Environmental impacts

A

The environmental impacts of the Tohoku earthquake and tsunami include

  1. contamination of groundwater (as the saltwater and pollution from the ocean infiltrate the ground due to the tsunami)
  2. removal of silt from coastal waterways due to the force of the tsunami
  3. and destruction of coastal ecosystems.

Further indirect impacts include the environmental toll of reconstruction. The earthquake also caused some beachfronts to drop by 0.5m, generating landfalls in the coastal areas.

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15
Q

what were the economic impacts

A

The economic impact of the earthquake and tsunami has been estimated to cost £159 billion, the most expensive disaster to date.

The earthquake and tsunami destroyed most of the infrastructure (ports, factories, businesses, and transportation systems) in the worst affected areas and they had to implement a ten-year recovery plan.

Moreover, 1046 buildings in Tokyo were damaged due to liquefaction (the loss of strength in soil due to the movement of earthquakes). The tsunami caused three nuclear power meltdowns, which have caused long-term challenges for recovery as high levels of radiation remain. TEPCO, the Tokyo Electric Power Company, announced that a full recovery of the plants can take 30 to 40 years. Finally, the Japanese government monitors food safety to ensure that they are within the safe limits of radiation content.

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16
Q

what were the social impacts

A

The social impacts of the earthquake and tsunami include:
• 15,899 people dead.
• 2527 missing and now presumed dead.
• 6157 injured.
• 450,000 lost their homes.
The unfortunate events caused other long-term consequences:
• 50,000 people were still living in temporary homes by 2017.
• 2083 children of all ages lost their parents.

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17
Q

how did activities of people intensify the impacts of the hazard

A

towns that were low lining in relation to sea level and had large amounts of agriculture and farming-based property, meaning that the landscape was very flat and had no natural protection in terms of trees, bushes, mangroves, and other natural features that act as barricades.

The Fukushima nuclear power plant was built right on the edge of the ocean, this put it in danger of tsunamis and other natural hazards. Therefore, when a 9.1 magnitude earthquake struck Japan, it caused a 15-meter tsunami as well. The water overwhelmed the defensive sea wall, flooding the plant and knocking out the emergency generators. This disabled the power supply and the cooling of three Fukushima Daiichi reactors, causing a nuclear accident beginning on 11 March 2011.

Authorities set up an exclusion zone which grew larger and larger as radiation leaked from the plant, forcing more than 150,000 people to evacuate from the area. There were no deaths immediately during the nuclear disaster. At least 16 workers were injured in the explosions, while dozens more were exposed to radiation as they worked to cool the reactors and stabilise the plant.

18
Q

explain one type of hazard risk management (tsunami gates)

A

The use of tsunami gates can be seen to be a very effective way to prevent the effects of a tsunami.

The basic idea behind using Tsunami gates is that you can have the gate opening during the normal time, and then, when need be, you are able to shut it which will block the water out. Tsunami gates can therefore extremely be useful for tsunamis that don’t have a high height as they will be able to completely block out this water.

However, once the tsunami gets too big then the water behind the tsunami gets more powerful and tsunami gates are unable to stop it.

Another important issue raised by the 2011 tsunami is that many firemen were lost in the call of duty as they closed many tsunami gates and the gates of seawalls

19
Q

explain one type of hazard risk management
(control forest)

A

A control forest is a popular method that is used all around the world to try and limit the amount of damage that a tsunami causes.

The role of the control forest is to provide coastal protection against the actions of waves, wind, and water currents in general.

The extent to which a controlled forest contributes to saving lives against large tsunamis depends on several factors including the height and velocity of the tsunami, the topography and orientation of the coastline, the width of the forest, and - to a lesser extent - the height, density, and species composition of the forest.

A control forest can be made from many sorts of plants, but mangroves often seem to work the best. The use of a controlled forest has both positives and negatives and is clear that with more work and planning the use of a controlled forest can be a great countermeasure for the future.

20
Q

explain an example of the hazard risk management being used (tsunami gates)

A

For example, we can see just how useful this tsunami countermeasure was in the 2011 tsunami.

Fudai used tsunami gates and the results were extremely positive. The water at Fudai was around 17 m and flowed over the gate but only went a few hundred meters past the gate. Most of Fudai village, including the evacuation shelters (primary and secondary schools), were protected, and no loss of human life was reported.

If there had not been a tsunami gate, the tsunami would have damaged the center of the village and caused a huge amount of damage to the town.

21
Q

explain an example of the hazard risk management being used (control forest)

A

The control forest in Ishinomaki did a good job of preventing large amounts of harm to the city. All the trees in Ishinomaki survived.

The forest reduced the destructive power of the tsunami and trapped debris, for example, cars, from the water before it entered the city. The trees may have been saved because the height of the tsunami at Ishinomaki was lower (6 m. Without control forests, it is predicted that a 16 m high tsunami would have overrun 600 m in 18 min with an average velocity of 10 m/s.

However, with the control forest, the tsunami arrival time was delayed by 6 min, and its velocity was reduced to 2 m/s. from this, it is clear that control forests work but in general, control forests can withstand tsunamis up to 3–5 m high.

22
Q

spell the city that implemented tsunami gates

23
Q

how tall was the tsunami wave at the city that implemented tsunami gates

24
Q

spell the town called that implemented control forest

A

Ishinomaki

25
how tall was the tsunami at Ishinomaki
6 metres
26
what was the prediction of the tsunami
that a 16 m high tsunami would have overrun 600 m in 18 min
27
what was the average velocity of the tsunami
average velocity of 10 m/s.
28
what height can control forest withstand
3-5 metres
29
how long was the tsunami arrive time delayed for
6 minutes
30
what was the tsunami velocity reduced to
2m/s
31
describe p waves
these are a form of body waves and are detected by a seismograph p wave = primary wave they travel with a great deal of speed
32
describe S waves
they are a type of body waves s waves= secondary wave although s waves are slower they can be more destructive particular in the case of shallow earthquakes
33
descibe love waves
named after the mathematician A.E.H love they are the fastest surface wave and move the earth side to side in a horizontal movement
34
describe Rayleigh waves
they cause most of the shaking that is felt the waves move the ground in an up and down and side to side direction and can be much longer than the other waves
35
where was the epicentre of the earthquake located
the earthquake had an epicenter in the Pacific Ocean, 72 km east of the Oshika Peninsula
36
where are convection currents located
in the earths mantle
37
describe what convection currents are
they are heated mantle material that is shown rising from deep inside the mantle, while cooler mantle material sinks, creating a convection current
38
what are convection currents thought to be responsible for
it is thought this type of current is responsible for the movements of the plates of earths crust.
39
what is the name of a sea side town
sendai
40
what was the name of the city that has a nuclear power plant
Fukushima