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Tōkai earthquakes

Tōkai earthquakes is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Tōkai earthquakes rather than just read about it. In short: The Tōkai earthquakes (Japanese: 東海地震) are major earthquakes that have occurred regularly with a return period of 100 to 150 years in the Tōkai region of Japan. The Tōkai segment has been struck by earthquakes in 1498, 1605, 1707, and 1854.

Tōkai earthquakes — main illustration
Tōkai earthquakes — illustration

Key takeaways

  • Tōkai earthquakes belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Tōkai earthquakes to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Tōkai earthquakes from memory before moving on to harder problems.

Reference excerpt

The Tōkai earthquakes (Japanese: 東海地震) are major earthquakes that have occurred regularly with a return period of 100 to 150 years in the Tōkai region of Japan. The Tōkai segment has been struck by earthquakes in 1498, 1605, 1707, and 1854. Given the historic regularity of these earthquakes, Kiyoo Mogi in 1969 pointed out that another great shallow earthquake was possible in the "near future" (i.e., in the next few decades). Given the magnitude of the last two earthquakes, the next is expected to have at least a magnitude scale of 8.0 Mw, with large areas shaken at the highest level in the Japanese intensity scale, 7. Emergency planners are anticipating and preparing for potential scenarios after such an earthquake, including the possibility of thousands of deaths and hundreds of thousands of injuries, millions of damaged buildings, and cities that include Nagoya and Shizuoka devastated. Concern has been expressed over the presence of the Hamaoka Nuclear Power Plant, close to the expected epicentre of a Tōkai earthquake. The Fukushima I Nuclear Power Plant was severely damaged after a large earthquake followed by a tsunami in 2011, causing the Fukushima nuclear accident, which was a nuclear event of level 7, the highest on the scale. Shortly after the 2011 Tōhoku earthquake, new reports were released which indicated the significant likelihood of another magnitude 9 earthquake occurring elsewhere in Japan, this time on the Nankai Trough. The reports stated that if a 9.0 earthquake occurred on the Nankai Trough, the effects would be very serious. The quake itself would likely kill thousands, and a series of 34-meter (112-foot) tall tsunamis would impact areas from the Kantō region to Kyūshū, adding thousands to the death toll, and destroying Shizuoka, Shikoku, and other areas with large populations.

Earthquake prediction The Tokai Earthquake is expected to occur in the near future along the trench near Suruga Bay with a magnitude of around 8. The Tokai region will be subjected to extremely strong shaking with seismic intensity of 6-lower or greater, and huge tsunamis are expected to hit the Pacific coast in the region. The Japanese government is taking the Tōkai earthquakes seriously and has charged the Japan Meteorological Agency with predicting the next one. There is now a dense array of instruments placed to accumulate a continuous stream of data related to seismicity, strain, crustal expansion, tilt, tidal variations, ground water fluctuations and other variables. They are watching for an anomaly in this data which might precede the next major Tōkai earthquake. Following the prediction of an earthquake in the relatively near future, and in order to try to predict when it would occur, the Coordinating Committee for Earthquake Prediction (CCEP) designated the Tōkai region as an Area of Specific Observation in 1970, and upgraded it to an Area of Intensified Observation in 1974. Following the passing of the Large-Scale Earthquake Countermeasure Act (大規模地震対策特別措置法) in 1978, the Earthquake Assessment Committee (EAC) was set up to warn the Prime Minister, via the Japan Meteorological Agency, if the next quake is imminent.

As serious damage from strong shaking and huge tsunamis is expected, the Japanese government has designated this region as Areas under Intensified Measures against Earthquake Disaster. Information on future quakes is published irregularly. Since November 2017, this information limited to Tokai earthquakes has not been announced, and "Information on the Nankai megathrust earthquake (南海トラフ地震に関連する情報) " targeting the Nankai megathrust earthquakes has been in operation. Future Tokai earthquakes are expected to occur with the sequence of

strain accumulation, pre-slip and earthquake occurrence. JMA monitors unusual deformation that may accompany pre-slip using strainmeters to support the prediction of its occurrence. As pre-slip may be too slight to be detected by the observation systems currently in place, it is not possible to say that the Tokai Earthquake will be predicted without fail.

Prediction information To support predictions, JMA has developed a seismic and crustal deformation observation network covering the region in conjunction with related organizations, and observes related data around-the-clock basis. After monthly assessments, or when anomalous data are detected, JMA issues Information on the Tokai Earthquake bulletins to allow emergency measures for earthquake disaster prevention. These are categorized into three types: Investigation Report on Tokai Earthquake Prediction, Tokai Earthquake Watch, and Explanatory Information on Tokai Earthquake Warning. Each report indicates the level of danger using a color code of blue, yellow and red.

To determine whether anomalous phenomena are precursors to the Tokai Earthquake, JMA convenes the Earthquake Assessment Committee for Areas under Intensified Measures against Earthquake Disaster (地震防災対策強化地域判定会), which consists of seismologists and members of governmental organizations. If the Committee concludes that the Tokai Earthquake is imminent, the Director-General of JMA will report this conclusion to the Prime Minister, who will then hold a Cabinet meeting and issue a warning statement (警戒宣言).

Relation to other major earthquakes The pattern of historical seismicity reveals that the megathrust surface is segmented, with five separate zones of rupturing identified, conventionally labeled A–E, from west to east. Earthquakes involving the A+B segments are generally referred to as Nankai (literally South Sea) earthquakes, C+D Tōnankai (literally Southeast Sea) earthquakes and E Tōkai (literally East Sea) earthquakes. These earthquakes repeat at intervals generally in the range of 90 – 200 years. On all but one occasion, rupture of segment C (±D ±E) has been followed by rupture of segments A+B within a few years. This behavior has been reproduced by modeling the viscoelastic response of the megathrust fault plane with lateral variations in both convergence rate and frictional properties.

Historical Tōkai earthquakes

See also 1944 Tōnankai earthquake Coordinating Committee for Earthquake Prediction Kanto earthquakes List of earthquakes in Japan Nankai megathrust earthquakes

References

External links Tokai earthquake information from Japan Meteorological Agency Tokai earthquake preparedness in Shizuoka prefecture

Illustrations

Tōkai earthquakes: Anticipated area of the Tokai Earthquake
Anticipated area of the Tokai Earthquake
Tōkai earthquakes: Nankai, Tōnankai and Tōkai earthquake areas
Nankai, Tōnankai and Tōkai earthquake areas
Tōkai earthquakes: Areas under Intensified Measures against Earthquake Disaster (shown in yellow)
Areas under Intensified Measures against Earthquake Disaster (shown in yellow)

Worked examples

Example 1 — a first encounter with Tōkai earthquakes

Start with the simplest possible case. Write down what Tōkai earthquakes claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Tōkai earthquakes before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Tōkai earthquakes ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Tōkai earthquakes

In research
Tōkai earthquakes appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Tōkai earthquakes in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Tōkai earthquakes is common in secondary-school and first-year university syllabi. It links to neighbouring topics Earthquake clusters, swarms, and sequences, Megathrust earthquakes in Japan, so understanding it makes those chapters shorter.
In everyday life
Look for Tōkai earthquakes outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Tōkai earthquakes in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Tōkai earthquakes means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Tōkai earthquakes out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Tōkai earthquakes in simple terms?

The Tōkai earthquakes (Japanese: 東海地震) are major earthquakes that have occurred regularly with a return period of 100 to 150 years in the Tōkai region of Japan. The Tōkai segment has been struck by earthquakes in 1498, 1605, 1707, and 1854.

Why does Tōkai earthquakes matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Tōkai earthquakes?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Tōkai earthquakes.

Tags

  • Earthquake clusters, swarms, and sequences
  • Megathrust earthquakes in Japan

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