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Three Pagodas Fault

Three Pagodas Fault 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 Three Pagodas Fault rather than just read about it. In short: The Three Pagodas Fault is a right-lateral displacement strike-slip fault between Burma and Thailand named after the Three Pagodas Pass. It developed as a consequence of the collision between the Indian and the Eurasian Plate.

Three Pagodas Fault — main illustration
Three Pagodas Fault — illustration

Key takeaways

  • Three Pagodas Fault 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 Three Pagodas Fault to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Three Pagodas Fault from memory before moving on to harder problems.

Reference excerpt

The Three Pagodas Fault is a right-lateral displacement strike-slip fault between Burma and Thailand named after the Three Pagodas Pass. It developed as a consequence of the collision between the Indian and the Eurasian Plate. The Three Pagodas Fault Zone (TPFZ) is a roughly 50 km wide zone separating the westernmost range of the Tenasserim Hills from the Tenasserim coast in Myanmar. The whole area is marked by a great number of fault traces and homoclinal ridges of Paleozoic limestone. The Three Pagodas Fault Zone accommodates the southeastward extrusion of Indochina, with stresses twisting clockwise. Together with the Wang Chao Fault and the Mae Ping Fault, it runs parallel to the Red River Fault. There is a fear that a future earthquake caused by the TPFZ and the Sri Sawat Fault Zone (SSFZ) could damage the large dams in Kanchanaburi Province in the future and that it could cause widespread damage to Bangkok. There was already a severe earthquake in the area about 2,500 years ago.

References

External links Recent paleoseismic investigations in Northern and Western Thailand Quake risk 'high' in Plains - Bangkok Post 25/12/2010

Illustrations

Three Pagodas Fault: Map of the tectonic setting of the 2004 Indian Ocean earthquake showing the fault lines across the Tenasserim Hills
Map of the tectonic setting of the 2004 Indian Ocean earthquake showing the fault lines across the Tenasserim Hills

Worked examples

Example 1 — a first encounter with Three Pagodas Fault

Start with the simplest possible case. Write down what Three Pagodas Fault 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 Three Pagodas Fault 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 Three Pagodas Fault 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 Three Pagodas Fault

In research
Three Pagodas Fault 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 Three Pagodas Fault 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
Three Pagodas Fault is common in secondary-school and first-year university syllabi. It links to neighbouring topics Geology of Myanmar, Geology of Thailand, Seismic faults of Southeast Asia, so understanding it makes those chapters shorter.
In everyday life
Look for Three Pagodas Fault 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 Three Pagodas Fault in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Three Pagodas Fault 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 Three Pagodas Fault out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Three Pagodas Fault in simple terms?

The Three Pagodas Fault is a right-lateral displacement strike-slip fault between Burma and Thailand named after the Three Pagodas Pass. It developed as a consequence of the collision between the Indian and the Eurasian Plate.

Why does Three Pagodas Fault 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 Three Pagodas Fault?

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 Three Pagodas Fault.

Tags

  • Geology of Myanmar
  • Geology of Thailand
  • Seismic faults of Southeast Asia
  • Strike-slip faults
  • Structural geology stubs
  • Tenasserim Hills

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