ArticleslgStudy

earth science

Kekerengu Fault

Kekerengu 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 Kekerengu Fault rather than just read about it. In short: The Kekerengu Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It is closely associated with the Hope Fault and Jordan Thrust at its south-easternmost edge and likely joins with the Clarence Fault to form the Wairarapa Fault offshore in Cook Strait.

Kekerengu Fault — main illustration
Kekerengu Fault — illustration

Key takeaways

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

Reference excerpt

The Kekerengu Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It is closely associated with the Hope Fault and Jordan Thrust at its south-easternmost edge and likely joins with the Clarence Fault to form the Wairarapa Fault offshore in Cook Strait. Early investigations immediately following the 14 November 2016 Kaikōura earthquake indicated that up to 10 m (33 ft) of motion may have occurred on the Kekerengu Fault during the 7.8 magnitude quake. The maximum displacement was later found to be 12.0 m (39.4 ft) ± 0.7 m (2 ft 4 in). During this earthquake the offshore continuation of the Kekerengu Fault to the north east, known as the Needles Fault, ruptured as well. NIWA marine geologist Dr Philip Barnes said the length of the Kekerengu–Needles Fault rupture may extend for about 70 km (43 mi), consisting of 36 km (22 mi) on land and 34 km (21 mi) under the sea.

References

Illustrations

Kekerengu Fault: Satellite radar image showing ground motion effects during the 2016 Kaikōura earthquake
Satellite radar image showing ground motion effects during the 2016 Kaikōura earthquake
Kekerengu Fault: Map of the Marlborough Fault System
Map of the Marlborough Fault System

Worked examples

Example 1 — a first encounter with Kekerengu Fault

Start with the simplest possible case. Write down what Kekerengu 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 Kekerengu 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 Kekerengu 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 Kekerengu Fault

In research
Kekerengu 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 Kekerengu 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
Kekerengu Fault is common in secondary-school and first-year university syllabi. It links to neighbouring topics 2016 Kaikōura earthquake, Plate tectonics, Plate tectonics stubs, so understanding it makes those chapters shorter.
In everyday life
Look for Kekerengu 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.
Ask Teacher Smith questions about this articleOpens your AI tutor with a question about “Kekerengu Fault” →

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Kekerengu Fault in 20 minutes

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

Frequently asked questions

What is Kekerengu Fault in simple terms?

The Kekerengu Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It is closely associated with the Hope Fault and Jordan Thrust at its south-easternmost edge and likely joins with the Clarence Fault to form the Wairarapa Fault offshor…

Why does Kekerengu 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 Kekerengu 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 Kekerengu Fault.

Tags

  • 2016 Kaikōura earthquake
  • Plate tectonics
  • Plate tectonics stubs
  • Seismic faults of New Zealand
  • Strike-slip faults

Keep exploring