Biology & life sciences · 09 / 12

Plate tectonics: read the evidence

High school · intermediate · Worked example and 4 exercises with solutions, at your pace.

The principle, simply

Lithospheric plates move relative to their neighbours. Divergent boundaries separate plates and create oceanic lithosphere at ridges. Convergent boundaries may involve subduction; transform boundaries slide past each other. Earthquakes, volcanism, seafloor ages and geodetic measurements provide complementary evidence.

THE PICTURE TO REMEMBERPlate tectonics: read the evidence
Simplified divergent boundary: rocks become older away from the axis on both sides. Arrows show relative plate separation.RidgeOlder ← young → older

Simplified divergent boundary: rocks become older away from the axis on both sides. Arrows show relative plate separation.

  1. 01Locate evidence
  2. 02Compare ages
  3. 03Draw a cross-section
  4. 04Explain movement

WORKED EXAMPLE

From principle to reasoning

At a ridge, rocks are youngest near the axis and become older away from it on both sides. Symmetrical magnetic bands provide further evidence of spreading.

Solve a problem in this subject

  1. Frame a question

    State the relationship to explain and its scale: molecule, cell, organism, population or geological time.

  2. Describe evidence

    Give a measurable observation, unit, comparison and conditions before explaining it. Observation and inference do different jobs.

  3. Connect a mechanism

    Use a precise concept and label arrows as production, transfer, action or transformation. Sequence alone does not prove causation.

  4. Answer with a limit

    Connect evidence and knowledge to the question. Distinguish the simplified model from living systems and identify a missing condition.

YOUR TURN

01 · Try before checking

Why can earthquakes deepening towards a continent suggest subduction?

One hint

Draw earthquake foci in cross-section, not only on a map.

Reveal and understand the solution

Foci may trace an inclined plane where an oceanic plate descends beneath another. Compare this with relief, volcanism and other observations.

Compare method, conditions and answer; identify the exact part to revisit.

IMPROVE THROUGH PRACTICE

Three additional challenges with solutions

Start with the first challenge. Write your method before opening a hint; use the solution to find the first step that needs work.

Reflect after practising
02 · Recognise and understandLink to this exercise

Do plates converge or diverge at an ocean ridge?

A hint to get started

Connect lithosphere formation to motion.

Step-by-step solution
  1. They move apart: divergence.
  2. Hot material rises and oceanic lithosphere forms.
  3. A ridge is not a subduction zone.

Which step did you miss? Retry without help, then explain why the method works.

03 · Apply the methodLink to this exercise

Seafloor age increases away from both sides of a ridge. What does this support?

A hint to get started

Compare a spreading prediction with observations.

Step-by-step solution
  1. The youngest lithosphere is near the ridge.
  2. Greater distance corresponds to greater age.
  3. This supports seafloor spreading, alongside other evidence.

Which step did you miss? Retry without help, then explain why the method works.

04 · Go furtherLink to this exercise

Why do some ocean trenches have deep earthquakes nearby?

A hint to get started

One plate descends beneath another.

Step-by-step solution
  1. In subduction, oceanic lithosphere sinks.
  2. Earthquake foci outline an inclined zone associated with the slab.
  3. Their depths help infer slab geometry.

Which step did you miss? Retry without help, then explain why the method works.

The trap to avoid

Plates are not merely continents; many include both continental and oceanic lithosphere.

Without notes, can you…

  • Explain the principle in your own words?
  • Rebuild the diagram and its connections?
  • Solve the exercise and justify the method?

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