Plate Tectonics

Grade 8 · Science · Study Guide

Discover how Earth's tectonic plates move and the geological features their interactions create.

Earth's lithosphere is divided into about 15 major tectonic plates that move slowly over the asthenosphere at a rate of a few centimeters per year. This movement is driven by convection currents in the mantle and creates most of Earth's major geological features.

Plates interact at three types of boundaries: convergent (plates move toward each other, forming mountains or trenches), divergent (plates move apart, forming rift valleys or mid-ocean ridges), and transform (plates slide past each other horizontally, causing earthquakes like along the San Andreas Fault).

Alfred Wegener proposed the theory of continental drift in 1912, noting that continents fit together like puzzle pieces. Evidence includes matching fossils across continents, similar rock formations on different continents, and paleomagnetic striping on the ocean floor — all supporting the idea of one ancient supercontinent called Pangaea.

Types of Plate Boundaries
Boundary TypeMovementFeatures CreatedExample
ConvergentPlates move togetherMountains, trenches, volcanoesHimalayas, Mariana Trench
DivergentPlates move apartRift valleys, mid-ocean ridgesMid-Atlantic Ridge
TransformPlates slide past each otherEarthquakes, fault linesSan Andreas Fault
Evidence for Continental Drift
EvidenceExplanation
Puzzle-piece fit of continentsAfrica and South America shorelines match closely
Matching fossilsSame species found on continents now separated by oceans
Similar rock formationsIdentical rock layers across ocean-separated continents
Seafloor spreadingNew crust forms at mid-ocean ridges as plates diverge

Key terms

Tectonic Plate
A large section of Earth's lithosphere that moves slowly on the asthenosphere.
Convergent Boundary
Where two tectonic plates move toward each other; creates mountains or ocean trenches.
Divergent Boundary
Where two plates move apart; creates rift valleys or mid-ocean ridges.
Subduction
When a denser plate sinks beneath a less dense plate at a convergent boundary.

Practice questions

  1. At which type of plate boundary would you expect to find mid-ocean ridges?

    1. Convergent
    2. Transform
    3. Divergent
    4. Subduction
    Show answer

    At divergent boundaries, plates move apart and magma rises to fill the gap, creating new seafloor and mid-ocean ridges.

  2. The San Andreas Fault in California is an example of a ___ boundary.

    1. Convergent
    2. Divergent
    3. Transform
    4. Subduction
    Show answer

    The San Andreas Fault is where the Pacific and North American plates slide horizontally past each other — a transform boundary.

  3. Alfred Wegener's theory of continental drift was immediately accepted by the scientific community.

    Show answer

    Wegener's theory was largely rejected in his lifetime because he couldn't explain the mechanism. Seafloor spreading evidence in the 1960s finally confirmed it.

  4. When a denser oceanic plate sinks beneath a less dense plate at a convergent boundary, the process is called ___.

    Show answer

    Subduction creates deep ocean trenches and volcanic arcs on the overriding plate.

  5. Describe two pieces of evidence that support the theory that all continents were once joined as Pangaea.

    Show answer

    These multiple independent lines of evidence strongly support Wegener's continental drift theory.

Fun facts

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