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Colliding Plates Raise Mountains

Two thick slabs of continental crust push into each other. The rock between them folds upward and thickens, building high mountain chains over millions of years.

In the picture

  1. A thick continental plate: one of the two landmasses pushing inward.
  2. The opposing continental plate: the second landmass pushing from the other side.
  3. Layered rock bands: strata bending upward where the plates meet.
  4. A sharp central peak: the highest part of the folded mountain chain.
  5. An hourglass: the millions of years needed for the mountains to rise.

Examples

  • The Himalayas rising as India pushes into Asia.
  • The Alps forming as Africa and Europe collide.

Quiz: Colliding Plates Raise Mountains (Age 15)

  1. What happens to the rock between two continental plates that push into each other?

    • It stays flat and unchanged.
    • It melts completely into magma.
    • It folds upward and thickens.
  2. According to the card, what can happen when continental plates collide?

    • They can stop all movement in the crust.
    • They can fold rock into high mountains.
    • They can turn the crust into ocean floor.
  3. How long does the card say mountain chains take to grow as the crust crumples and thickens?

    • Millions of years.
    • A few hundred years.
    • A single human lifetime.

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Geography, Age 15