Continental drift — Science definition

Alfred Wegener's idea that continents were once joined together and have since slowly moved to their current positions.

Where it is taught

In use

That idea — continents wandering across the globe over vast stretches of time — became known as continental drift.

Evidence for Continental Drift

Questions using continental drift

Problem 1

Who proposed the idea of continental drift in 1912?
  1. Isaac Newton
  2. Alfred Wegener
  3. Charles Darwin
  4. Albert Einstein
Answer and explanation

Alfred Wegener

Alfred Wegener proposed continental drift in 1912, based on evidence like matching coastlines and fossils.

Problem 2

Which piece of evidence did Wegener use to support continental drift?
  1. Matching fossils of the same species on continents now separated by oceans
  2. Modern GPS measurements of plate motion
  3. Satellite photographs of Earth
  4. Identical languages spoken on separated continents
Answer and explanation

Matching fossils of the same species on continents now separated by oceans

GPS and satellites didn't exist in 1912 — Wegener relied on evidence like matching fossils, rock layers, coastlines, and climate clues.

Problem 3

Why was Wegener's continental drift hypothesis rejected by most scientists for decades?
Answer and explanation

Wegener could not explain a physical mechanism for how huge, solid continents could move or plow through solid ocean floor, so most scientists didn't accept the idea until seafloor spreading was discovered in the 1960s.

Problem 4

What discovery in the 1960s finally gave continental drift a believable mechanism?
  1. The invention of the seismograph
  2. Seafloor spreading and paleomagnetic stripes on the ocean floor
  3. The discovery of Mesosaurus fossils
  4. Wegener's original 1912 publication
Answer and explanation

Seafloor spreading and paleomagnetic stripes on the ocean floor

Seafloor spreading, confirmed by symmetric paleomagnetic stripes recorded in ocean-floor rock, finally explained how continents could move — giving plate tectonics its mechanism.

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