continental drift

Tectonic plate movement

Continental drift is the theory that Earth's continents have slowly moved across the planet's surface over geological time.

First proposed in the early twentieth century, the idea explained why coastlines of different continents seem to fit together like puzzle pieces and why similar fossils appear on widely separated landmasses.

Continental drift was initially dismissed but later confirmed and incorporated into the broader theory of plate tectonics.

supercontinents

Pangaea

Prehistoric unified landmass

  • GondwanaAncient southern supercontinent
  • TethysGreek sea titaness
  • breakupRomantic relationship's termination

assembly · dispersal · Columbia · landmass · paleogeography · amalgamation · fragmentation · reconfiguration

theory

plate tectonics

Earth's crust mobility theory

isostasy · scientific controversy · paradigm shift · geological history

mechanism

tectonic plates

Mobile crustal sections

mid-ocean ridge · convection currents · plate boundaries · hotspot

geological

earthquakes

Sudden ground movement

oceanic trench · orogeny · rifting · seismic activity · volcanic arc · island chain · geological time · Mesozoic · Paleozoic · Triassic

evidence

rock strata

Layered geological deposits

Categories
Opposites
scale of geological motion

continental driftvolcanic activity

Geological heat release

subsidence

Family

drift, drifting, continent, continents, continental, intercontinental

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