supercontinents

Ancient combined landmasses

Supercontinents are landmasses comprising most or all of Earth's continental crust, formed when tectonic plates drift together over hundreds of millions of years.

Pangaea, which existed about 300 million years ago, is the most famous example.

The term also applies to earlier formations like Rodinia and Gondwana.

Geologists theorize that supercontinents assemble and break apart in cycles spanning roughly 500 million years.

geological

Pangaea

Prehistoric unified landmass

  • GondwanaAncient southern supercontinent
  • ColumbiaAmerica personified, or its namesakes
  • UrEarly Mesopotamian metropolis

plate tectonics · craton · landmass · rifting · breakup · assembly · cycle · paleogeography · reconstruction · shield

paleobiology

biogeography

Science of species distribution

fossil record · extinction · evolution · biodiversity · isolation · speciation · land bridges · fauna · flora · dinosaurs

paleoclimate

ice age

Era of massive glaciation

ocean currents · Tethys · monsoonal · paleoclimate · hothouse · icehouse · albedo · weathering · carbon cycle

evidence

glacial striations

Scratches carved by moving ice

stratigraphic

Categories
Opposites
landmass size/scale

supercontinentsislands

Land surrounded by water

archipelagos · islets · microcontinents · atolls · oceanic islands

land vs. water dominance

supercontinentsTethys Sea

Vanished equatorial ocean

deep sea

geological convergence vs. divergence

supercontinentscontinental drift

Gradual landmass repositioning

fragmentation · rift valleys

Family

supercontinent

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