Pangaea
Pangaea was a geologically recent supercontinent that brought together nearly all of Earth's major landmasses. It was surrounded by the global ocean Panthalassa and assembled by the Early Permian, roughly 300 million years ago. Beginning about 200 million years ago, it gradually broke apart as tectonic plates moved, giving rise to the continents and ocean basins recognizable today. Evidence of matching continental margins and geological formations helped inform the theory of continental drift and, later, modern plate tectonics.
Formation and geography
Pangaea was the most recent supercontinent to incorporate almost all of Earth's major landmasses. Its assembly took place over geological time as continental fragments moved and collided. Britannica dates its completed assembly to the Early Permian, about 299–273 million years ago; the National Park Service describes the joined landmass as a snapshot from roughly 250 million years ago. Pangaea was surrounded by the vast ocean Panthalassa. A curved embayment on its eastern side formed the Tethys sea region. The exact outlines of land and sea changed over time, so reconstructions depict a sequence rather than one unchanging map.
Breakup and moving continents
Pangaea did not split apart in a single event. Rifting began roughly 200 million years ago, and the supercontinent fragmented in stages as parts of Earth's lithosphere moved apart. In one early rift system, separation among Africa, South America and North America helped open the Atlantic basin; later movements further divided the southern continents and opened other ocean basins. The U.S. Geological Survey describes how rifting and volcanic activity along the separating landmasses contributed to the growth of the Atlantic and the mid-Atlantic ridge. The process continues in the sense that Earth's tectonic plates are still moving, although the present-day continental arrangement developed over many millions of years.
Evidence and scientific significance
The idea that continents had once been joined gained support from their complementary shapes, especially the margins of South America and Africa, and from geological patterns found across now-separated regions. Alfred Wegener developed the concept of Pangaea as part of his continental-drift hypothesis in the early twentieth century. The idea was initially controversial because Wegener could not provide a convincing mechanism for continental motion. Plate tectonics later supplied a broader physical framework: Earth's outer shell is divided into plates that move relative to one another. Pangaea is one reconstructed episode in Earth's longer history of supercontinent assembly and breakup, not the only supercontinent that has existed.
Key facts
- Type
- A supercontinent incorporating almost all of Earth's major landmasses.
- Surrounding ocean
- Panthalassa.
- Assembly
- Complete by the Early Permian, approximately 299–273 million years ago; estimates are geological reconstructions.
- Breakup
- Began about 200 million years ago and proceeded in stages.
- Scientific context
- Pangaea figured in Alfred Wegener's continental-drift hypothesis and is now understood through plate tectonics.
Timeline
Early Permian, about 299–273 million years ago
Pangaea's assembly was complete, according to Britannica's geological chronology.
About 200 million years ago
The supercontinent began to break apart in stages during the Early Jurassic, as reconstructed from geological evidence.
1912
Alfred Wegener proposed Pangaea as part of his theory of continental drift.
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References
- 1.Pangea Definition, Map, History, & Facts
Encyclopaedia Britannica · other · reliability: high · retrieved 22 October 2026
Supports: Assembly and breakup chronology, geography, Panthalassa, Wegener's proposal and the relationship between continental drift and plate tectonics.
- 2.What was Pangea?
U.S. Geological Survey · other · reliability: high · retrieved 22 October 2026
Supports: Pangaea's existence, approximate time span, initial rifting, volcanic activity and the opening of the Atlantic basin.
- 3.Plate Tectonics—The Unifying Theory of Geology
National Park Service, U.S. Department of the Interior · other · reliability: high · retrieved 22 October 2026
Supports: Plate-tectonic framework, continental fit and the approximate 250-million-year-old configuration of Pangaea.
- 4.Historical perspective
U.S. Geological Survey · other · reliability: high · retrieved 22 October 2026
Supports: The breakup of Pangaea, continental drift and the development of modern plate-tectonic theory.
References are suggested by the research engine and may be incomplete. Unverified URLs are omitted rather than guessed.
Article history
- Version 122 October 2026 · EditorCreated by Zapia