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The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
WikiVisually
The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
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Rodinia
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In the geological history of Earth, Rodinia was a Mesoproterozoic and Neoproterozoic supercontinent that assembled 1.26–0.90 billion years ago and broke up 750–633 million years ago. Valentine & Moore
Reconstruction of Rodinia at 900 million years ago, using modern images to illustrate where today's recognisable continents were at the time.
Reconstruction of Rodinia at 900 million years ago, using modern images to illustrate where today's recognisable continents were at the time.
Iapetus Ocean
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The Iapetus Ocean existed in the late Neoproterozoic and early Paleozoic eras of the geologic timescale. It was in the Southern Hemisphere, between the paleocontinents of Laurentia, Baltica and Avalon
Reconstruction of how the Iapetus Ocean and surrounding continents might have been arranged during the late Ediacaran period
Reconstruction of how the Iapetus Ocean and surrounding continents might have been arranged during the late Ediacaran period
Geological fault at Niarbyl. The narrow white diagonal line near centre of picture is where the two sides of the Iapetus Ocean met during its closure.
Geological fault at Niarbyl. The narrow white diagonal line near centre of picture is where the two sides of the Iapetus Ocean met during its closure. Sutures such as these are the modern evidence for this ancient ocean.