The Mechanism of Supercontinent Assembly and Breakup
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The Wilson Cycle: Plate Tectonics and Supercontinent Formation
The Wilson Cycle, named after geologist John Tuzo Wilson, describes the cyclical process of integrating the pace of geological time and the merging and breaking apart of tectonic plates and continents.
Initiation of the Cycle: Continental Breakup
The Wilson Cycle begins with the breakup of a continent, typically due to the action of a hot spot. This hot spot forms beneath the continent, often attributed to poor 'ventilation' (heat dissipation) in the underlying mantle. This focused heat produces thinning and fracturing of the lithosphere.
A rift then appears, which will evolve into an ocean basin. The floor of this ocean is formed by parallel bands of basalt that reflect Earth's magnetic... Continue reading "The Mechanism of Supercontinent Assembly and Breakup" »