Pangaea or Pangea is the name given to the supercontinent that existed during the Paleozoic and Mesozoic eras, before the process of plate tectonics separated each of the component continents into their current configuration.
The name was coined by Alfred Wegener, chief proponent of Continental Drift in 1915.
For more information about the topic Pangaea, read the full article at Wikipedia.org, or see the following related articles:
Gondwana The southern supercontinent Gondwana (originally Gondwanaland) included most of the landmasses which make up today's continents of the southern ... >
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Mesozoic The Mesozoic Era is one of three geologic eras of the Phanerozoic eon. The Mesozoic includes three geologic periods: from oldest to youngest, they ... >
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Crust (geology) In geology, a crust is the outermost layer of a planet.
The crust of the Earth is composed of a great variety of igneous, metamorphic, and ... >
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Paleozoic The Paleozoic Era is a major division of the geologic timescale, one of four geologic eras. The Paleozoic includes six geologic periods; from oldest ... >
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Geology of the Alps The Alps form a part of a Tertiary orogenic belt of mountain chains along the southern margin of the continents Asia and Europe, called the Alpide ... >
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Ocean Though generally recognized as several 'separate' oceans, these waters comprise one global, interconnected body of salt water often referred to as ... >
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Plate tectonics Plate tectonics is a theory of geology developed to explain the phenomenon of continental drift and is currently the theory accepted by the vast ... >
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Cenozoic The Cenozoic Era is the most recent of the four classic geological eras. The Cenozoic is divided into two periods, the Palaeogene and Neogene, and ... >
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Cretaceous The Cretaceous period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic period, about 146 million years ... >
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