EURAMERICA
'Euramerica' (also known as 'Laurussia' or 'Old Red Continent') was a minor supercontinent created in the Devonian as the result of a collision between the Laurentian and Baltica cratons (Caledonian orogeny).
Euramerica became a part of the major supercontinent Pangaea in the Permian. In the Jurassic, when Pangaea rifted into two continents, Gondwana and Laurasia, Euramerica was a part of Laurasia. In the Cretaceous, Laurasia split into the continents of North America and Eurasia. The Laurentian craton became a part of North America, while Baltica became a part of Eurasia.
★ Continental drift
★ Eurasia
★ Palaeos Earth: Geography: Euramerica
★ Paleogeographic globe of the Devonian Earth
Euramerica became a part of the major supercontinent Pangaea in the Permian. In the Jurassic, when Pangaea rifted into two continents, Gondwana and Laurasia, Euramerica was a part of Laurasia. In the Cretaceous, Laurasia split into the continents of North America and Eurasia. The Laurentian craton became a part of North America, while Baltica became a part of Eurasia.
| Contents |
| See also |
| External links |
See also
★ Continental drift
★ Eurasia
External links
★ Palaeos Earth: Geography: Euramerica
★ Paleogeographic globe of the Devonian Earth
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