Central Pangean Mountains
The Central Pangean Mountains were an extensive northeast-southwest trending mountain range in the central portion of the supercontinent Pangaea during the Triassic period. They were formed as a result of collision between the minor supercontinents Laurussia and Gondwana during the formation of Pangaea.[1] Remnants of this massive mountain range include the Appalachian Mountains of North America, the Little Atlas of Morocco, Africa and much of the Scottish Highlands including Ben Nevis.
A number of mountain building periods were involved in the formation of the Central Pangean Mountains, including the Acadian, Caledonian, Alleghenian and Mauritanide orogenies.
References
Triassic Period | ||
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Lower/Early Triassic | Middle Triassic | Upper/Late Triassic |
Induan |Olenekian | Anisian | Ladinian | Carnian | Norian Rhaetian |
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