Central Pangean Mountains

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by 213.106.152.139 (talk) at 23:30, 24 March 2015 (Added Ben Nevis in the Scottish Islands as part of the remnants of the range.). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Map of Pangaea, including the 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 and Alleghenian orogenies.

References