词条 | Central Pangean Mountains |
释义 |
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. References1. ^Europe - Forces That Made Europe, The Mediterranean Desert - Miscellaneous regions and events {{clr}}{{Triassic Footer}}{{Major African geological formations}}{{-}}{{Palaeo-geo-stub}}{{Triassic-stub}} 9 : Mountain ranges of Africa|Mountain ranges of Europe|Mountain ranges of North America|Triassic paleogeography|Triassic Africa|Triassic Europe|Triassic United States|Appalachian Mountains|Atlas Mountains |
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