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- Orogeny refers to the process of mountain building. Examples of orogenies include12:
- Alleghenian (Appalachian), Laramide, and Andean orogenies in the Americas.
- Algoman, Penokean and Antler orogenies, which are older and inactive, and are represented by deformed and metamorphosed rocks with sedimentary basins further inland.
- Pan-African orogeny, Damara orogeny, Kibaran orogeny, and Eburnean orogeny in Africa.
- Cordilleran system and the Tethyan system, which are orogenic systems that appear as loosely coherent clusters or stringers of orogenic belts that are at least 20,000 km long and 100–1000 km wide.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Large modern orogenies often lie on the margins of present-day continents; the Alleghenian (Appalachian), Laramide, and Andean orogenies exemplify this in the Americas. Older inactive orogenies, such as the Algoman, Penokean and Antler, are represented by deformed and metamorphosed rocks with sedimentary basins further inland.
en.wikipedia.org/wiki/OrogenyAfrican orogenies [ edit]
- Pan-African orogeny – Series of major mountain-forming events, Neoproterozoic Era (550 Ma)
- Damara orogeny – Mountain building event at the intersection of the Congo and the Kalahari cratons.
en.wikipedia.org/wiki/List_of_orogenies - People also ask
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