Laurentia, also called the North American craton, is the ancient continental core of North America. It first assembled around 2.0 to 1.8 billion years ago from a group of Archean crustal fragments, including the Slave, Rae-Hearne, Superior, Wyoming and Nain cratons, welded together along the Trans-Hudson orogenic belt. It contains some of Earth's oldest known rock, the Acasta Gneiss, dated to 4.04 billion years. In Canada the craton is exposed at the surface as the Canadian Shield, while across much of the United States it lies buried beneath younger sedimentary rock. Laurentia has repeatedly been part of larger supercontinents, including Rodinia and Pangaea, before emerging again as the stable core of the modern North American continent. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
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Wikidata P31 formation-type mapped to formative process Plate Tectonics via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Laurentia
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Wikidata P31 formation-type mapped to discipline Structural Geology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Laurentia
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Source Wikidata: Laurentia
Also in Geography Atlas: where this subject is found.
Source Wikidata: Laurentia
Sources
Laurentia (Wikipedia)
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Laurentia or the North American craton is a large continental craton that forms the ancient geological core of North America.
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Wikidata Q858071, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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