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About: Trans-Hudson orogeny     Goto   Sponge   NotDistinct   Permalink

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Type: yago:WikicatCratonsyago:Craton109259500yago:Part109385911yago:PhysicalEntity100001930sports eventyago:Thing100002452 New Facet based on Instances of this Class

The Trans-Hudson orogeny or Trans-Hudsonian orogeny was the major mountain building event (orogeny) that formed the Precambrian Canadian Shield and the North American Craton (also called Laurentia), forging the initial North American continent. It gave rise to the Trans-Hudson orogen (THO), or Trans-Hudson Orogen Transect (THOT), (also referred to as the Trans-Hudsonian Suture Zone (THSZ) or Trans-Hudson suture) which is the largest Paleoproterozoic orogenic belt in the world. It consists of a network of belts that were formed by Proterozoic crustal accretion and the collision of pre-existing Archean continents. The event occurred 2.0–1.8 billion years ago.