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About: Taconic orogeny     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatTaconicMountains, within Data Space : dbpedia.org associated with source document(s)

Type: yago:GeologicalFormation109287968yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitycountryyago:WikicatTaconicMountains New Facet based on Instances of this Class

The Taconic orogeny was a mountain building period that ended 440 million years ago and affected most of modern-day New England. A great mountain chain formed from eastern Canada down through what is now the Piedmont of the East coast of the United States. As the mountain chain eroded in the Silurian and Devonian periods, sediments from the mountain chain spread throughout the present-day Appalachians and midcontinental North America.