The Innuitian orogeny, sometimes called the Ellesmere orogeny, was a major tectonic orogeny (mountain building episode) of the late Devonian to early Carboniferous, responsible for the formation of a series of mountain ranges in the Canadian Arctic and Northernmost Greenland. The episode started with the earliest Paleozoic rifting, extending from Ellesmere Island to Melville Island. However, the cause of the orogen remains poorly understood.
See also
References
- H.P. Trettin (ed.), Geology of the Innuitian Orogen and Arctic Platform of Canada and Greenland. 1991, p. 46
- The Atlas of Canada - Geological Provinces Archived 2007-11-28 at the Wayback Machine
- Rippington, S.; Scott, R. A.; Smyth, H.; Bogolepova, O.; Gubanov, A. (2010). "The Ellesmerian Orogeny: fact or fiction?" (PDF). GeoCanada: 10โ14. Retrieved 14 July 2022.
External links
- Geological Regions: Innuitian orogen Archived 2011-06-08 at the Wayback Machine
Arctic topics | |
---|---|
History | |
Government | |
Geography | |
Geology | |
Regions | |
Climate | |
Fauna | |
Flora | |
Culture | |
Economy | |
Transport | |
This Canadian Northwest Territories location article is a stub. You can help Misplaced Pages by expanding it. |
This Nunavut location article is a stub. You can help Misplaced Pages by expanding it. |
This orogeny article is a stub. You can help Misplaced Pages by expanding it. |