Grenville Channel | |
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Grenville Channel | |
Grenville ChannelLocation in British Columbia | |
Location | North Coast RD, British Columbia |
Coordinates | 53°37′0″N 129°43′0″W / 53.61667°N 129.71667°W / 53.61667; -129.71667 |
Type | Strait |
Ocean/sea sources | Pacific Ocean |
Grenville Channel is a strait on the North Coast of British Columbia, Canada, between Pitt Island and the mainland to the south of Prince Rupert. It is part of the Inside Passage shipping route, about 45 nautical miles (83 km; 52 mi) long and is 0.2 nautical miles (0.37 km; 0.23 mi) wide at its narrowest point.
The Grenville Channel Fault that forms the channel dates back to the Cretaceous Era. Both sides are mountainous and densely wooded, and a linear magnetic anomaly runs parallel to the channel south of 51"30'N.
See also
- Baker Inlet
- Pa-aat River
- Kumealon Inlet
- Kxngeal Inlet
- Klewnuggit Inlet Marine Provincial Park
- Lowe Inlet Marine Provincial Park
- Union Passage Marine Provincial Park
References
- "Grenville Channel". BC Geographical Names.
- ^ "Chart 3772, 3773, Grenville Channel". Sailing Directions, British Columbia Coast, (Northern Portion). II (Ninth Edition): 158–159. 1983.
- Nelson J, Diakow L, van Staal C, Chipley D (2013). "Ordovician volcanogenic sulphides in the southern Alexander terrane, coastal NW British Columbia: geology, Pb isotopic signature, and a case for correlation with Appalachian and Scandinavian deposits" (PDF). British Columbia Geological Survey. 2013 (1): 13–33. S2CID 207961330. Archived from the original (PDF) on 2020-06-26. Retrieved 2020-06-23.
- Chardon D, Andronicos C, Holliste L (April 1999). "Large-scale transpressive shear zone patterns and displacements within magmatic arcs: The Coast Plutonic Complex, British Columbia". Tectonics. 18 (2): 278–292. Bibcode:1999Tecto..18..278C. doi:10.1029/1998TC900035.
External links
Media related to Grenville Channel at Wikimedia Commons
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