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- Karmutsen_Formation abstract "The Karmutsen Formation is a Late Triassic volcanic sequence of tholeiitic pillow basalts and breccias on Vancouver Island, British Columbia, Canada. It is perhaps the thickest accreted section of an oceanic plateau worldwide, exposing up to 6000 m of basal sediment-sill complexes, basaltic to picritic pillow lavas, pillow breccia, and thick, massive basalt flows. The widespread succession of basalts and breccias are part of the Insular Mountains, a large volcanic mountain range that forms Vancouver Island and the Queen Charlotte Islands. In Strathcona Provincial Park, pillow basalts is the most abundant rock unit. About half the mountains, including the highest ones, are carved from these basalts, such as Golden Hinde, which is the highest peak on Vancouver Island.".
- Karmutsen_Formation thumbnail Ghinde2.jpg?width=300.
- Karmutsen_Formation wikiPageID "14407542".
- Karmutsen_Formation wikiPageLength "1494".
- Karmutsen_Formation wikiPageOutDegree "20".
- Karmutsen_Formation wikiPageRevisionID "589648475".
- Karmutsen_Formation wikiPageWikiLink Basalt.
- Karmutsen_Formation wikiPageWikiLink Breccia.
- Karmutsen_Formation wikiPageWikiLink British_Columbia.
- Karmutsen_Formation wikiPageWikiLink Canada.
- Karmutsen_Formation wikiPageWikiLink Category:Flood_basalts.
- Karmutsen_Formation wikiPageWikiLink Category:Geography_of_Vancouver_Island.
- Karmutsen_Formation wikiPageWikiLink Category:Triassic_volcanism.
- Karmutsen_Formation wikiPageWikiLink Category:Volcanism_of_British_Columbia.
- Karmutsen_Formation wikiPageWikiLink Golden_Hinde_(mountain).
- Karmutsen_Formation wikiPageWikiLink Haida_Gwaii.
- Karmutsen_Formation wikiPageWikiLink Insular_Mountains.
- Karmutsen_Formation wikiPageWikiLink Late_Triassic.
- Karmutsen_Formation wikiPageWikiLink Mountain_range.
- Karmutsen_Formation wikiPageWikiLink Oceanic_plateau.
- Karmutsen_Formation wikiPageWikiLink Pillow_basalt.
- Karmutsen_Formation wikiPageWikiLink Queen_Charlotte_Islands.
- Karmutsen_Formation wikiPageWikiLink Sill_(geology).
- Karmutsen_Formation wikiPageWikiLink Strathcona_Provincial_Park.
- Karmutsen_Formation wikiPageWikiLink Vancouver_Island.
- Karmutsen_Formation wikiPageWikiLink Volcanism_of_Western_Canada.
- Karmutsen_Formation wikiPageWikiLink Volcanology_of_Western_Canada.
- Karmutsen_Formation wikiPageWikiLink File:Ghinde2.jpg.
- Karmutsen_Formation wikiPageWikiLinkText "Karmutsen Formation".
- Karmutsen_Formation hasPhotoCollection Karmutsen_Formation.
- Karmutsen_Formation wikiPageUsesTemplate Template:BritishColumbiaCoast-geo-stub.
- Karmutsen_Formation wikiPageUsesTemplate Template:Coord_missing.
- Karmutsen_Formation wikiPageUsesTemplate Template:Portal.
- Karmutsen_Formation wikiPageUsesTemplate Template:Reflist.
- Karmutsen_Formation subject Category:Flood_basalts.
- Karmutsen_Formation subject Category:Geography_of_Vancouver_Island.
- Karmutsen_Formation subject Category:Triassic_volcanism.
- Karmutsen_Formation subject Category:Volcanism_of_British_Columbia.
- Karmutsen_Formation type Article.
- Karmutsen_Formation type Event.
- Karmutsen_Formation type Article.
- Karmutsen_Formation type Event.
- Karmutsen_Formation type Formation.
- Karmutsen_Formation type Hazard.
- Karmutsen_Formation comment "The Karmutsen Formation is a Late Triassic volcanic sequence of tholeiitic pillow basalts and breccias on Vancouver Island, British Columbia, Canada. It is perhaps the thickest accreted section of an oceanic plateau worldwide, exposing up to 6000 m of basal sediment-sill complexes, basaltic to picritic pillow lavas, pillow breccia, and thick, massive basalt flows.".
- Karmutsen_Formation label "Karmutsen Formation".
- Karmutsen_Formation sameAs m.03d2l96.
- Karmutsen_Formation sameAs Q6372779.
- Karmutsen_Formation sameAs Q6372779.
- Karmutsen_Formation wasDerivedFrom Karmutsen_Formation?oldid=589648475.
- Karmutsen_Formation depiction Ghinde2.jpg.
- Karmutsen_Formation isPrimaryTopicOf Karmutsen_Formation.