Volcanism of Canada
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Volcanic activity is a major part of the geology of Canada and is characterized by many types of volcanic landform, including lava flows, volcanic plateaus, lava domes, cinder cones, stratovolcanoes,
Mount Edziza, a stratovolcano in northwestern British Columbia
Eve Cone, one of the best preserved cinder cones in Canada.
Plinth Peak of the Mount Meager massif in southwestern British Columbia is the source for a large-scale Plinian eruption that occurred 2,350 years ago, sending ash as far as Alberta
Komatiite sample collected in the Abitibi greenstone belt near Englehart, Ontario. Specimen is 9 cm (4 in) wide. Bladed olivine crystals are visible, though spinifex texture is weak or absent in this sample.
Volcanism of Eastern Canada
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The volcanism of Eastern Canada includes the hundreds of volcanic areas and extensive lava formations in Eastern Canada. The region's different volcano and lava types originate from different tectonic
Mount McKay, a mafic sill related to volcanism of the Midcontinent Rift System in Thunder Bay, Ontario.
Mont Saint-Hilaire, an intrusive mountain of the Monteregian Hills in southern Quebec formed by the New England hotspot
Basal contact of a lava flow section of the Fundy Basin