They are geologically composed of igneous hypabyssal rocks, tuffs and basaltic andesite.
2.
Hypabyssal rocks are less common than plutonic or volcanic rocks and often form dikes, sills, laccoliths, lopoliths, or phacoliths.
3.
These differing facies are associated with a particular style of magmatic activity, namely crater, diatreme and hypabyssal rocks ( Clement and Skinner 1985, and Clement, 1982 ).
4.
Eruptions of basaltic to rhyolitic volcanoes and hypabyssal rocks of the Alert Bay Volcanic Belt in northern Vancouver Island are probably linked with the subducted margin flanked by the Explorer and Juan de Fuca Plates at the Cascadia subduction zone.
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