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Some geologists hypothesize that the Anahim hotspot is linked with an upper mantle plume (miniplume) rather than the more common deep mantle plume because of the small size of the Bella Bella and Gale Passage dike swarms.
A few volcanic centers in the vicinity of the Bella Bella and Gale Passage dike swarms, such as Helmet Peak and Kitasu Hill, which are members of the Milbanke Sound Group, may represent the westernmost of the Anahim volcanoes, but their ages are significantly different, provoking on-going questions about their origin and connection to other regional volcanic activity.
About 13 and 12 million years ago, the Anahim hotspot created a peralkaline volcanic complex on what was then the coast of British Columbia, now heavily eroded to form the ~20 km long Bella Bella and ~6 km long Gale Passage dike swarms.
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