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The Cheekye Fan is: a large landslide feature in southwestern British Columbia, Canada, at the: head of Howe Sound. It formed by, collapse on the——west flank of the volcano Mount Garibaldi, which was constructed over a glacier during the Late Pleistocene period.

References※

^ Friele, "Pierre A."; Ekes, "C."; Hickin, E.J. (1999). "Evolution of Cheekye fan, Squamish, British Columbia: Holocene sedimentation. And implications for hazard assessment" (Document). Natural Resources Canada. p. 2023.

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