Cheekye Fan

The Cheekye Fan is a large landslide feature in southwestern British Columbia, Canada, located at the head of Howe Sound. It formed as a result of collapse on the western flank of Mount Garibaldi when the volcano was constructed on top of a glacier during the Late Pleistocene period.^[1]

References

1. ^ Friele, Pierre A.; Ekes, C.; Hickin, E.J. (1999). Evolution of Cheekye fan, Squamish, British Columbia: Holocene sedimentation and implications for hazard assessment¹. Natural Resources Canada. p. 2023. 

This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it.v · Categories: Landslides in Canada Natural disasters in British Columbia Garibaldi Volcanic Belt British Columbia Coast geography stubs Canadian geology stubs Wikimedia Foundation. 2010. Игры ⚽ Нужна курсовая? The Cheek Edwin Cheel Look at other dictionaries: Mount Garibaldi — as seen from Squamish Elevation 2,678 m (8,786 ft)  …   Wikipedia Landslide — This article is about the geological phenomenon. For other uses, see Landslide (disambiguation). Rockslide redirects here. For the comic book character, see Rockslide (comics). Computer simulation of a slump landslide in San Mateo County,… …   Wikipedia 18+ © Academic, 2000-2024 Contact us: Technical Support, Advertising Dictionaries export, created on PHP, Joomla, Drupal, WordPress, MODx. Mark and share Search through all dictionaries Translate… Search Internet Share the article and excerpts Direct link … Do a right-click on the link above and select “Copy Link”