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The most famous mountain in Japan is also one of its most dangerous. As, Mount Fuji is still an active volcano which only about 300 years ago produced a destructive eruption which was 30% larger than the 1980 eruption of Mount Saint Helens. This video will discuss that eruption and elaborate on how Mount Fuji grew to its modern height. Thumbnail Photo Credit: kimura2, Pixabay, Pixabay License, https://pixabay.com/photos/mountain-v.... The color contrast of this image was reduced, the brightness of this image was increased, it was overlaid with text, and then overlaid with GeologyHub made graphics (the image border & the GeologyHub logo). If you would like to support this channel, consider using one of the following links: (Patreon: / geologyhub ) (YouTube membership: / @geologyhub ) (Gemstone & Mineral Etsy store: http://prospectingarizona.etsy.com) (GeologyHub Merch Etsy store: http://geologyhub.etsy.com) Google Earth imagery used in this video: ©Google & Data Providers This video is protected under "fair use". If you see an image and/or video which is your own in this video, and/or think my discussion of a scientific paper (and/or discussion/mentioning of the data/information within a scientific paper) does not fall under the fair use doctrine, and wish for it to be censored or removed, contact me by email at [email protected] and I will make the necessary changes. Various licenses used in sections of this video (not the entire video, this video as a whole does not completely fall under one of these licenses) and/or in this video's thumbnail image (and this list does not include every license used in this video and/or thumbnail image): Public Domain: https://creativecommons.org/publicdom... CC BY 2.0: https://creativecommons.org/licenses/... Pixabay License: https://pixabay.com/service/terms/#li... Sources/Citations: [1] Japanese Meteorological Agency (JMA) [2] Japanese Meteorological Agency, 55, Fujisan [3] VEIs, dates/years, composition, tephra layer name, DRE estimates, and bulk tephra volume estimates for volcanic eruptions shown in this video which were assigned a VEI 4 or larger without an asterisk after their name are sourced from the LaMEVE database (British Geological Survey © UKRI), https://www2.bgs.ac.uk/vogripa/view/c..., Used with Permission [4] Source of Volcanic Explosivity Index (VEI) methodology and criteria: Newhall, C. G., and Self, S. (1982), The volcanic explosivity index (VEI) an estimate of explosive magnitude for historical volcanism, J. Geophys. Res., 87(C2), 1231–1238, doi:10.1029/JC087iC02p01231. Accessed / Read by / geologyhub on Oct 5th, 2022. [5] Sano, T. & Fukuoka, T. & Ishimoto, M.. (2011). Petrological constraints on magma evolution of the Fuji volcano: A case study for the 1707 Hoei eruption. Mem. Nat. Mus. Nat. Sci. 47. 471-496. [6] J. Ewert, A. Diefenbach, D. Ramsey, "2018 Update to the U.S. Geological Survey National Volcanic Threat Assessment", U.S. Geological Survey, Accessed October 22, 2022. https://pubs.usgs.gov/sir/2018/5140/s... 0:00 Mount Fuji 1:12 Red Coloration 1:52 Geologic History 3:28 1707 - 1708 Eruption 4:29 Future Hazards