Mount Echizen-dake explained
is a Japanese volcanic peak in the area south-east of Mount Fuji. Its summit, 1,504 meters high,[1] is located in the Susono City, Shizuoka. It is the highest peak of the Mount Ashitaka lava dome.
History
- Mount Echizen-dake erupted in the mid-Pleistocene epoch,[2] about 100,000 years ago.[3] It is an extinct volcano.[4]
- Echizen-dake was depicted on the 50-yen banknote of the 1938 issue.
See also
References
The page incorporated material from Japanese Wikipedia page 越前岳, accessed 23 April 2019
Notes and References
- Karátson, D. "Erosion calderas: origins, processes, structural and climatic control," Bulletin of Volcanology Vol. 61 (1999), pp. 179 [PDF 6 of 20]; retrieved 2012-6-21.
- University of Tokyo, Volcano Research Center, "Geology of Fuji Volcano"; retrieved 2012-6-21.
- Kishimoto, Hiroshi et al. "Pyroclastic cone on southwestern flank of Ashikita Volcano," Japan Geoscience Union, 2010; retrieved 2012-6-21.
- Shizuoka Guide, "Overview of Mt Fuji; retrieved 2012-6-21.