Mount Chōkai
Chokaisan
Stratovolcano · Japan · 2236m
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- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- Elevation
- 2236m
- Coordinates
- 39.099, 140.049
- Last eruption
- 1974
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
Massive Chokaisan volcano is composed of two overlapping stratovolcanoes with a conical profile that inspired the local names of Akita-Fuji or Dewa-Fuji. The summit of the gently sloping western edifice (Nishi-Chokaisan) is cut by a large scarp open to the south that contains lava domes. The younger eastern volcano (Higashi-Chokaisan) began forming about 20,000 years ago, and also has a large scarp, breached to the north. During an eruption about 2,600 years ago it was the source of the voluminous Kisakata debris avalanche, which reached the Pacific coast. Two post-caldera lava domes have been constructed at the upper SE end of the caldera. Intermittent reports of eruptions date back to the 6th century CE.
From Wikipedia
Mount Chōkai is an active volcano located on the border of Akita and Yamagata in the Tōhoku region of Japan, and is 2,236 m (7,336 ft) tall. Because of its (roughly) symmetrical shape and massive size, it is also variously known as Dewa Fuji (出羽富士), Akita Fuji (秋田富士) or Shōnai Fuji (庄内富士) depending on the location of the viewer. In addition to being one of the 100 Famous Landscapes of Japan, it is also included as one of the 100 famous mountains in Japan, and famous 100 Geographical Features of Japan. It is surrounded by Chōkai Quasi-National Park. It is also a National Historic Site of Japan, and is regarded as a sacred mountain by followers of the Shugendō branch of Shinto which has the shrine Chōkaisan Ōmonoimi Shrine there and is popular with hikers.
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Eruption history
Detailed timeline
- 1974VEI 1Observed1974-03-01 – 1974-04-30E side of Shinzan, W of Kojin-yama
- 1834VEI 2Observed1834-07-09 – 1834-07
- 1821VEI 2Observed1821-05-23 – OngoingNear Shinzan and Shichiko-zan
- 1800VEI 2Observed1800-12 – 1804-07Shinzan (foot of Kojin-yama)
- 1764VEI 2Geological estimate1764 – Ongoing
- 1740VEI 2Observed1740-06 – 1747Small crater at foot of Kojin-yama
- 1738VEI 2Geological estimate1738-12-31 – Ongoing
- 1735VEI 2Geological estimate1735 – Ongoing
- 1659VEI ?Observed1659-04 – 1663
- 1560VEI ?Geological estimate1560 – Ongoing
- 1477VEI ?Geological estimate1477 – Ongoing
- 999VEI ?Geological estimate999 – Ongoing
- 948VEI ?Geological estimate948-12-31 – Ongoing
- 939VEI ?Observed939-05-15 – Ongoing
- 884VEI ?Geological estimate884-07-26 – 884-08
- 871VEI 2Observed871-05-05 – Ongoing
- 861VEI 3Geological estimate861-05 – Ongoing
- 857VEI ?Geological estimate857-05 – Ongoing
- 856VEI ?Geological estimate856 – Ongoing
- 839VEI ?Geological estimate839-10-14 – Ongoing
- 830VEI ?Observed830-01 – Ongoing
- 817 (±7 yrs)VEI ?Observed817 – Ongoing
- 804VEI ?Geological estimate804 – 806
- 717VEI ?Geological estimate717-07 – Ongoing
- 711 (±3 yrs)VEI ?Observed711 – Ongoing
- 610 (±18 yrs)VEI ?Geological estimate610 – Ongoing
- 577VEI ?Geological estimate577-12-01 – 578-07-15
- 573VEI ?Geological estimate573-03 – Ongoing
- 450 BCEVEI ?Geological estimateBCE 450 – Ongoing
- 650 BCEVEI ?Geological estimateBCE 650 – OngoingHigashi-Chokai
- 1050 BCEVEI 0Geological estimateBCE 1050 – OngoingWest flank (Saruana crater)
External links
⚠ For reference only. Not for emergency response.