Mount Chōkai
Chokaisan
Stratovulcano · Japan · 2236 m
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- Tipo
- Stratovulcano
- Paese
- Japan
- Regione
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- Altitudine
- 2236 m
- Coordinate
- 39.099, 140.049
- Ultima eruzione
- 1974
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Andesite / Basaltic Andesite
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in ingleseMount 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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Storia delle eruzioni
Cronologia dettagliata
- 1974VEI 1Osservata1974-03-01 – 1974-04-30E side of Shinzan, W of Kojin-yama
- 1834VEI 2Osservata1834-07-09 – 1834-07
- 1821VEI 2Osservata1821-05-23 – In corsoNear Shinzan and Shichiko-zan
- 1800VEI 2Osservata1800-12 – 1804-07Shinzan (foot of Kojin-yama)
- 1764VEI 2Stima geologica1764 – In corso
- 1740VEI 2Osservata1740-06 – 1747Small crater at foot of Kojin-yama
- 1738VEI 2Stima geologica1738-12-31 – In corso
- 1735VEI 2Stima geologica1735 – In corso
- 1659VEI ?Osservata1659-04 – 1663
- 1560VEI ?Stima geologica1560 – In corso
- 1477VEI ?Stima geologica1477 – In corso
- 999VEI ?Stima geologica999 – In corso
- 948VEI ?Stima geologica948-12-31 – In corso
- 939VEI ?Osservata939-05-15 – In corso
- 884VEI ?Stima geologica884-07-26 – 884-08
- 871VEI 2Osservata871-05-05 – In corso
- 861VEI 3Stima geologica861-05 – In corso
- 857VEI ?Stima geologica857-05 – In corso
- 856VEI ?Stima geologica856 – In corso
- 839VEI ?Stima geologica839-10-14 – In corso
- 830VEI ?Osservata830-01 – In corso
- 817 (±7 anni)VEI ?Osservata817 – In corso
- 804VEI ?Stima geologica804 – 806
- 717VEI ?Stima geologica717-07 – In corso
- 711 (±3 anni)VEI ?Osservata711 – In corso
- 610 (±18 anni)VEI ?Stima geologica610 – In corso
- 577VEI ?Stima geologica577-12-01 – 578-07-15
- 573VEI ?Stima geologica573-03 – In corso
- 450 a.C.VEI ?Stima geologicaBCE 450 – In corso
- 650 a.C.VEI ?Stima geologicaBCE 650 – In corsoHigashi-Chokai
- 1050 a.C.VEI 0Stima geologicaBCE 1050 – In corsoWest flank (Saruana crater)
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.