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The Akahoya eruption was the strongest known volcanic eruption of the Kikai Caldera in Kyūshū, Japan. It ejected about 150 cubic kilometres (36 cu mi) of volcanic material, giving it a Volcanic Explosivity Index of 7.[2]

Akahoya eruption
VolcanoKikai Caldera
Date6,860 to 7,440 years calibrated before present[1]
TypeUltra-Plinian
LocationKyūshū, Japan
30.789°N 130.308°E / 30.789; 130.308
VEI7.2[1]
ImpactOne of only six confirmed eruptions of its size in the Holocene; dramatically changed vegetation in Southern Kyūshū and impacted on the Jōmon culture
Affected areas of the eruption

Retrospective dating


Archaeologically it has been dated around 7,300 cal. BP during the earliest stage of the Jōmon period,[3] but it had also been uncorrected radiocarbon dated to as recent as 6,500 BP.[4] The current accepted dating adjustment from multiple other sources is about 7,200 to 7,300 years ago.[5][6][1]


Aftermath


This eruption has been linked to the end of the initial Jōmon culture in southern Kyūshū although impact, although marked, was not as great as some commentary had suggested with Nishinozono sub-type pottery tradition, that had started prior maintained throughout and after the eruption sequence in Kyūshū.[7] It took nearly 1000 years to recover.[8] Jōmon who lived further away survived such as on northern Kyūshū, Honshū and Hokkaidō but likely had to revert for a period to maritime food sources mainly.[7]

The fate of the initial Jōmon culture on south Kyūshū does not quite parallel the demise of the Minoan civilization, which ended as a consequence of another massive volcanic eruption.

However these events give more credence to cultural traditions that maintain stories of established cultures vanishing quickly and completely, since it is known to have happened in (Holocene) human history, in two very different parts of the world. The events also call for deeper study into the effects of volcanic activity on human cultural development.


References


  1. Smith, Victoria C.; Staff, Richard A.; Blockley, Simon P.E.; Ramsey, Christopher Bronk; Nakagawa, Takeshi; Mark, Darren F.; Takemura, Keiji; Danhara, Toru (2013). "Identification and correlation of visible tephras in the Lake Suigetsu SG06 sedimentary archive, Japan: chronostratigraphic markers for synchronising of east Asian/west Pacific palaeoclimatic records across the last 150 ka". Quaternary Science Reviews. 67: 121–137. doi:10.1016/j.quascirev.2013.01.026. ISSN 0277-3791.
  2. "Eruptive history of Kikai". Global Volcanism Program. Washington, DC: Smithsonian Institution.
  3. Kuwahata, Mitsuhiro (2002). "Age and cultural influence of the Kikai-Akahoya eruption as seen from archaeological material in south Kyūshū, Japan". Quaternary Research. 41 (4): 317–330. doi:10.4116/jaqua.41.317. ISSN 0418-2642.
  4. Maeno, Fukashi; Taniguchi, Hiromitsu (2005). "Eruptive history of Satsuma Iwo-jima Island, Kikai caldera, after a 6.5 ka caldera-forming eruption". Bulletin of the Volcanological Society of Japan. 50 (2): 71–85. ISSN 0453-4360.
  5. Okuno, Mitsuru (2019-04-15). "Chronological study on widespread tephra and volcanic stratigraphy of the past 100,000 years". The Journal of the Geological Society of Japan. 125 (1): 41–53. doi:10.5575/geosoc.2018.0069. ISSN 1349-9963.
  6. Tsuji, Tomohiro; Ikeda, Michiharu; Furusawa, Akira; Nakamura, Chisato; Ichikawa, Kiyoshi; Yanagida, Makoto; Nishizaka, Naoki; Ohnishi, Kozo; Ohno, Yuki (2018). "High resolution record of Quaternary explosive volcanism recorded in fluvio-lacustrine sediments of the Uwa basin, southwest Japan". Quaternary International. 471: 278–297. doi:10.1016/j.quaint.2017.10.016. ISSN 1040-6182.
  7. Junzo, Uchiyama (2021). "After a Super Volcanic Eruption: a new project on social-ecological impacts of the Kikai-Akahoya disaster, 7,300 years ago". Retrieved 2022-09-18.
  8. "巨大カルデラ噴火のメカニズムとリスクを発表" [Announcement of the mechanism and risks of a massive caldera eruptions] (Press release). Kobe University. 22 October 2014. Archived from the original on 30 March 2019. Retrieved 31 March 2019.





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