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Hiuchigatake: Difference between revisions

Coordinates: 36°57′7″N 139°17′19″E / 36.95194°N 139.28861°E / 36.95194; 139.28861
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{{About|a mountain in Fukushima Prefecture|a mountain in Niigata Prefecture|Mount Hiuchi}}
{{About|a mountain in Fukushima Prefecture|a mountain in Niigata Prefecture|Mount Hiuchi}}
{{short description|Mountain in Japan}}
{{Infobox mountain
{{Infobox mountain
| name = Hiuchi
| name = Mount Hiuchi
| other_name =Mount Hiuchigatake
| other_name =Hiuchigatake
| native_name = 燧ヶ岳ひうちがたけ
| native_name ={{native name|ja|燧ヶ岳ひうちがたけ}}
| native_name_lang =
| photo = Hiuchigatake 080923 4.JPG
| photo = Hiuchigatake 080923 4.JPG
| photo_size =
| photo_size =
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}}
}}


'''Hiuchi''', also '''Hiuchigatake''' ({{lang-ja|燧ヶ岳ひうちがたけ}}) is a 2,356m tall [[stratovolcano]] mountain in [[Oze National Park]], and located in [[Hinoemata, Fukushima|Hinoemata]] Village, Minami-Aizu gun, [[Fukushima Prefecture]], [[Japan]]. This is the highest mountain in [[Tōhoku region]].<ref>https://www.env.go.jp/en/nature/nps/park/oze/guide/view.html</ref> The volcano rises in the north of {{ill2|Lake Ozenuma|ja|尾瀬沼おぜぬま}}. It is one of the [[100 Famous Japanese Mountains]].<ref name=kotobank /><ref name=kotobank2 />
'''Mount Hiuchi''', also '''Hiuchigatake''' ({{lang-ja|燧ヶ岳ひうちがたけ}}) is a 2,356 m tall [[stratovolcano]] in [[Oze National Park]], and located in [[Hinoemata, Fukushima|Hinoemata]] Village, Minami-Aizu gun, [[Fukushima Prefecture]], [[Japan]]. This is the highest mountain in [[Tōhoku region]].<ref>{{Cite web|url=https://www.env.go.jp/en/nature/nps/park/oze/guide/view.html|title=Oze National Park_Guide of Highlights &#91;MOE&#93;}}</ref> The volcano rises in the north of {{ill2|Lake Ozenuma|ja|尾瀬沼おぜぬま}}. It is one of the [[100 Famous Japanese Mountains]].<ref name=kotobank /><ref name=kotobank2 />


==Morphology==
==Morphology==
{{unreferenced section|date=December 2017}}
{{unreferenced section|date=December 2017}}


Hiuchi initially formed around 350,000&nbsp;years ago. Around 160,000–170,000&nbsp;years ago, Hiuchi erupted, creating a large [[pyroclastic]] flow deposit. At the summit of the volcano lie two [[lava dome]]s, Akanagure (赤あかナグレ) and Mi-ike (御池岳おいけがたけ). Akanagure, the southern dome, produced a series of [[Viscosity|viscous]] [[lava flow]]s that flowed down the southern and western parts of the volcano about 3500&nbsp;years ago. Mi-ike is responsible for the only recorded activity.
Hiuchi initially formed around 350,000&nbsp;years ago. Around 160,000–170,000&nbsp;years ago, Hiuchi erupted, creating a large [[Pyroclastic rock|pyroclastic]] flow deposit. At the summit of the volcano lie two [[lava dome]]s, Akanagure (赤あかナグレ) and Mi-ike (御池岳おいけがたけ). Akanagure, the southern dome, produced a series of [[Viscosity|viscous]] [[lava flow]]s that flowed down the southern and western parts of the volcano about 3500&nbsp;years ago. Mi-ike is responsible for the only recorded activity.


==Historic eruptions==
==Historic eruptions==
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| lat3_deg = 35
| lat3_deg = 35
| lon3_deg = 90
| lon3_deg = 90
| label4 = {{ill2|Mont Shibutsu|ja|至仏山しぶつさん}}
| label4 = [[Mount Shibutsu]]
| position4 =
| position4 =
| background4 =
| background4 =
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==Further reading==
==Further reading==
* {{cite journal| title=Eruptive History of Hiuchi Volcano|authors=Yukio HAYAKAWA, Fusao ARAI and Tomohiro KITAZUME | journal=Journal of Geography (Chigaku Zasshi) | volume=106 | number=5 | pages=660–664 | year=1997 | doi=10.5026/jgeography.106.5_660}}
* {{cite journal| title=Eruptive History of Hiuchi Volcano|author1=Yukio Hayakawa |author2=Fusao Arai |author3=Tomohiro Kitazume | journal=Journal of Geography (Chigaku Zasshi) | volume=106 | number=5 | pages=660–664 | year=1997 | doi=10.5026/jgeography.106.5_660| doi-access=free }}


==External links==
==External links==
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* [http://www.data.jma.go.jp/svd/vois/data/tokyo/STOCK/souran_eng/volcanoes/038_hiuchigatake.pdf National catalogue of the active volcanoes in Japan: Hiuchigatake] - Japan Meteorological Agency
* [http://www.data.jma.go.jp/svd/vois/data/tokyo/STOCK/souran_eng/volcanoes/038_hiuchigatake.pdf National catalogue of the active volcanoes in Japan: Hiuchigatake] - Japan Meteorological Agency
* [https://gbank.gsj.jp/volcano/Quat_Vol/volcano_data/E06.html Quaternary Volcanoes: Hiuchigatake] - Geological Survey of Japan, AIST
* [https://gbank.gsj.jp/volcano/Quat_Vol/volcano_data/E06.html Quaternary Volcanoes: Hiuchigatake] - Geological Survey of Japan, AIST
* {{cite gvp|name=Hiuchigatake|vn=283131|access-date=2021-06-24}}
* [http://volcano.si.edu/volcano.cfm?vn=283131 Global Volcanism Program: Hiuchigatake] - Smithsonian Institution
* [http://www.volcanolive.com/hiuchi.html Volcanolive.com]
* [http://www.volcanolive.com/hiuchi.html Volcanolive.com]


{{100 Famous Japanese Mountains}}
{{100 Famous Japanese Mountains}}
{{National parks of Japan}}
{{National parks of Japan}}



{{authority control}}
{{authority control}}


[[Category:Volcanoes of Japan]]
[[Category:Stratovolcanoes of Japan]]
[[Category:Active volcanoes]]
[[Category:Active volcanoes]]
[[Category:National parks of Japan]]
[[Category:National parks of Japan]]

Latest revision as of 06:19, 26 December 2023

This article is about a mountain in Fukushima Prefecture. For a mountain in Niigata Prefecture, see Mount Hiuchi.
Mount Hiuchi
Hiuchigatake
Highest point
Elevation2,356[1] m (7,730 ft)
Coordinates36°57′7″N 139°17′19″E / 36.95194°N 139.28861°E / 36.95194; 139.28861
Naming
Native name燧ヶ岳ひうちがたけ (Japanese)
Geography
Mount Hiuchi is located in Japan
Mount Hiuchi
Mount Hiuchi
Honshu, Japan
Mount Hiuchi is located in Fukushima Prefecture
Mount Hiuchi
Mount Hiuchi
Mount Hiuchi (Fukushima Prefecture)
Geology
Age of rockQuaternary
Mountain typeStratovolcano[2]
Last eruptionJuly 1544[1]

Mount Hiuchi, also Hiuchigatake (Japanese: 燧ヶ岳ひうちがたけ) is a 2,356 m tall stratovolcano in Oze National Park, and located in Hinoemata Village, Minami-Aizu gun, Fukushima Prefecture, Japan. This is the highest mountain in Tōhoku region.[3] The volcano rises in the north of Lake Ozenuma [ja]. It is one of the 100 Famous Japanese Mountains.[2][4]

Morphology

[edit]

Hiuchi initially formed around 350,000 years ago. Around 160,000–170,000 years ago, Hiuchi erupted, creating a large pyroclastic flow deposit. At the summit of the volcano lie two lava domes, Akanagure (赤あかナグレ) and Mi-ike (御池岳おいけがたけ). Akanagure, the southern dome, produced a series of viscous lava flows that flowed down the southern and western parts of the volcano about 3500 years ago. Mi-ike is responsible for the only recorded activity.

Historic eruptions

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1544 eruptions

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The only recorded activity was on July 28, 1544. A moderate phreatic eruption at the Mi-ike Lava Dome produced lahars and an associated tephra layer.[1][5]

class=notpageimage|
Around Ozegahara

See also

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References

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  1. ^ a b c "Hiuchigatake: National catalogue of the active volcanoes in Japan" (PDF). Japan Meteorological Agency. Retrieved 2017-12-13.
  2. ^ a b "燧ヶ岳ひうちがたけ" (in Japanese). kotobank. Retrieved 2017-12-13.
  3. ^ "Oze National Park_Guide of Highlights [MOE]".
  4. ^ "日本にっぽん百名山ひゃくめいざん" (in Japanese). kotobank. Retrieved 2017-12-13.
  5. ^ Yukio Hayakawa (1994). "燧ヶ岳ひうちがたけで見みつかった約やく500年ねん前まえの噴火ふんか堆積たいせき物ぶつ". 火山かざん (in Japanese). 39 (5). doi:10.18940/kazan.39.5_243.

Further reading

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[edit]
Wikimedia Commons has media related to Mount Hiuchi (Fukushima).


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