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白頭山

Changbaishan

成層火山 · China-North Korea · 2744m

Lake Tianchi occupies the 5-km-wide, 850-m-deep summit caldera of Changbaishan, which straddles the China/Korea border. The volcano is also known as Baitoushan and by the Korean names of Baegdu or P'aektu-san. This view looks from the northern rim on the Chinese side towards the SE caldera wall on the Korean side. One of the world's largest known Holocene explosive eruptions took place from Changbaishan about 1000 CE, depositing tephra as far away as northern Japan.
Lake Tianchi occupies the 5-km-wide, 850-m-deep summit caldera of Changbaishan, which straddles the China/Korea border. The volcano is also known as Baitoushan and by the Korean names of Baegdu or P'aektu-san. This view looks from the northern rim on the Chinese side towards the SE caldera wall on the Korean side. One of the world's largest known Holocene explosive eruptions took place from Changbaishan about 1000 CE, depositing tephra as far away as northern Japan. · 写真: Photo by Xiang Liu, 1983 (Changchun University). · Wikimedia Commons
タイプ
成層火山
China-North Korea
地域
Eastern Asia Volcanic Regions / Central East Asia Volcanic Province
標高
2744m
座標
41.980, 128.080
最終噴火
1903年
テクトニクス環境
Intraplate / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Trachyte / Trachydacite
地質学的概要

Massive Changbaishan stratovolcano (also known as Baitoushan and by the Korean names of Baegdu, Paektu, or P'aektu-san), is located along the China/Korea border. A 5-km-wide, 850-m-deep summit caldera is filled by Lake Tianchi (Sky Lake). The 60-km-diameter dominantly trachytic and rhyolitic volcano was constructed over the Changbaishan (Laoheidingzi) shield volcano. Satellitic cinder cones are aligned along a NNE trend. One of the largest known Holocene explosive eruptions took place here about 946 CE, depositing tephra as far away as northern Japan and forming in part the present caldera; Yang et al. (2021) estimated the total erupted volume to be 40-98 km3. Minor eruptions have been recorded since the 15th century.

Wikipedia の要約

要約が短いです。詳細は記事全文をご覧ください。

長白山脈 は、中華人民共和国と朝鮮民主主義人民共和国との国境付近を走る山脈である。

Wikipedia · CC BY-SA · 記事全文を読む

噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
2155 BCE~1962 BCE · 1件 · 最大 VEI 41189 BCE~996 BCE · 1件 · 最大 VEI ?223 BCE~29 BCE · 1件 · 最大 VEI 4937~1130 · 1件 · 最大 VEI 61323~1517 · 1件 · 最大 VEI ?1517~1710 · 3件 · 最大 VEI ?1710~1903 · 2件 · 最大 VEI 22155 BCE1189 BCE223 BCE7441710

詳細タイムライン

  1. 1903年VEI ?観測記録
    1903-04-15 ~ 進行中
    Liuhaojie tuff ring?
  2. 1898年VEI 2観測記録
    1898 ~ 進行中
  3. 1702年VEI ?観測記録
    1702-06-09 ~ 進行中
  4. 1668年VEI ?観測記録
    1668-06 ~ 進行中
  5. 1597年VEI ?地質学的推定
    1597-10-06 ~ 進行中
  6. 1413年VEI ?地質学的推定
    1413 ~ 進行中
  7. 946年VEI 6地質学的推定
    946-11-15 ~ 進行中
    Millennium Eruption
  8. 紀元前 180年 (±80年)VEI 4地質学的推定
    BCE 180 ~ 進行中
  9. 紀元前 1000年VEI ?地質学的推定
    BCE 1000 ~ 進行中
  10. 紀元前 2155年 (±90年)VEI 4地質学的推定
    BCE 2155 ~ 進行中

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。