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ケニア · 楯状火山

バリアー山

Barrier, The

タイプ
楯状火山
標高
1032m
最終噴火
1921年
A northward-looking aerial view shows the summit caldera of Kakorinya volcano of The Barrier volcanic complex with Lake Turkana in the distance. The 3.8-km-wide summit caldera was formed about 92,000 years ago, and post-caldera lava domes and flows fill much of the caldera floor. Fresh-looking lava flows and tuff cones occur along the shores of Lake Turkana. Teleki's Cone on the northern flank and Andrew's Cone (lower left foreground) on the southern flank have been the source of historical lava flows.
A northward-looking aerial view shows the summit caldera of Kakorinya volcano of The Barrier volcanic complex with Lake Turkana in the distance. The 3.8-km-wide summit caldera was formed about 92,000 years ago, and post-caldera lava domes and flows fill much of the caldera floor. Fresh-looking lava flows and tuff cones occur along the shores of Lake Turkana. Teleki's Cone on the northern flank and Andrew's Cone (lower left foreground) on the southern flank have been the source of historical lava flows. · 写真: Photo by Martin Smith, 1993 (copyright British Geological Survey, NERC).
タイプ
楯状火山
国
ケニア
地域
東アフリカ / Kenyan Rift Volcanic Province
標高
1032m
座標
2.320, 36.570
最終噴火
1921年
テクトニクス環境
リフト帯 / 大陸地殻 (> 25 km)
火山地形
楯状火山
主要岩石
粗面岩 / 粗面デイサイト
地質学的概要

The Barrier volcanic complex separates Lake Turkana from the broad Suguta Trough to the S, the site of a former lake. The volcano is comprised of four overlapping shield volcanoes, with the youngest, Kakorinya, located over the axis of the East African Rift. Kalolenyang volcano lies W of Kakorinya, and Likaiu West and Likaiu East are located to the ENE. A 3.8-km-wide summit caldera was formed at Kakorinya about 92,000 years ago. Youthful-looking trachytic and phonolitic lava domes and flows erupted within the caldera and along its ring fracture fill much of the caldera floor. Early Holocene fissure-related scoria cones and lava flows dot the S and N flanks. Solfataric fields are located within the caldera and on the W and S flanks. Historical eruptions from Teleki's and Andrew's cones on the N and S flanks, respectively, have produced basaltic explosive activity and lava flows during the 19th and 20th centuries.

噴火履歴

12件の記録用語集
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 · 矢印キーで棒を移動、Enterで表示
紀元前 7710~紀元前 7389 · 1件 · 最大 VEI ?958~1279 · 3件 · 最大 VEI 01600~1921 · 8件 · 最大 VEI 2紀元前 7710紀元前 5463紀元前 2894紀元前 6471600

詳細タイムライン

  1. 1921年VEI 2観測記録
    1921-12-31 ~ 終了日不明
    North flank (Teleki)
  2. 1920年 (±3年)VEI ?根拠の記載なし
    1920-07-02 ~ 終了日不明
    South flank (Andrew's Volcano)
  3. 1917年VEI 2観測記録
    1917-07-02 ~ 終了日不明
    Andrew's or Teleki's Volcanoes
  4. 1906年VEI ?根拠の記載なし
    1906-07-02 ~ 終了日不明
    Andrew's or Teleki's Cones
  5. 1897年VEI 2観測記録
    1897-05-16 ~ 終了日不明
    North flank (Teleki) and Likaiu
  6. 1895年VEI 2観測記録
    1895-07-02 ~ 終了日不明
    North flank (Teleki's Cone)
  7. 1888年VEI 0観測記録
    1888-07-02 ~ 終了日不明
    North flank (Teleki's Cone)
  8. 1871年 (±3年)VEI 2観測記録
    1871-07-02 ~ 終了日不明
    North flank (Teleki's Cone)
  9. 1090年 (±50年)VEI 0地質学的推定
    1090 ~ 終了日不明
    North flank
  10. 1050年 (±150年)VEI 0地質学的推定
    1050 ~ 終了日不明
    North flank
  11. 1030年 (±150年)VEI 0地質学的推定
    1030 ~ 終了日不明
    North flank
  12. 紀元前 7710年 (±200年)VEI ?地質学的推定
    紀元前 7710 ~ 終了日不明
    North (Abili Agituk) and south flanks

近くの火山

外部リンク

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