アクタン山
Akutan
成層火山 · United States · 1303m

- タイプ
- 成層火山
- 国
- United States
- 地域
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- 標高
- 1303m
- 座標
- 54.134, -165.986
- 最終噴火
- 1992年
- テクトニクス環境
- Subduction zone / Intermediate crust (15-25 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Akutan contains a 2-km-wide caldera with a large cinder cone in the NE part of the caldera that has been the source of frequent explosive eruptions and occasional lava effusion that covers the caldera floor. An older, largely buried caldera was formed during the late Pleistocene or early Holocene. Two volcanic centers are located on the NW flank. Lava Peak is of Pleistocene age, and a cinder cone lower on the flank produced a lava flow in 1852 that extended the shoreline of the island and forms Lava Point. The 60-365 m deep younger caldera was formed during a major explosive eruption about 1,600 years ago and contains at least three lakes. A lava flow in 1978 traveled through a narrow breach in the north caldera rim almost to the coast. Fumaroles occur at the base of the caldera cinder cone, and hot springs are located NE of the caldera at the head of Hot Springs Bay valley and along the shores of Hot Springs Bay.
Wikipedia の要約
英語版の要約Mount Akutan, officially Akutan Peak, is a stratovolcano in the Aleutian Islands of Alaska. Akutan Peak, at 4,275 feet (1,303 m), is the highest point on the caldera of the Akutan stratovolcano. Akutan contains a 2 km-wide caldera formed during a major explosive eruption about 1600 years ago. Recent eruptive activity has originated from a large cinder cone on the NE part of the caldera. It has been the source of frequent explosive eruptions with occasional lava effusion that blankets the caldera floor. A lava flow in 1978 traveled through a narrow breach in the north caldera rim to within 2 km of the coast. A small lake occupies part of the caldera floor. Two volcanic centers are located on the NW flank: Lava Peak is of Pleistocene age; and, a cinder cone lower on the flank which produced a lava flow in 1852 that extended the shoreline of the island and forms Lava Point. An older, mostly buried caldera seems to have formed in Pleistocene or Holocene time, while the current caldera formed in a VEI-5 eruption c. 340 AD. AVO has recorded 33 confirmed eruptions at Akutan, making it the volcano with the most eruptions in Alaska.
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噴火履歴
詳細タイムライン
- 1992年VEI 2観測記録1992-03-08 ~ 1992-05-21
- 1992年VEI 1観測記録1992-12-18 ~ 1992-12-18
- 1991年VEI 2観測記録1991-09-15 ~ 1991-10-29
- 1990年VEI 2観測記録1990-01-26 ~ 1990-01-26
- 1990年VEI 2観測記録1990-09-06 ~ 1990-10-01
- 1989年VEI 2観測記録1989-02-27 ~ 1989-03-28
- 1988年VEI 2観測記録1988-03-26 ~ 1988-07-20
- 1987年VEI 2観測記録1987-01-31 ~ 1987-06-24
- 1986年VEI 2観測記録1986-03-18 ~ 1986-06-30
- 1982年VEI 2観測記録1982-10-05 ~ 1983-05-16
- 1980年VEI 2観測記録1980-07-03 ~ 1980-07-08
- 1978年VEI 2観測記録1978-09-25 ~ 1978-10-16
- 1976年VEI 2観測記録1976-10-15 ~ 1977-05-09
- 1974年VEI 2観測記録1974-02-11 ~ 進行中West flank ?
- 1973年VEI 2観測記録1973-03-16 ~ 1973-05-16
- 1972年VEI 2地質学的推定1972-09-16 ~ 進行中
- 1962年VEI 2観測記録1962-11-05 ~ 進行中
- 1953年VEI 2観測記録1953-07-02 ~ 進行中
- 1951年VEI 2観測記録1951-10-16 ~ 進行中
- 1948年VEI 2観測記録1948-04-29 ~ 1948-08-07
- 1946年VEI 2観測記録1946-12 ~ 1947-01
- 1931年VEI 2観測記録1931-05 ~ 1931-08
- 1929年VEI 2観測記録1929-05 ~ 進行中
- 1927年VEI 2観測記録1927 ~ 1928
- 1912年VEI ?地質学的推定1912 ~ 進行中
- 1911年VEI 2観測記録1911 ~ 進行中
- 1908年VEI 0観測記録1908-02-22 ~ 進行中
- 1907年VEI ?観測記録1907 ~ 進行中
- 1896年VEI ?観測記録1896 ~ 進行中
- 1895年VEI 2観測記録1895-08-01 ~ 1895-08-14
- 1892年VEI 1観測記録1892-09-23 ~ 進行中
- 1887年VEI 0観測記録1887 ~ 進行中
- 1883年VEI 2観測記録1883 ~ 進行中
- 1867年VEI ?観測記録1867 ~ 進行中
- 1865年VEI ?観測記録1865 ~ 進行中
- 1862年VEI ?地質学的推定1862 ~ 進行中
- 1852年VEI ?観測記録1852 ~ 進行中NW flank (Lava Point)
- 1848年VEI 2観測記録1848-03-05 ~ 進行中
- 1845年VEI ?地質学的推定1845 ~ 進行中
- 1838年VEI ?地質学的推定1838 ~ 進行中
- 1828年VEI ?地質学的推定1828 ~ 進行中
- 1790年VEI ?地質学的推定1790 ~ 進行中
- 1420年 (±100年)VEI ?地質学的推定1420 ~ 進行中
- 550年VEI ?地質学的推定550 ~ 進行中
- 340年VEI 5地質学的推定340 ~ 進行中
- 紀元前 4150年VEI ?地質学的推定BCE 4150 ~ 進行中
- 紀元前 7620年 (±300年)VEI ?地質学的推定BCE 7620 ~ 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。