ウキンレク・マール群
Ukinrek Maars
マール · United States · 91m

- タイプ
- マール
- 国
- United States
- 地域
- North America Volcanic Regions / Alaska Peninsula Volcanic Arc
- 標高
- 91m
- 座標
- 57.834, -156.520
- 最終噴火
- 1977年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Minor (Basaltic)
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Ukinrek Maars are two explosion craters that were created in an area without previous volcanic activity during a 10-day phreatomagmatic eruption March-April 1977. The basaltic maars were erupted through glacial deposits in the Bering Sea lowlands 1.5 km S of Becharof Lake and 12 km W of Peulik volcano; their location is related to the regional Bruin Bay fault. The elliptical West Maar, which was the first to form, is 105 x 170 m and 35 m deep. The other maar, 600 m to the east, is 300 m wide and 70 m deep. Both maars are now filled by crater lakes; the eastern lake encircles a 49-m-high lava dome that was emplaced at the end of the eruption. Base surges were directed primarily to the NW. Juvenile material from the Ukinrek eruptions was of mantle-derived olivine basaltic composition. The dacitic Gas Rocks lava domes, of Quaternary age, are located on the shores of Becharof Lake, 3 km N of Ukinrek maars and were the site of a phreatic eruption about 2,300 years ago.
Wikipedia の要約
英語版の要約The Ukinrek maars are two volcanic craters on the north side of the Aleutian Range in Alaska that were formed by a phreatomagmatic eruption in 1977. The maars are 1.5 km south of Becharof Lake and 12 km northwest of Peulik Volcano, on a low area of the range, bordering the Bering Sea. The western of the two is elliptical in shape and up to 170 m in diameter and 35 m deep. The other lies 600 m to the east and is circular and up to 300 m in diameter and 70 m deep. The east maar has a 49 m-high lava dome within its crater lake.
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噴火履歴
詳細タイムライン
- 1977年VEI 3観測記録1977-03-30 ~ 1977-04-09West and East Ukinrek Maars
- 紀元前 350年VEI ?地質学的推定BCE 350 ~ 進行中Gas Rocks
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。