Mount Andrus
Andrus
楯状火山 · Antarctica · 2978m

- タイプ
- 楯状火山
- 国
- Antarctica
- 地域
- Antarctic-Scotia Volcanic Regions / Western Antarctica Volcanic Province
- 標高
- 2978m
- 座標
- -75.800, -132.330
- 最終噴火
- 不明
- テクトニクス環境
- Intraplate / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Trachyte / Trachydacite
地質学的概要
Three coalescing trachytic shield volcanoes with a combined volume of 252 km3 formed during the Miocene along a N-S line in the Ames Range of western Marie Byrd Land. The youngest and best exposed is Mount Andrus, the southernmost volcano, where late-stage volcanic activity resumed during the late-Pleistocene or Holocene (Gonzalez-Ferran and Gonzalez-Bonorino 1972, LeMasurier and Thomson 1990). A distinct 4.5-km-wide caldera truncates the summit of Mount Andrus. Weak fumarolic activity was observed in 1977 at Mount Kauffman, the northernmost volcano, which also has a morphologically distinct 3-km-wide summit caldera.
Wikipedia の要約
英語版の要約Mount Andrus is a peak 2 nautical miles southeast of Mount Boennighausen in the southeast extremity of the Ames Range, in Marie Byrd Land, Antarctica.
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噴火履歴
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噴火記録はありません。
外部リンク
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