グレーシャーピーク山
Glacier Peak
成層火山 · United States · 3213m

- タイプ
- 成層火山
- 国
- United States
- 地域
- North America Volcanic Regions / Garibaldi Volcanic Arc
- 標高
- 3213m
- 座標
- 48.112, -121.113
- 最終噴火
- 1700年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Dacite
地質学的概要
Glacier Peak, the most isolated of the Cascade volcanoes, rises above the rugged forested terrain of the Glacier Peak Wilderness Area in the North Cascades. This dacitic-andesitic stratovolcano with summit and flank lava domes resembles St. Helens in its explosive vigor. More than a dozen glaciers descend its flanks, prompting its name. Although its summit towers above surrounding valleys, the volcano was constructed above a high ridge and is itself less than 1,000 m high. Repeated major explosive eruptions associated with lava dome growth during the late Pleistocene and Holocene deposited tephra over wide distances to the east. Voluminous pyroclastic flows and mudflows extended into the Puget Sound lowlands to the west and diverted several river courses into adjacent valleys. The latest eruption only a few hundred years ago was noted by indigenous Pacific Northwest Indians, and hot springs occur on its flanks.
Wikipedia の要約
英語版の要約Glacier Peak or Dakobed is a stratovolcano in the U.S state of Washington. Located in the Glacier Peak Wilderness in Mount Baker–Snoqualmie National Forest, the volcano is visible from the west in Seattle, and from the north in the higher areas of eastern suburbs of Vancouver such as Coquitlam, New Westminster and Port Coquitlam. The volcano is the fourth tallest peak in Washington state and the most isolated volcano of the Cascade Volcanic Arc.
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噴火履歴
詳細タイムライン
- 1700年 (±100年)VEI 2地質学的推定1700 ~ 進行中
- 1300年 (±300年)VEI ?地質学的推定1300 ~ 進行中
- 900年 (±50年)VEI 3地質学的推定900 ~ 進行中
- 200年 (±50年)VEI 4地質学的推定200 ~ 進行中
- 紀元前 850年VEI ?地質学的推定BCE 850 ~ 進行中
- 紀元前 3150年VEI ?地質学的推定BCE 3150 ~ 進行中
- 紀元前 3550年VEI ?地質学的推定BCE 3550 ~ 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。