ベルクナップ・クレーター
Belknap
楯状火山 · United States · 2094m

- タイプ
- 楯状火山
- 国
- United States
- 地域
- North America Volcanic Regions / High Cascades Volcanic Arc
- 標高
- 2094m
- 座標
- 44.285, -121.842
- 最終噴火
- 475年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
The Belknap Crater area near McKenzie Pass in Oregon, north of the Three Sisters volcanoes, was the source of one of the largest concentrations of youthful volcanism in the Cascade Range. The basaltic to basaltic andesite Belknap shield volcano, topped by the Belknap Crater pyroclastic cone and the Little Belknap shield volcano immediately to the east, have produced widespread late Holocene lava flows on all sides, much of which took place between about 3,000 and 1,500 years ago. Eruptions from the NE base of Belknap crater produced lava flows that traveled 15 km W into the McKenzie River valley.
Wikipedia の要約
英語版の要約Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness. Belknap is not forested and most of its lava flows are not vegetated, though there is some wildlife in the area around the volcano, as well as a number of tree molds formed by its eruptive activity.
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噴火履歴
詳細タイムライン
- 475年 (±215年)VEI 2地質学的推定475 ~ 進行中Belknap Crater
- 紀元前 685年 (±50年)VEI 2地質学的推定BCE 685 ~ 進行中South Belknap and Twin Craters
- 紀元前 1071年 (±241年)VEI 0地質学的推定BCE 1071 ~ 進行中Little Belknap
- 紀元前 5050年VEI ?地質学的推定BCE 5050 ~ 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。