West Crater
火山原 · United States · 1329m

- タイプ
- 火山原
- 国
- United States
- 地域
- North America Volcanic Regions / High Cascades Volcanic Arc
- 標高
- 1329m
- 座標
- 45.880, -122.080
- 最終噴火
- -5750年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Cluster
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
West Crater, a small andesitic lava dome with associated lava flows, is part of a Quaternary volcanic field in southern Washington consisting primarily of small basaltic and basaltic andesite cinder cones and shield volcanoes, oriented along a NW-SE zone to the SE of St. Helens. This 20-km-wide zone extends from Marble Mountain, north of Swift Reservoir, to south of Trout Creek Hill. The Pleistocene basaltic Trout Creek Hill shield volcano produced a lava flow about 340,000 years ago that traveled 20 km SE, temporarily damming the Columbia River. At least three vents in this field are of Holocene age: West Crater, a small cone at Hackamore Creek, and a phreatic crater at the summit of Bare Mountain. The latest eruptions at these locations have been dated at about 8,000 years before present, and have included emplacement of an andesitic lava dome and associated lava flow at West Crater and formation of a phreatic explosion crater at Bare Mountain.
Wikipedia の要約
英語版の要約West Crater is a small lava dome with associated lava flows in southern Washington, United States. Located in Skamania County, it rises to an elevation of 4,131 feet (1,259 m), and forms part of the Cascade Volcanic Arc. It is also part of the Marble Mountain-Trout Creek Hill volcanic field, a little-known Quaternary volcanic field in the southern Cascades of Washington state. The area can be hiked, and can be accessed by roads in the Gifford Pinchot National Forest.
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噴火履歴
詳細タイムライン
- 紀元前 5750年VEI 2地質学的推定BCE 5750 ~ 進行中Bare Mountain
- 紀元前 6110年VEI 2地質学的推定BCE 6110 ~ 進行中West Crater, Hackamore Creek cone
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。