スパー山
Spurr
成層火山 · United States · 3374m

- タイプ
- 成層火山
- 国
- United States
- 地域
- North America Volcanic Regions / Alaska Peninsula Volcanic Arc
- 標高
- 3374m
- 座標
- 61.299, -152.251
- 最終噴火
- 1992年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
Mount Spurr is the closest volcano to Anchorage, Alaska (130 km W) and just NE of Chakachamna Lake. The summit is a large lava dome at the center of a roughly 5-km-wide amphitheater open to the south formed by a late-Pleistocene or early Holocene debris avalanche and associated pyroclastic flows that destroyed an older edifice. The debris avalanche traveled more than 25 km SE, and the resulting deposit contains blocks as large as 100 m in diameter. Several ice-carved post-collapse cones or lava domes are present. The youngest vent, Crater Peak, formed at the southern end of the amphitheater and has been the source of about 40 identified Holocene tephra layers. Eruptions from Crater Peak in 1953 and 1992 deposited ash in Anchorage.
Wikipedia の要約
英語版の要約Mount Spurr (Dena'ina: K'idazq'eni) is a stratovolcano in the Aleutian Arc of Alaska, named after United States Geological Survey geologist and explorer Josiah Edward Spurr, who led an expedition to the area in 1898. The Alaska Volcano Observatory (AVO) rates Mount Spurr as Level of Concern Color Code Yellow. The mountain is known aboriginally by the Dena'ina Athabascan name K'idazq'eni, literally 'that which is burning inside'.
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噴火履歴
詳細タイムライン
- 1992年VEI 4観測記録1992-06-27 ~ 1992-09-17South flank (Crater Peak)
- 1953年VEI 4観測記録1953-07-09 ~ 1953-07-16South flank (Crater Peak)
- 1650年 (±50年)VEI ?地質学的推定1650 ~ 進行中South flank (Crater Peak)
- 紀元前 3250年VEI ?地質学的推定BCE 3250 ~ 進行中Mt. Spurr central lava/cone complex
- 紀元前 4050年VEI ?地質学的推定BCE 4050 ~ 進行中South flank (Crater Peak)
- 紀元前 5110年 (±100年)VEI ?地質学的推定BCE 5110 ~ 進行中Mt. Spurr central dome/cone complex
- 紀元前 6050年VEI ?地質学的推定BCE 6050 ~ 進行中Mt. Spurr central dome/cone complex
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。