メキシコ · 成層火山
Sangangüey
Sanganguey
- タイプ
- 成層火山
- 標高
- 2340m
- 最終噴火
- 不明

- タイプ
- 成層火山
- 国
- メキシコ
- 地域
- 中央アメリカ・カリブ海 / Trans-Mexican Volcanic Arc
- 標高
- 2340m
- 座標
- 21.450, -104.730
- 最終噴火
- 不明
- テクトニクス環境
- 沈み込み帯 / 大陸地殻 (> 25 km)
- 火山地形
- 複成火山
- 主要岩石
- 安山岩 / 玄武岩質安山岩
地質学的概要
Volcán Sangangüey, the highest volcano of the NW-SE-trending Tepic-Zacoalco graben, is an eroded andesitic and dacitic stratovolcano that contains a prominent lava spine at its summit. The NW and SE flanks of the Pleistocene edifice have 45 cinder cones that erupted during the past 300,000 years along five parallel lines. Some of the cinder cones appear morphologically similar to cones on nearby Ceboruco volcano that are known to be less than 1,000 years old. There are no confirmed historical eruptions from Sangangüey. An incorrect report of an eruption in 1859 from San Juan (a synonym of Sangangüey) refers to the nearby Pleistocene San Juan volcano. An native tradition records an eruption in 1742 (Sapper, 1917), which may refer to activity from one of the flank cinder cones.
Wikipedia の要約
英語版の要約Sangangüey is an eroded stratovolcano standing 2340 meters tall in the Trans-Mexican Volcanic Belt of Mexico. The volcano is located immediately southeast of Tepic in the state of Nayarit in Mexico. There has been no confirmed historical eruptions, and the volcano is believed to be dormant; although an indigenous legend recorded the volcano erupting in 1742. The eruption is believed to be one occurring on a flank cinder cone on the volcano. Within the last 300,000 years however, the volcano has produced 45 cinder cones and lava flows.
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噴火履歴
1件の記録用語集詳細タイムライン
- 1742年VEI ?根拠の記載なし1742 ~ 終了日不明
近くの火山
外部リンク
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