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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
Sangangüey
写真: Christian Frausto Bernal · CC BY-SA 2.0 · Wikimedia Commons
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
概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます · 矢印キーで棒を移動、Enterで表示
1742~1742 · 1件 · 最大 VEI ?17421742174317431743

詳細タイムライン

  1. 1742年VEI ?根拠の記載なし
    1742 ~ 終了日不明

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