サンチャゴ島
Santiago
楯状火山 · Ecuador · 920m

- タイプ
- 楯状火山
- 国
- Ecuador
- 地域
- 東太平洋 / Galapagos Hotspot Volcano Group
- 標高
- 920m
- 座標
- -0.220, -90.770
- 最終噴火
- 1906年
- テクトニクス環境
- Rift zone / Oceanic crust (< 15 km)
- 火山地形
- Shield
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The elongated shield volcano of Santiago Island, also known as San Salvador Island or James Island, has numerous scattered Holocene pyroclastic cones. Fresh-looking lava flows from these cones cover the flanks. The summit ridge, lined with a chain of NW-trending cinder and spatter cones, is located at the NW end of the island. Prominent flank tuff cones occur at the western and eastern coasts. The most recent activity has been concentrated at the NW and SE ends of the island. The pahoehoe lava flows at James and Sullivan Bays, on opposite ends of the island, were erupted in the past few hundred years. The James Bay flows were dated by fragments of marmalade pots left by buccaneers in 1684 that were subsequently embedded in the lava flows described by Charles Darwin in 1835.
Wikipedia の要約
英語版の要約Santiago Island is one of the Galápagos Islands. The island, which consists of two overlapping volcanoes, has an area of 585 square kilometers (226 mi2) and a maximum altitude of 907 meters (2,976 ft), atop the northwestern shield volcano. The volcano in the island's southeast erupted along a linear fissure and is much lower. The oldest lava flows on the island date back to 750,000 years ago.
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噴火履歴
詳細タイムライン
- 1904年VEI 0観測記録1904-07-02 ~ 1906-12-15SE flank
- 1897年VEI 0観測記録1897-07-02 ~ 進行中SE flank (Sullivan Bay?)
- 1759年 (±75年)VEI ?地質学的推定1759 ~ 進行中West flank (James Bay)
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。