グラシオーザ島
Graciosa
成層火山 · Portugal · 402m

- タイプ
- 成層火山
- 国
- Portugal
- 地域
- 大西洋 / Azores-Terceira Rift Volcanic Province
- 標高
- 402m
- 座標
- 39.020, -27.970
- 最終噴火
- -1950年
- テクトニクス環境
- Rift zone / Oceanic crust (< 15 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The SE end of Graciosa, the northernmost of the central Azorean islands, contains a 0.9 x 1.6 km caldera with active fumaroles. The SE caldera rim is the high point of the 7 x 12 km island. The caldera has been the source of eruptions producing significant tephra falls, pyroclastic flows, lahars, and lava flows. Fumaroles are present in a volcanic cave inside the caldera, and a submarine fumarole occurs off the NW coast. Scoria cones erupted along several widely spaced NE-SW-trending fissures fed a youthful lava field that forms the NW end of the island. The most recent eruption from Pico Tomao, NW of the caldera, produced a lava flow during the mid-to-late Holocene that reached the eastern coast NW of the village of Praia.
Wikipedia の要約
英語版の要約Graciosa Island, also referred to as the White Island, is a volcanic island in the Atlantic Ocean. It is the northernmost of the Central Group of islands in the Azores archipelago. The ovular Portuguese island has an area of 60.65 square kilometres, a length of 10 kilometres and a width of 7 kilometres. Its landscape is dominated by a 1.6-kilometre-wide (1.0-mile) central caldera located in the southeast.
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噴火履歴
詳細タイムライン
- 紀元前 1950年 (±1400年)VEI ?地質学的推定BCE 1950 ~ 進行中San Tamao
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。