チナメカ
Chinameca
成層火山 · El Salvador · 1300m

- タイプ
- 成層火山
- 国
- El Salvador
- 地域
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- 標高
- 1300m
- 座標
- 13.478, -88.330
- 最終噴火
- 不明
- 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
The small Chinameca stratovolcano (also known as El Pacayal) lies across a low saddle abotu 7 km NW of the large San Miguel volcano. A 2-km-wide, steep-sided caldera, Laguna Seca el Pacayal, truncates the summit, whose flanks are covered with coffee plantations. The Holocene cone of Cerro el Limbo on the W flank rises above the level of the caldera rim, and a Holocene lava flow extends from a NNW-flank vent into the lowlands to the N beyond the town of Chinameca (Weber and Weisemann, 1978). A group of fumarole fields on the N flank surrounds the city of Chinameca, and the volcano has been the site of a geothermal exploration program.
Wikipedia の要約
英語版の要約Chinameca is a stratovolcano in central-eastern El Salvador. It lies north of San Miguel volcano and rises over the town of Chinameca. The volcano is topped by a 2 kilometres (1.2 mi) wide caldera known as Laguna Seca el Pacayal, and a satellite cone on the west side, Cerro el Limbo, rises higher than the caldera rim. Fumaroles can be found on the north side, and it has been the site of a geothermal exploration program.
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噴火履歴
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