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Resago

Resago, Volcan

火砕丘 · Chile · 1890m

The crescent-shaped lake at the top-center of this NASA International Space Station image (with north to the bottom right) is Laguna del Dial. A cinder cone named Volcán Resago, on the SE side of the lake, produced a basaltic andesite lava flow that traveled about 3 km to the WNW into Laguna Dial. The youthful cone may have been formed during an undocumented eruption during historical time. The lake at the lower left is Laguna Valvarco.
The crescent-shaped lake at the top-center of this NASA International Space Station image (with north to the bottom right) is Laguna del Dial. A cinder cone named Volcán Resago, on the SE side of the lake, produced a basaltic andesite lava flow that traveled about 3 km to the WNW into Laguna Dial. The youthful cone may have been formed during an undocumented eruption during historical time. The lake at the lower left is Laguna Valvarco. · 写真: NASA International Space Station image ISS008-E-7432, 2003 (http://eol.jsc.nasa.gov/).
タイプ
火砕丘
国
Chile
地域
South America Volcanic Regions / Southern Andean Volcanic Arc
標高
1890m
座標
-36.461, -70.903
最終噴火
不明
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Minor (Basaltic)
主要岩石
Andesite / Basaltic Andesite
地質学的概要

Volcán Resago, in the Linares province of central Chile, is a cinder cone with a double crater. It produced a basaltic andesite lava flow that traveled ~3 km WNW into Laguna Dial. The youthful cone may have been formed during an undocumented Holocene eruption (González-Ferrán, 1995).

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Resago is a cinder cone in the Linares Province of Chile.

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