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Cerro Solo

Solo, El

成層火山 · Chile-Argentina · 6205m

Light-colored rhyodacitic pyroclastic-flow deposits blanket El Solo volcano in the Ojos del Salado area.  Snow partially mantles the summit of El Solo, a stratovolcano composed of nine eruptive centers located west of Nevados del Ojos de Salado and SE of Tres Cruces volcano.  The 6190-m-high El Solo volcano was the source of major pyroclastic-flow deposits erupted during the Holocene that thickly fill adjacent valleys.
Light-colored rhyodacitic pyroclastic-flow deposits blanket El Solo volcano in the Ojos del Salado area. Snow partially mantles the summit of El Solo, a stratovolcano composed of nine eruptive centers located west of Nevados del Ojos de Salado and SE of Tres Cruces volcano. The 6190-m-high El Solo volcano was the source of major pyroclastic-flow deposits erupted during the Holocene that thickly fill adjacent valleys. · 写真: Photo courtesy of Oscar González-Ferrán (University of Chile). · Wikimedia Commons
タイプ
成層火山
Chile-Argentina
地域
South America Volcanic Regions / Central Andean Volcanic Arc
標高
6205m
座標
-27.105, -68.713
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
Dacite
地質学的概要

El Solo is large stratovolcano composed of nine eruptive centers located west of Nevados del Ojos de Salado and SE of Tres Cruces volcano. The 6205-m-high volcano was the source of major rhyodacitic pyroclastic-flow deposits erupted during the Holocene that thickly fill adjacent valleys (González-Ferrán, 1995).

Wikipedia の要約

英語版の要約

Cerro Solo is a large stratovolcano on the border between Argentina and Chile, west of Ojos del Salado with an elevation of 6,215 metres (20,390 ft) metres. It consists of nine eruptive centers and is covered in light-colored rhyodacite pyroclastic flow deposits.

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