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エクアドル · 火砕丘

Licto volcanic field

Licto

タイプ
火砕丘
標高
3322m
最終噴火
不明
Cerro Tulabug (right-center), part of the Licto group of basaltic andesite to andesitic scoria cones, is seen here from the SW.  The cones lie along the Río Chambo about 25 km SE of the city of Riobamba and just north of the town of Licto and form the southernmost area of Quaternary volcanism in the Interandean valley of Ecuador.  The cloud-draped conical volcano in the left-center background is Reventador, and the Cordillera Real forms the right horizon.
Cerro Tulabug (right-center), part of the Licto group of basaltic andesite to andesitic scoria cones, is seen here from the SW. The cones lie along the Río Chambo about 25 km SE of the city of Riobamba and just north of the town of Licto and form the southernmost area of Quaternary volcanism in the Interandean valley of Ecuador. The cloud-draped conical volcano in the left-center background is Reventador, and the Cordillera Real forms the right horizon. · 写真: Photo by Patricio Ramon, 1998 (Instituto Geofisca, Escuela Politecnica Nacional).
タイプ
火砕丘
国
エクアドル
地域
南アメリカ / Northern Andean Volcanic Arc
標高
3322m
座標
-1.786, -78.614
最終噴火
不明
テクトニクス環境
沈み込み帯 / 大陸地殻 (> 25 km)
火山地形
小規模 (玄武岩質)
主要岩石
安山岩 / 玄武岩質安山岩
地質学的概要

The Licto group of scoria cones lies along the Río Chambo ~25 km SE of the city of Riobamba and just north of the town of Licto. These three basaltic andesite to andesitic cones form the southernmost area of Quaternary volcanism in the Interandean valley of Ecuador. The Cerro Tulabug cone is the largest, with Loma Bellavista ~2 km SE and Licto, the smallest, ~1 km down the WNW flank. The group was considered to be of late Pleistocene or Holocene age (Hall, 1987, pers. comm; Eissen, 2006, pers. comm.) based on the relatively youthful morphology of the cones.

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Licto is a volcanic field in Ecuador, close to the town of Licto.

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