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Global Volcanism Program | Image GVP-07422

Cerro Juana Pancha, seen from the south near the Pan-American highway on the way to La Unión, is part of the Pleistocene Cerro Yayantique volcanic field.  Cerro Yayantique is the most prominent and least-eroded  feature in a broad area of Pleistocene volcanic rocks in the SE corner of El Salvador west of the NW arm of the Gulf of Fonseca.  An E-W-trending area of smaller Pleistocene volcanic cones to the NE straddles both sides of the Río Amatillo Sirama. Photo by Giuseppina Kysar, 1999 (Smithsonian Institution).

Cerro Juana Pancha, seen from the south near the Pan-American highway on the way to La Unión, is part of the Pleistocene Cerro Yayantique volcanic field. Cerro Yayantique is the most prominent and least-eroded feature in a broad area of Pleistocene volcanic rocks in the SE corner of El Salvador west of the NW arm of the Gulf of Fonseca. An E-W-trending area of smaller Pleistocene volcanic cones to the NE straddles both sides of the Río Amatillo Sirama.

Photo by Giuseppina Kysar, 1999 (Smithsonian Institution).

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Cerro Yayantique