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El Salvador · Stratovolkan

Usulután

Usulutan

Tipe
Stratovolkan
Ketinggian
1449 m
Letusan terakhir
Tidak diketahui
Usulután
Foto: Lee Siebert, Smithsonian Institution · Public domain · Wikimedia Commons
Tipe
Stratovolkan
Negara
El Salvador
Wilayah
Amerika Tengah & Karibia / Central America Volcanic Arc
Ketinggian
1449 m
Koordinat
13.419, -88.471
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

Usulután volcano anchors the SE end of a cluster of basaltic to basaltic andesite stratovolcanoes between San Vicente and San Miguel volcanoes. The flanks of the forested volcano are dissected, but youthful lava flows are present on its southern flanks. The younger summit rocks of Usulután and the Cerro Nanzal pyroclastic cone on the lower SE flank were mapped as Holocene (Weber and Wiesemann, 1978). A broad 1.3-km-wide crater is breached to the E from the summit to its lower flank.

Ringkasan Wikipedia

Ringkasan Inggris

Usulután is a stratovolcano in central El Salvador, rising above the coastal plain between the San Vicente and San Miguel volcanoes, and just east of Taburete volcano. The volcano is topped by a 1.3 kilometres (0.8 mi) wide summit crater which is breached to the east.

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