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El Salvador · Stratovolkan

Cordillera de Apaneca-Lamatepec

Apaneca Range

Tipe
Stratovolkan
Ketinggian
2028 m
Letusan terakhir
Tidak diketahui
Cordillera de Apaneca-Lamatepec
Foto: Lee Siebert, Smithsonian Institution · Public domain · Wikimedia Commons
Tipe
Stratovolkan
Negara
El Salvador
Wilayah
Amerika Tengah & Karibia / Central America Volcanic Arc
Ketinggian
2028 m
Koordinat
13.872, -89.742
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

The Apaneca Range (also known as the Cuyanausul Range) consists of a group of basaltic-to-andesitic Pleistocene and Holocene stratovolcanoes in western El Salvador between the Santa Ana complex and the Guatemala border. The Pleistocene dacitic-rhyolitic Concepción de Ataco caldera (5 x 3.5 km) lies at the W end of the complex, along with post-caldera late-Pleistocene to Holocene andesitic-dacitic lava domes. The post-caldera cones of Cerro el Aguila (the highest peak of the complex) and Cerro los Naranjos at the E end of the chain were mapped as Holocene by Weber and Weisemann (1978). Young craters on the basaltic Cerro Laguna Verde stratovolcano may also have been active during the Holocene. Numerous fumarole fields are located on the N flank of the range, and the Ahuachapán geothermal field has been producing since 1975. Several small hydrothermal explosions have occurred in historical time, including one in October 1990 at the Agua Shuca thermal area in which 26 people were killed.

Ringkasan Wikipedia

Ringkasan Inggris

Cordillera de Apaneca is a volcanic mountain range in western El Salvador. It consists mainly of volcanoes. Ilamatepec volcano, one of the most active in the region, is a part of this range.

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