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Resago

Resago, Volcan

Kerucut piroklastik · Chile · 1890 m

The crescent-shaped lake at the top-center of this NASA International Space Station image (with north to the bottom right) is Laguna del Dial.  A cinder cone named Volcán Resago, on the SE side of the lake, produced a basaltic andesite lava flow that traveled about 3 km to the WNW into Laguna Dial.  The youthful cone may have been formed during an undocumented eruption during historical time.  The lake at the lower left is Laguna Valvarco.
The crescent-shaped lake at the top-center of this NASA International Space Station image (with north to the bottom right) is Laguna del Dial. A cinder cone named Volcán Resago, on the SE side of the lake, produced a basaltic andesite lava flow that traveled about 3 km to the WNW into Laguna Dial. The youthful cone may have been formed during an undocumented eruption during historical time. The lake at the lower left is Laguna Valvarco. · Foto: NASA International Space Station image ISS008-E-7432, 2003 (http://eol.jsc.nasa.gov/).
Tipe
Kerucut piroklastik
Negara
Chile
Wilayah
South America Volcanic Regions / Southern Andean Volcanic Arc
Ketinggian
1890 m
Koordinat
-36.461, -70.903
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Minor (Basaltic)
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

Volcán Resago, in the Linares province of central Chile, is a cinder cone with a double crater. It produced a basaltic andesite lava flow that traveled ~3 km WNW into Laguna Dial. The youthful cone may have been formed during an undocumented Holocene eruption (González-Ferrán, 1995).

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Resago is a cinder cone in the Linares Province of Chile.

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