Cile · Stratovulcano
Palomo
- Tipo
- Stratovulcano
- Altitudine
- 4860 m
- Ultima eruzione
- Sconosciuto
- Tipo
- Stratovulcano
- Paese
- Cile
- Regione
- Sud America / Southern Andean Volcanic Arc
- Altitudine
- 4860 m
- Coordinate
- -34.608, -70.295
- Ultima eruzione
- Sconosciuto
- Contesto tettonico
- Zona di subduzione / Crosta continentale (> 25 km)
- Forma vulcanica
- Composito
- Roccia principale
- Andesite / Andesite basaltica
Sintesi geologica
Palomo is a small stratovolcano that is somewhat dissected by glaciers. A NE-flank cone, Andres, is postglacial in age and has produced andesitic lava flows. The volcano lies W of the massive Caldera del Atuel and was constructed within double calderas 3 and 5 km in diameter. The largely ice-covered volcano has erupted basaltic andesite to dacitic lava flows; the double crater indicates migration of activity to the NE. The youthful morphology suggests a very recent, perhaps pre-Hispanic, age.
Sintesi da Wikipedia
Riassunto in inglesePalomo is a 4,860 metres (15,940 ft) high Chilean stratovolcano located in the commune of Machali, Cachapoal province, Libertador General Bernardo O'Higgins Region, west of Caldera del Atuel. Together with Tinguiririca it is one of two volcanoes in the region with evidence of Holocene volcanism. The volcano is remote and knowledge on its geology and potential volcanic hazards is limited.
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