Cile · Kaldera
Laguna del Maule
Maule, Laguna del
- Tipe
- Kaldera
- Ketinggian
- 2162 m
- Letusan terakhir
- -50

- Tipe
- Kaldera
- Negara
- Cile
- Wilayah
- Amerika Selatan / Southern Andean Volcanic Arc
- Ketinggian
- 2162 m
- Koordinat
- -36.058, -70.492
- Letusan terakhir
- -50
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Kaldera
- Batuan utama
- Andesit / Andesit basaltik
Ringkasan geologi
The Laguna del Maule volcanic complex includes a 15 x 25 km caldera with a cluster of small stratovolcanoes, lava domes, and pyroclastic cones of Pleistocene-to-Holocene age. The caldera lies mostly on the Chilean side of the border, but partially extends into Argentina. Fourteen Pleistocene basaltic lava flows were erupted down the upper part of the Maule river valley. A cluster of Pleistocene cinder cones was constructed on the NW side of Maule lake in the northern part of the caldera. The latest activity produced an explosion crater on the E side of the lake and a series of Holocene rhyolitic lava domes and blocky lava flows that surround it.
Ringkasan Wikipedia
Ringkasan InggrisLaguna del Maule is a volcanic field in the Andes mountain range of Chile, close to, and partly overlapping, the Argentina–Chile border. The bulk of the volcanic field is in the Talca Province of Chile's Maule Region. It is a segment of the Southern Volcanic Zone, part of the Andean Volcanic Belt. The volcanic field covers an area of 500 km2 (190 sq mi) and features at least 130 volcanic vents. Volcanic activity has generated cones, lava domes, lava coulees and lava flows, which surround the Laguna del Maule lake. The field gets its name from the lake, which is also the source of the Maule River.
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Riwayat letusan
4 tercatatGlosariumGaris waktu rinci
- 50 SMVEI 0Perkiraan geologi50 SM – akhir tidak diketahui
- 250 SMVEI 0Perkiraan geologi250 SM – akhir tidak diketahui
- 1550 SMVEI 0Perkiraan geologi1550 SM – akhir tidak diketahui
- 4450 SMVEI 0Perkiraan geologi4450 SM – akhir tidak diketahui
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