Tata Sabaya
Stratovulcano · Bolivia · 5430 m

- Tipo
- Stratovulcano
- Paese
- Bolivia
- Regione
- South America Volcanic Regions / Central Andean Volcanic Arc
- Altitudine
- 5430 m
- Coordinate
- -19.130, -68.530
- Ultima eruzione
- Sconosciuto
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Andesite / Basaltic Andesite
Sintesi geologica
The symmetrical Tata Sabaya towers above the northern end of the Salar de Coipasa in the Altiplano of Bolivia. A pyroclastic shield capped by lava domes was topped by effusive eruptions that formed the unglaciated andesitic stratovolcano. Collapse of this edifice produced a large late-Pleistocene debris avalanche that swept into the Salar de Coipasa and covered an area of more than 300 km2 S of the volcano, traveling up to 30 km. Tufa deposits on avalanche hummocks correspond to a ~12,000 year old high stand of the lake. Renewed eruptions during the Holocene constructed lava domes and flows that have restored much of the original edifice. Youthful lava flows extend down the NW and W flanks, and pyroclastic-flow deposits from partial collapse of the summit dome extend to the lower SW flank.
Sintesi da Wikipedia
Riassunto in ingleseTata Sabaya is a 5,430-metre (17,810 ft) high volcano in Bolivia. It is part of the Central Volcanic Zone, one of several volcanic belts in the Andes which are separated by gaps without volcanic activity. This section of the Andes was volcanically active since the Jurassic, with an episode of strong ignimbritic volcanism occurring during the Miocene. Tata Sabaya lies in a thinly populated region north of the Salar de Coipasa salt pan.
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Storia delle eruzioni
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