
Sabancaya
Sign in to saveSabancaya is an active stratovolcano in the Andes of southern Peru, about northwest of Arequipa. It is considered part of the Central Volcanic Zone of the Andes, one of the three distinct volcanic belts of the Andes. The Central Volcanic Zone includes a number of volcanoes, some of which, like Huaynaputina, have had large eruptions, and others, such as Sabancaya and Ubinas, have been active in historical time. Sabancaya forms a volcanic complex together with Hualca Hualca to the north and Ampato to the south and has erupted andesite and dacite. It is covered by a small ice cap, which leads to
Key facts
- Mountain.name
- Sabancaya
- Mountain.photo
- File:Volcan Sabancaya (meaning Tongue of Fire) (30031766090).jpg
- Mountain.photo_caption
- Aerial view of Sabancaya, the summit in the left background is Ampato
- Mountain.map
- Peru
- Mountain.map_caption
- Peru
- Mountain.location
- Southern Peru
- Mountain.label_position
- left
- Mountain.elevation_m
- 5960
- Mountain.prominence
- ~
- Mountain.range
- Andes
- Mountain.type
- Stratovolcano
- Mountain.volcanic_zone
- Central Volcanic Zone
- Mountain.last_eruption
- Ongoing since November 2016
- Mountain.first_ascent
- 1966
via Wikipedia infobox
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Encyclopedic overview
17 sectionsContents
- Name origin and first ascent
- Geography and geomorphology
- Regional
- Local
- Geology
- Composition
- Eruptive history
- Historical activity
- Seismicity
- Hazards
- Monitoring
- Hazard maps and scenarios
- Climate and vegetation
- Access and human use
- See also
- References
- Sources
Sabancaya is an active stratovolcano in the Andes of southern Peru, about northwest of Arequipa. It is considered part of the Central Volcanic Zone of the Andes, one of the three distinct volcanic belts of the Andes. The Central Volcanic Zone includes a number of volcanoes, some of which, like Huaynaputina, have had large eruptions, and others, such as Sabancaya and Ubinas, have been active in historical time. Sabancaya forms a volcanic complex together with Hualca Hualca to the north and Ampato to the south and has erupted andesite and dacite. It is covered by a small ice cap, which leads to a risk of lahars during eruptions.
Sabancaya has generated numerous long lava flows, especially during the early Holocene, while activity in the later Holocene has been more explosive. Historical reports indicate eruptions during the 18th century. The volcano returned to activity in 1986, culminating in a large eruption in 1990. Since then, it has been continuously active with the emission of ash and gas.
Excerpted from Wikipedia’s “Sabancaya” article, available under the CC BY-SA 4.0 licence.
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