Aerial view of the active volcano Sabancaya (foreground) and the dormant volcano Ampato (background) from the northeast.
|Elevation||5,976 m (19,606 ft)|
|Prominence||~ 500 m (1,600 ft)|
|Volcanic arc/belt||Central Volcanic Zone|
Sabancaya is an active 5,976-metre (19,606 ft) stratovolcano in the Andes of southern Peru, about 100 kilometres (62 mi) northwest of Arequipa. It is the most active volcano in Peru and is part of a 20-kilometre (12 mi) north-south chain of three major stratovolcanoes, including the extinct and eroded 6,025 metres (19,767 ft) high volcano Wallqa Wallqa at the northern end, the dormant 6,288 metres (20,630 ft) high volcano Ampato to the south, and Sabancaya in the middle. Sabancaya hosts several glaciers which cover an area of about 3.5 square kilometres (1.4 sq mi) and descend as low as 5,400 metres (17,700 ft) on its flanks.
Volcanic activity 
The andesite stratovolcano of Sabancaya has been very active during historic times, with the earliest recorded eruptions in 1695 and 1758 (other sources list 1750 and 1784 as possible eruptions, too). Following over 200 years of dormancy, satellites detected an increase in thermal emission in July 1986 and intense activity resumed in December of that year, with several eruptive cycles over the next two years producing a lava dome in the crater.
The most sustained period of activity began with explosive eruptions on May 28, 1990, and continued for over eight years. The eruptive cycle rated a VEI of 3, with more than 25 million cubic metres (880×106 cu ft) of lava flows and tephra produced over that period. At the height of the activity in 1994, eruptions producing large ash clouds occurred every two hours. Although published topographic maps have not been revised since the eruptive cycyle, it is suspected that the cone may have grown to just over 6,000 metres (20,000 ft) during that time. Additional smaller eruptions occurred in 2000 and 2003.
Volcanic hazards 
Sabancaya is considered one of the most hazardous volcanoes in Peru, along with the massive Coropuna and the cone of El Misti near Arequipa. As of the mid-1990s, over 8,000 people lived in the valleys draining the flanks of the volcano. Potential hazards include lahars and pyroclastic flows down the Majes, Colca, and Siguas river drainages. During the 1988 eruption, cattle died in nearby areas either directly from poisonous volcanic gases or from eating contaminated vegetation.
See also 
- Biggar, p. 154
- Da Silva, p. 27
- "Sabancaya". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1504-006.
- De Silva, Shanaka L.; Francis, Peter (1991). Volcanoes of the Central Andes. Springer-Verlag. pp. 216 pp. ISBN 3-540-53706-6.
- González-Ferrán, Oscar (1995). Volcanes de Chile. Santiago, Chile: Instituto Geográfico Militar. pp. 640 pp. ISBN 956-202-054-1. (in Spanish; also includes volcanoes of Argentina, Bolivia, and Peru)
- Biggar, John (2005). The Andes: A Guide for Climbers (3rd ed.). Andes Publishing (Scotland). pp. 304 pp. ISBN 0-9536087-2-7.