El Misti
Summit Elevation: 5822 m
Latitude: 16.294°S
Longitude: 71.409°W
El Misti, Peru's most well-known volcano, is a
symmetrical andesitic stratovolcano with nested
summit craters that towers above the city of Arequipa.
The modern symmetrical cone, constructed within a
small 1.5 x 2 km wide summit caldera that formed
between about 13,700 and 11,300 years ago, caps older
Pleistocene volcanoes that underwent caldera collapse
about 50,000 years ago. A large scoria cone has grown
with the 830-m-wide outer summit crater of El Misti.
At least 20 tephra-fall deposits and numerous
pyroclastic-flow deposits have been documented
during the past 50,000 years, including a pyroclastic
flow that traveled 12 km to the south about 2000 years
ago. El Misti's most recent activity has been dominantly pyroclastic, and strong winds have formed a
parabolic dune field of volcanic ash extending up to 20 km downwind. An eruption in the 15th century
affected Inca inhabitants living near the volcano. Some reports of historical eruptions may represent
increased fumarolic activity. (Global Volcanism Program)
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