Jc. Thouret et al., Largest explosive eruption in historical times in the Andes at Huaynaputina volcano, A.D. 1600, southern Peru, GEOLOGY, 27(5), 1999, pp. 435-438
The largest explosive eruption (volcanic explosivity index of 6) in histori
cal times in the Andes took place in A.D. 1600 at Huaynaputina volcano in s
outhern Peru, According to chronicles, the eruption began on February 19 wi
th a Plinian phase and lasted until March 6, Repeated tephra falls, pyrocla
stic flows, and surges devastated an area 70 x 40 km(2) west of the vent an
d affected all of southern Peru, and earthquakes shook the city of Arequipa
75 km away. Eight deposits, totaling 10.2-13.1 km(3) in bulk volume, are a
ttributed to this eruption: (1) a widespread, similar to 8.1 km(3) pumice-f
all deposit; (2) channeled ignimbrites (1.6-2 km(3)) with (3) ground-surge
and ash-cloud-surge deposits; (4) widespread co-ignimbrite ash layers; (5)
base-surge deposits; (6) unconfined ash-flow deposits; (7) crystal-rich dep
osits; and (8) late ash-fall and surge deposits. Disruption of a hydrotherm
al system and hydromagmatic interactions are thought to have fueled the lar
ge-volume explosive eruption. Although the event triggered no caldera colla
pse, ring fractures that cut the vent area point to the onset of a funnel-t
ype caldera collapse.