Largest explosive eruption in historical times in the Andes at Huaynaputina volcano, A.D. 1600, southern Peru

Citation
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
Citations number
11
Categorie Soggetti
Earth Sciences
Journal title
GEOLOGY
ISSN journal
00917613 → ACNP
Volume
27
Issue
5
Year of publication
1999
Pages
435 - 438
Database
ISI
SICI code
0091-7613(199905)27:5<435:LEEIHT>2.0.ZU;2-3
Abstract
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.