Jc. Thouret et al., CURRENT ACTIVITY OF THE NEVADO SABANCAYA STRATOVOLCANO (SOUTH PERU) -GEOLOGICAL FRAMEWORK AND VOLCANIC HAZARD-ZONE MAPPING, Bulletin de la Societe geologique de France, 165(1), 1994, pp. 49-63
The May 28, 1990, eruption of Nevado Sabancaya volcano (south volcanic
zone of Peru) ended a dormant stage of about 200 year duration. This
ice-clad stratovolcano still poses a threat to about 35,000 people and
to irrigated tilled land in the Rio Colca and Siguas valleys. This st
udy aims to develop a model for volcanic hazards appraisal and hazard-
zone mapping available for remote stratovolcanoes like Nevado Sabancay
a which lack geological information. The method is based on remote sen
sing using 5 SPOT images collected during 1990, geological and geomorp
hological survey of the summit volcano, and calculation of parameters
for tephra dispersal and pyroclastic flowage. Nevado Sabancaya is pote
ntially hazardous because it was active 200 years ago, and because it
is still ice-clad despite its three years of recent activity. In addit
ion, recent tephra-fall deposits on similar volcanoes in this area poi
nt to the occurrence of Plinian eruptions during the past 500 years. T
wo maps showing hazard zones for tephra fallout, pyroclastic flows, la
hars, and potentially catastrophic events are presented. Hazard zones
are portrayed according to three types of behaviour: moderate-magnitud
e vulcanian activity (e.g. june 1990-december 1992), violent explosive
activity, and a potentially paroxysmal Plinian event.