The role of dyking and fault control in the rapid onset of eruption at Chaitén Volcano, Chile

By: , and 



Rhyolite is the most viscous of liquid magmas, so it was surprising that on 2 May 2008 at Chaitén Volcano, located in Chile’s southern Andean volcanic zone, rhyolitic magma migrated from more than 5 km depth in less than 4 hours and erupted explosively with only two days of detected precursory seismic activity. The last major rhyolite eruption before that at Chaitén was the largest volcanic eruption in the twentieth century, at Novarupta volcano, Alaska, in 1912. Because of the historically rare and explosive nature of rhyolite eruptions and because of the surprisingly short warning before the eruption of the Chaitén volcano, any information about the workings of the magmatic system at Chaitén, and rhyolitic systems in general, is important from both the scientific and hazard perspectives. Here we present surface deformation data related to the Chaitén eruption based on radar interferometry observations from the Japan Aerospace Exploration Agency (JAXA) DAICHI (ALOS) satellite. The data on this explosive rhyolite eruption indicate that the rapid ascent of rhyolite occurred through dyking and that melt segregation and magma storage were controlled by existing faults.

Study Area

Publication type Article
Publication Subtype Journal Article
Title The role of dyking and fault control in the rapid onset of eruption at Chaitén Volcano, Chile
Series title Nature
DOI 10.1038/nature10541
Volume 478
Issue 7369
Year Published 2011
Language English
Contributing office(s) Earthquake Science Center
Description 4 p.
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Nature
First page 374
Last page 377
Country Chile
Other Geospatial Chait�n Volcano
Google Analytic Metrics Metrics page
Additional publication details