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Titel One Mother Two DADs: the two fault-related avalanches of Iriga, Philippines
VerfasserIn Engielle Mae Paguican, Alfredo Mahar Francisco Mahar, Benjamin van Wyk de Vries
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250048556
 
Zusammenfassung
Volcanic rock-slidedebris avalanches are low-frequency, high-volume events generated by volcanic sector collapse that begins as a rock-slide and progressively disintegrates on steep edifice slopes. They are linked to edifice instability and a triggering mechanism, related either to a volcanic event, extreme rainfall or tectonic movement. The case of the Iriga debris avalanche with a volume of 1.5 km2 and runout length of about 10 km has long been associated with a non-volcanic trigger. We revisit the debris field of Iriga avalanche to investigate its causal mechanisms and determine its time of occurrence. The absence of a soil layer between the pyroclastic flow (PF) deposit and hummocks, the mixture of the PF deposit with avalanche-related lava blocks, and hummocks comprised of PF deposits may indicate an eruptive event close in timing with respect to the debris avalanche. Also, a previously unidentified debris avalanche field in the west-northwest sector of Iriga volcano was identified. This debris avalanche is older than the more obvious debris avalanche field in the southeast sector, which is associated with a well-formed horseshoe-shaped amphitheatre crater. Both events are organised around a characteristic sigmoid structure- a negative flower structure caused by a major strike-slip fault that cuts the cone in two. The remaining structures on the cone and the avalanche structure are consistent with a fault movement related origin, and possible associated gravity spreading. Iriga serves as a textbook example of fault related volcanic landsliding that can be applied to other potential at risk volcanoes in strike-slip environments, such as Mayon.