Rock fracture as a precursor to lava dome eruptions at Mount St Helens from June 1980 to October 1986

• Published in: Bulletin of volcanology 2007-04, Vol.69 (6), p.681-693
• Main Authors: SMITH, R, KILBURN, C. R. J, SAMMONDS, P. R
• Format: Article
• Language: English
• Subjects: Crystalline rocks; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Igneous and metamorphic rocks petrology, volcanic processes, magmas; Lava; Lava domes; Natural hazards: prediction, damages, etc; Rocks; Seismic activity; Volcanic eruptions; Volcanoes; Volcanology
• ISSN: 0258-8900; 1432-0819
• DOI: 10.1007/s00445-006-0102-5

Following its plinian eruption on 18 May 1980, Mount St Helens (Washington State, USA) entered a period of intermittent lava-dome extrusion until 1986. Renewed extrusion was frequently preceded by accelerating rates of seismicity, with more precursory seismicity observed prior to eruptions later in the sequence. Here the failure forecasting method (FFM) is used to investigate changes in the observed rate of volcano-tectonic (VT) seismicity. The analysis indicates that: (1) all VT crises resulted in an eruption within 3 weeks (usually less than 10 days), (2) the majority of eruptions had VT precursors, and (3) patterns of precursory seismicity showed fluctuations about the ideal model trend. Thus, although these seismic events could be used to warn of an impending eruption, specific forecasts were subject to an uncertainty of weeks or more. It is proposed that: (1) increased seismicity prior to later eruptions is a result of a larger and more solidified dome acting as a greater impediment to magma ascent; (2) the consistency of seismic swarms resulting in an eruption indicates that stresses high enough to initiate fracturing in the country rock and lava dome carapace were only achieved once the approach to an eruption had already begun; and (3) discrepancies between models of accelerating rock fracture and the observed seismicity may arise due to a significant amount of the rocks deforming through ductile mechanisms rather than seismogenic fracture.[PUBLICATION ABSTRACT]