Multiple levels of magma storage during the 1980 summer eruptions of Mount St. Helens, WA

• Published in: Bulletin of volcanology Vol. 68; no. 1; pp. 57 - 75
• Main Authors: CASHMAN, K. V, MCCONNELL, S. M
• Format: Journal Article
• Language: English
• Published: Heidelberg Springer 01.11.2005; Springer Nature B.V
• 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; Magma; Natural hazards: prediction, damages, etc; Volcanic eruptions; Volcanoes; Volcanology; experimental studies; chain silicates; oxides; textures; pyroclastic flows; domes; vulcanian-type eruptions; Decompression crystallization; storage; fragmentation; lava; clasts; silicates; craters; Eruption style; models; Mount St. Helens; hornblende; Magma storage; reaction rims; volcanoes; magmas; pressure; microlite; intrusions; clinoamphibole; depth; growth; style; plinian-type eruptions; melts; amphibole; inclusions; volatiles
• ISSN: 0258-8900; 1432-0819
• DOI: 10.1007/s00445-005-0422-x

Transitions in eruptive style--explosive to effusive, sustained to pulsatory--are a common aspect of volcanic activity and present a major challenge to volcano monitoring efforts. A classic example of such transitions is provided by the activity of Mount St. Helens, WA, during 1980, where a climactic Plinian event on May 18 was followed by subplinian and vulcanian eruptions that became increasing pulsatory with time throughout the summer, finally progressing to episodic growth of a lava dome. Here we use variations in the textures, glass compositions and volatile contents of melt inclusions preserved in pyroclasts produced by the summer 1980 eruptions to determine conditions of magma ascent and storage that may have led to observed changes in eruptive activity. Five different pyroclast types identified in pyroclastic flow and fall deposits produced by eruptions in June 12, July 22 and August 7, 1980, provide evidence for multiple levels of magma storage prior to each event. Highly vesicular clasts have H^sub 2^O-rich (4.5-5.5 wt%) melt inclusions and lack groundmass microlites or hornblende reaction rims, characteristics that require magma storage at P≥160 MPa until shortly prior to eruption. All other clast types have groundmass microlites; P^sub H20^ estimated from both H^sub 2^O-bearing melt inclusions and textural constraints provided by decompression experiments suggest pre-eruptive storage pressures of 75, 40, and 10 MPa. The distribution of pyroclast types within and between eruptive deposits can be used to place important constraints on eruption mechanisms. Fall and flow deposits from June 12, 1980, lack highly vesicular, microlite-free pyroclasts. This eruption was also preceded by a shallow intrusion on June 3, as evidenced by a seismic crisis and enhanced SO^sub 2^ emissions. Our constraints suggest that magma intruded to a depth of ≤4 km beneath the crater floor fed the June eruption. In contrast, eruptions of July and August, although shorter in duration and smaller in volume, erupted deep volatile-rich magma. If modeled as a simple cylinder, these data require a step-wise decrease in effective conduit diameter from 40-50 m in May and June to 8-12 m in July and August. The abundance of vesicular (intermediate to deep) clast types in July and August further suggests that this change was effected by narrowing the shallower part of the conduit, perhaps in response to solidification of intruded magma remaining in the shallow system after the June eruption. Eruptions from July to October were distinctly pulsatory, transitioning between subplinian and vulcanian in character. As originally suggested by Scandone and Malone (1985), a growing mismatch between the rate of magma ascent and magma disruption explains the increasingly pulsatory nature of the eruptions through time. Recent fragmentation experiments Spieler et al. (2004) suggest this mismatch may have been aided by the multiple levels at which magma was stored (and degassed) prior to these events.[PUBLICATION ABSTRACT]