Geologic Publications for Mount Rainier
Fumaroles in ice caves on the summit of Mount Rainier: Preliminary stable isotope, gas and geochemical studies
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Author(s):
David R. Zimbelman,
Robert O. Rye,
G P. Landis
Category: PUBLICATION
Document Type:
Publisher: Journal of Volcanology and Geothermal Research
Published Year: 2000
Volume: 97
Number: 1-4
Pages: 457 to 473
DOI Identifier: 10.1016/S0377-0273(99)00180-8
ISBN Identifier:
Keywords: fumaroles magmatic hydrothermal
Abstract:
The edifice of Mount Rainier, an active stratovolcano, has episodically collapsed leading to major debris flows. The largest debris flows are related to argillically altered rock which leave areas of the edifice prone to failure. The argillic alteration results from the neutralization of acidic magmatic gases that condense in a meteoric water hydrothermal system fed by the melting of a thick mantle of glacial ice. Two craters atop a 2000-year-old cone on the summit of the volcano contain the world's largest volcanic ice-cave system. In the spring of 1997 two active fumaroles (T=62°C) in the caves were sampled for stable isotopic, gas, and geochemical studies.
Stable isotope data on fumarole condensates show significant excess deuterium with calculated δD and δ
18O values (−234 and −33.2‰, respectively) for the vapor that are consistent with an origin as secondary steam from a shallow water table which has been heated by underlying magmatic–hydrothermal steam. Between 1982 and 1997, δD of the fumarole vapor may have decreased by 30‰.
The compositions of fumarole gases vary in time and space but typically consist of air components slightly modified by their solubilities in water and additions of CO
2 and CH
4. The elevated CO
2 contents (δ
13C
CO2=−11.8±0.7‰), with spikes of over 10,000 ppm, require the episodic addition of magmatic components into the underlying hydrothermal system. Although only traces of H
2S were detected in the fumaroles, most notably in a sample which had an air δ
13C
CO2 signature (−8.8‰), incrustations around a dormant vent containing small amounts of acid sulfate minerals (natroalunite, minamiite, and woodhouseite) indicate higher H
2S (or possibly SO
2) concentrations in past fumarolic gases.
Condensate samples from fumaroles are very dilute, slightly acidic, and enriched in elements observed in the much higher temperature fumaroles at Mount St. Helens (K and Na up to the ppm level; metals such as Al, Pb, Zn Fe and Mn up to the ppb level and volatiles such as Cl, S, and F up to the ppb level).
The data indicate that the hydrothermal system in the edifice at Mount Rainier consists of meteoric water reservoirs, which receive gas and steam from an underlying magmatic system. At present the magmatic system is largely flooded by the meteoric water system. However, magmatic components have episodically vented at the surface as witnessed by the mineralogy of incrustations around inactive vents and gas compositions in the active fumaroles. The composition of fumarole gases during magmatic degassing is distinct and, if sustained, could be lethal. The extent to which hydrothermal alteration is currently occurring at depth, and its possible influence on future edifice collapse, may be determined with the aid of on site analyses of fumarole gases and seismic monitoring in the ice caves.
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In Text Citation:
Zimbelman and others (2000) or (Zimbelman et al., 2000)
References Citation:
Zimbelman, D.R., R.O. Rye, and G.P. Landis, 2000, Fumaroles in ice caves on the summit of Mount Rainier: Preliminary stable isotope, gas and geochemical studies: Journal of Volcanology and Geothermal Research, Vol. 97, No. 1-4, pp. 457-473, doi:
10.1016/S0377-0273(99)00180-8.