Variability in geyser eruptive timing and its causes: Yellowstone National Park

Details Variability in geyser eruptive timing and its causes: Yellowstone National Park Variability in geyser eruptive timing and its causes: Yellowstone National Park

Sep 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30rhls2r&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 18, pp. HLS 2-1, CiteID 1953, DOI 10.1029/2003GL017853

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Volcanology: Hydrothermal Systems (8135), Hydrology: Water/Energy Interactions, Hydrology: Groundwater Hydrology

Scientific paper

Field data from Upper Geyser Basin, Yellowstone, indicate that geyser frequency is less sensitive to elastic deformation than might be surmised from a review of the literature. Earth-tide influences are not identifiable in any of the geysers we monitored. Though atmospheric-pressure influences are observed, only long-period variations on the order of 5 mBars or greater seem to influence geyser frequency. Long-distance interconnections between geysers are common and add to the difficulty of identifying strain influences. Additional variations in geyser periodicity may be governed by the internal dynamics of the geysers rather than external influences.

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