38 Undergraduate and Graduate Geoscience Student Lightning Talk Showcase (Posters)
Friday, 17 May 2024
9:00 AM - 1:30 PM
Grand Ballroom
ANALYZING THE ERUPTIVE HISTORY AND TRENDS OF MOUNT ST. HELENS, CASCADIA SUBDUCTION ZONE
Paper number: 38-13
Program: Theme Sessions
Time: 9:00 AM – 1:30 PM
Authors
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David GonzalesFort Lewis College, Durango, CO
Abstract
The record of MSH eruptions over the past 40 ka reveal cyclic patterns defined by initial Plinian-style eruptions that progress into smaller pyroclastic events. The latter stages involve lahars followed by dacitic to rhyolitic lava dome or flows. In the past 40 ka, the repose intervals of eruptions have decreased over time.
Over the 40 ka history there is a general progression from early dacitic to andesitic compositions followed by andesitic to basaltic compositions. Some models propose that this progression is indicative of different magma batches sourced from a progressively graded magma chamber. Other models posited that this progression was a result of magma sourced from a rising pluton of vertically graded, mantle-derived magma. The latter hypothesis is supported by Nd and Sr isotopic signatures that reveal mantle contributions to felsic and intermediate MSH magmas.
The results of this study show long-term shifts in the eruptive patterns and products at MSH that are linked to the evolution of magma reservoirs and structural controls. This record serves as a potential predictive tool for future eruptions from Mount St. Helens.
Geological Society of America Abstracts with Programs. Vol. 56, No. 4
doi: 10.1130/abs/2024CD-399441
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