Vesiculation of high fountaining Hawaiian eruptions: episodes 15 and 16 of 1959 Kīlauea Iki

• Published in: Bulletin of volcanology 2012-03, Vol.74 (2), p.441-455
• Main Authors: Stovall, Wendy K., Houghton, Bruce F., Hammer, Julia E., Fagents, Sarah A., Swanson, Don A.
• Format: Article
• Language: English
• Subjects: Crystalline rocks; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Geology; Geomorphology; Geophysics; Geophysics/Geodesy; Igneous and metamorphic rocks petrology, volcanic processes, magmas; Lava; Mineralogy; Natural hazards: prediction, damages, etc; Research Article; Sedimentology; Volcanic eruptions; Volcanoes; Volcanology; Zonation
• ISSN: 0258-8900; 1432-0819
• DOI: 10.1007/s00445-011-0531-7

The 1959 summit eruption of Kīlauea volcano produced the highest recorded Hawaiian fountain in Hawai‘i. Quantitative analysis of closely spaced samples from the final two high-fountaining episodes of the eruption result in a fine-scale textural study of pyroclasts and provide a record of postfragmentation processes. As clast vesicularity increases, the vesicle number density decreases and vesicle morphology shifts from small and round to larger and more irregular. The shift in microtexture corresponds to greater degrees of postfragmentation expansion of clasts with higher vesicularity. We suggest the range of clast morphologies in the deposit is related to thermal zonation within a Hawaiian fountain where the highest vesicularity clasts traveled in the center and lowest traveled along the margins. Vesicle number densities are greatest in the highest fountaining episode and therefore scale with intensity of activity. Major element chemical analyses and fasciculate crystal textures indicate microlite-rich zones within individual clasts are portions of recycled lava lake material that were incorporated into newly vesiculating primary melt.