Explosive eruptions at the summit of Mauna Loa: Lithology, modeling, and dating

Frank A. Trusdell, Jefferson D.G. Hungerford, John O. Stone, Keith Fifield, Kaitlin McCann, Harold Wershow, Shikma Zaarur, Melissa Dimeo Boyd

Research output: Chapter in Book/Report/Conference proceedingChapterpeer-review

Abstract

Near Moku‘āweoweo, Mauna Loa’s summit caldera, there are three fans of explosive deposits. The fans, located to the west, northwest, and east, are strongly arcuate in map view. Along ‘Āinapō Trail, 2.8–3.5 km southeast of the caldera, there are several small kīpuka that expose a fourth explosive deposit. Although these explosive deposits have been known for some time, no study bearing on the nature of the explosive activity that formed them has been done. By analyzing cosmogenic exposure age data and the physical properties of the debris fans—lithology, size distributions, and clast dispersal—we conclude that the lithic deposits are the result of five separate phreatic events. The lithic ejecta consist of fragments of ponded lavas, pāhoehoe, gabbroic xenoliths, and “bread-crust” fragments. The exposure ages indicate that the explosive deposit on the west caldera rim was erupted 868 ± 57 yr B.P.; for the northwest fan, the age determination is 829 ± 51 yr B.P.; and on the east rim, ejecta deposits are younger, with ages of 150 ± 20 and 220 ± 20 yr B.P. Lavas underlying these deposits have exposure ages of 960–1020 yr B.P., consistent with the stratigraphy. Near ‘Āinapō Trail, the explosive deposit is much older, overlain by flows dated with a pooled mean age of 1507 ± 19 yr B.P. From the cosmogenic dating, we have three reliable and unambiguous dates. At a much earlier time, a fourth explosive eruption created the ‘Āinapō Trail deposit. We conclude there were at least five explosive episodes around the summit caldera. These deposits, along with recent work done on Kīlauea’s explosive activity, further discredit the notion that Hawaiian volcanoes are strictly effusive in nature. The evidence from the summit of Mauna Loa indicates that it, too, has erupted explosively in recent history.

Original languageAmerican English
Title of host publicationSpecial Paper of the Geological Society of America
EditorsM.P. Poland, M.O. Garcia, V.E. Camp, A. Grunder
PublisherGeological Society of America
Pages325-349
Number of pages25
DOIs
StatePublished - 2018

Publication series

NameSpecial Paper of the Geological Society of America
Volume538
ISSN (Print)0072-1077

Bibliographical note

Publisher Copyright:
© 2018 The Geological Society of America. All rights reserved.

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