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Glaciovolcanism at Volcán Sollipulli, southern Chile: Lithofacies analysis and interpretation

Lachowycz, Stefan M.; Pyle, David M.; Gilbert, Jennie S.; Mather, Tamsin A.; Mee, Katy; Naranjo, Jos� A.; Hobbs, Laura K.

Authors

Stefan M. Lachowycz

David M. Pyle

Jennie S. Gilbert

Tamsin A. Mather

Katy Mee

Jos� A. Naranjo

Dr Laura Hobbs Laura5.Hobbs@uwe.ac.uk
Senior Research Fellow - CHSS - DAS



Abstract

© 2015 The Authors. Magma-ice-meltwater interactions produce diverse landforms and lithofacies, reflecting the multitude of factors that influence glaciovolcanism, including both magmatic (e.g., composition, eruption rate) and glacial (e.g., ice thickness, thermal regime) conditions. This is exemplified by the walls of the partly ice-filled summit caldera of Volcán Sollipulli, a stratovolcano in southern Chile, which include lithofacies from eruptions of a wide range of magma compositions beneath or in contact with ice. Here we analyse these lithofacies and hence propose new interpretations of the eruptive and glacial history of Sollipulli. The facies include a thick, laterally extensive sequence of fragmental glaciovolcanic deposits, comprising massive, mafic lava pillow-bearing hyaloclastite overlain by sills and then hyaloclastic debris flow deposits (similar to Dalsheidi-type sequences). The distribution and thickness of these units indicate an unusual abundance of magma-meltwater interaction for an arc stratovolcano in temperate latitudes, perhaps due to eruptions beneath a thick ice cap. Coherent lava coulées, domes, lobes, and stacks of basaltic andesite-trachydacite composition are present around the top of the caldera rim; these display morphologies and fracture patterns on caldera-facing margins that indicate that the caldera was filled with ice when these lavas were erupted. The lithofacies characterised in this study demonstrate the diversity of glaciovolcanism that is possible at arc stratovolcanoes capped by temperate ice or with ice-filled calderas, and the potential for uncertainties in inference of the palaeoenvironmental conditions of their emplacement.

Journal Article Type Article
Acceptance Date Jun 29, 2015
Publication Date Sep 5, 2015
Journal Journal of Volcanology and Geothermal Research
Print ISSN 0377-0273
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 303
Pages 59-78
DOI https://doi.org/10.1016/j.jvolgeores.2015.06.021
Keywords volcano–ice interaction, glaciovolcanic lithofacies, hyaloclastite, stratovolcano, caldera paleo environment reconstruction
Public URL https://uwe-repository.worktribe.com/output/805641
Publisher URL https://doi.org/10.1016/j.jvolgeores.2015.06.021