Abstract

Friedrich and coauthors [1] propose that two prominent eruption deposits of Santorini Volcano are in fact the same unit, resulting in a major reinterpretation of the volcanic history of this caldera. Here I summarize published field and petrological evidence showing that their proposal is not correct.

Highlights

  • License (CC BY 4.0).http://creativecommons.org/licenses/by/4.0/ Friedrich and coauthors [1] propose that two prominent eruption deposits of Open AccessSantorini Volcano are a single unit

  • Http://creativecommons.org/licenses/by/4.0/ Friedrich and coauthors [1] propose that two prominent eruption deposits of Santorini Volcano are a single unit

  • While I agree with the authors on the existence of ancient caldera cliff surfaces and plastering relationships at Santorini, I reject the interpretation that the LPS2 was, like the Upper Pumice Series (UPS), laid down by the LBA eruption

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Summary

Introduction

License (CC BY 4.0).http://creativecommons.org/licenses/by/4.0/ Friedrich and coauthors [1] propose that two prominent eruption deposits of Open AccessSantorini Volcano are a single unit. Reference [1] proposes that the products of the LBA eruption were deposited on the cliff of an ancient (pre-LBA) caldera, and that this cliff had a terrace about half way down it.

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