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Corrigendum: Maars to calderas: End-members on a spectrum of explosive volcanic depressions (Front. Earth Sci., (2015) 3, 10.3389/feart.2015.00036)

  • University of Rome La Sapienza
  • National Research Council of Italy
  • Istituto Nazionale Di Geofisica E Vulcanologia

Research output: Contribution to journalComment/debate

1 Scopus citations

Abstract

In the original article (Palladino et al., 2015), there was an error in Figure 1. The vertical axis of the qualitative plot reported erroneously “ratio of juvenile to lithic materials in deposits outside of depression”. The correct wording is as follows: “ratio of juvenile to total (i.e., juvenile+lithic) materials in deposits outside of depression”. In fact, as it was reported correctly in the text, the amount of juvenilematerial (i.e., scoria or pumice) deposited ouside the different types of explosive volcanic depressions increases from zero (i.e., no juvenile, all lithic products), as is the case of hydrothermal (phreatic) explosion craters, to become largely dominant over the lithic component in the case of ash flow deposits associated with large overpressure collapse calderas. The corrected Figure 1 appears below. The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way.

Original languageEnglish
Article number42
JournalFrontiers in Earth Science
Volume5
DOIs
StatePublished - May 22 2017

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