Simmons, J.M., Cas, R.A.F., Druitt, T.H. and Folkes, C.B. (2016) Complex Variations during a Caldera-Forming Plinian Eruption, Including Precursor Deposits, Thick Pumice Fallout, Co-Ignimbrite Breccias and Climactic Lag Breccias: The 184 ka Lower Pumice 1 Eruption Sequence, Santorini, Greece. Journal of Volcanology and Geothermal Research, 324, 200-219.

has been cited by the following article:

• TITLE: A Comment on “A major Change in the Stratigraphy of the Santorini Volcano in Greece”

  AUTHORS: Timothy H. Druitt

  KEYWORDS: Santorini, Lower Pumice, Upper Pumice, Minoan, Caldera

  JOURNAL NAME: International Journal of Geosciences, Vol.8 No.9, September 19, 2017

  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.