“…Paleo‐firing temperatures are important indicators for reconstructions of characteristics of lava flows and their influence on the host rocks (e.g., Mare et al, ; Silva et al, ), as well as for constraining the maximum temperature achieved in the rupture zone during an earthquake (e.g., Yang et al, ). Furthermore, determination of (paleo)firing temperatures is of great importance in archeology and specifically for pottery characterization in order to ascertain the technological development and/or provenance of the finds (Maniatis, ) or to document the human use of fire in sediments (Barbetti, ; Carrancho et al, ; Kapper et al, ). Different analytical methods are employed for such analysis (mineralogical studies, scanning electron microscopy (SEM), color determination, Mössbauer spectroscopy, thermal analysis, etc.)…”