11:00 AM - 1:00 PM
[SVC30-P06] New publication series of large-volume ignimbrites derived from large-scale eruptions in Japan
Keywords:Large-volume, Large Eruption, Ignimbrite, Ash fall, Distribution
"Distribution Map of Ito Ignimbrite and associated deposits, Aira Caldera, Japan," which is the first publication of this series, contains a 1:250,000 scale map of the distribution of the Ito ignimbrite in the area within ~100 km from Kagoshima Bay. In addition to the distribution of the Ito ignimbrite on the ground surface, this map also shows the subsurface distribution of the ignimbrite based on borehole data. The map also indicates point data of the distribution of the altitude and the thickness of the ignimbrite, the maximum size of pumice and lithic fragments in the ignimbrite, and the preferred orientation of the pumice fragments (Figure). The distribution of the Aira-Tn ash fall deposit, the co-ignimbrite ash of the Ito ignimbrite, is also shown. The reconstructed distribution of the Ito ignimbrite based on numerical simulation is also shown. The distribution map contains an explanation booklet that provides background geological information about the Aira caldera and sequence of the Ito eruption, as well as descriptions of the Ito ignimbrite and associated deposits. The explanation booklet provides a pictorial of representative field occurrences of the Ito ignimbrite and associated deposits. All contents in PDF and GIS files can be downloaded from the website: https://www.gsj.jp/Map/JP/lvi.html.
GSJ plans to publish 12 distribution maps for the series on large-volume ignimbrites in Japan: Ito, Shikotsu, Aso-4, Aso-3, Toya, Ata, Kutcharo IV, Kutcharo I, Hachinohe, Ofudo, Koya, and Hakone-Tokyo ignimbrites. The "Distribution Map of Large-volume Ignimbrite in Japan" series will use a standard format to present the distribution of large-volume ignimbrites and associated ash fall deposits. These publications are expected to be used by researchers in universities and research institutes and will provide information about the possible extent of affected areas during future large-volume eruptions. This information could play a crucial role in disaster mitigation plans operated by national and regional governments and the construction of resilient infrastructure.