Volcanic edifices consist of diverse suites of pyroclastic successions, originated from primary (e.g. tephra fall, lava flow) and reworking processes (e.g. alluvial activity). The volcanoclastic sediments have witnessed the magma fragmentation and subsequent transportation mechanism as flow, turbulent current or tephra fall. Such pyroclastic deposits therefore hold key evidence to understand volcano-stratigraphy, eruption re-occurrence rates, and dominant transportation modes. This session aims to discuss sedimentary and volcanological aspects of volcanoclastic deposits. We invite presentations covering (1) field-based description and interpretation of volcanoclastic sediments, (2) reconstruction of eruptive and sediment transport processes, (3) experimental and numerical simulation of volcano-related sediment transport, and (4) development of new methodologies to understand the formation of volcanoclastic sediments. These topics are critical to understand volcanic phenomena and to improve upon existing volcanic monitoring efforts, and to forecast volcanic hazards in the future.

Co-organized as NH2.9/SSP3.12, co-sponsored by IAVCEI-CVS
Convener: Gabor Kereszturi | Co-conveners: Eric Breard, Andrea Di Capua, Gonca Gençalioğlu-Kuşcu, Alison Rust
| Attendance Tue, 09 Apr, 16:15–18:00
Hall X2

Attendance time: Tuesday, 9 April 2019, 16:15–18:00 | Hall X2

Chairperson: Gabor Kereszturi, Andrea Di Capua
X2.257 |
Greg Smith, Rebecca Williams, Peter Rowley, and Daniel Parsons
X2.258 |
Fabio Dioguardi, Pierfrancesco Dellino, Daniela Mele, and Domenico Maria Doronzo
X2.259 |
Rebecca Williams, Michael Branney, Tiffany Barry, and Michael Norry
X2.261 |
Andrea Di Capua, Federica Barilaro, János Szepesi, Réka Lukács, Gianluca Groppelli, Roberto Sulpizio, Gianluca Norini, Ildikó Soós, and Szabolcs Harangi
X2.263 |
| solicited
Samantha Engwell, Steve Carey, Sebastian Watt, Simon Day, and Dave Tappin
X2.265 |
Lauren Schaefer, Gabor Kereszturi, and Ben Kennedy