Vertical ground displacement at Campi Flegrei ( Italy) in the fifth century: Rapid subsidence driven by pore pressure drop

Campi Flegrei (Italy) caldera has experienced episodes of ground deformation throughout its geological history, alternating between uplift and subsidence phases. Although uplift periods are typically more alarming, here we focus on subsidence, looking for its driving mechanisms and its role in the caldera evolution. Historical and archaeological records constrain ground deformation over the last two millennia. Here we revise such records and combine them with published radiometric dating and with the simulation of sea level change. The resulting analysis highlights for the first time a rapid subsidence during the fifth century. We show that rate and magnitude of this subsidence are consistent with the compaction of porous material caused by a pressure drop of similar to 1MPa within the hydrothermal system. We interpret this event as the decompression of the hydrothermal system following an unrecognized episode of unrest, during Roman times. These findings redefine the pattern of ground deformation and bear important implications for volcanic hazard assessment. Key Points An integrated approach constrains fast subsidence at Campi Flegrei in the fifth century Fast subsidence can be caused by compaction due to decompression of hydrothermal system A sequence of unrest events preceded last eruption with no secular subsidence