Resources (1-1 of 1)

1. Magma flow between summit and Pu`u `O`o at Kilauea volcano, Hawai`i

   14 Mar 2014 | Contributor(s):: Chiara Paola Montagna, Helge Gonnermann

   Volcanic eruptions are often accompanied by spatiotemporal migration ofground deformation, a consequence of pressure changes within magma reser-voirs and pathways. We model the propagation of pressure variations byeruptive magma withdrawal during the early episodes of the ongoing Pu‘u ̄...