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