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C. P. Montagna and H. M. Gonnermann Magma flow between summit and Pu‘u ‘Ō‘ō at K̄lauea Volcano, Hawai‘i Geochemistry, Geophysics, Geosystems 14

Article first published online: 29 JUL 2013 | DOI: 10.1002/ggge.20145

Key Points

  • Propagation of pressure transients in elastic-walled dikes is non-linear
  • An elastic-walled dike model reproduces ground deformation patterns at Kilauea
  • Insights on the time-dependent transport properties of the east rift zone

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