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We present a synopsis of geophysical imaging results from the RHUM-RUM experiment (2011-2015), integrating the findings of whole-mantle body-wave tomography, anisotropic surface-wave tomography, and shear-wave split- ting analyses. In one of the largest attempts to image an oceanic mantle plume from crust to core, RHUM-RUM deployed almost 90 broadband seismometers on 2000 x 2000 km2 of sea floor and islands surrounding the La Réunion hotspot, including 57 broadband ocean-bottom seismometers for 13 months.