Recent results suggest that an iron-rich oxide may have fractionally crystallized from a primordial magma ocean and settled on the core–mantle boundary (CMB). Based on experimental results, the presence of only a few percent of Fe-rich oxide could slow seismic waves down by several percent. This heavy layer can become highly undulating as predicted from dynamic modeling but can remain as a search for such structures. Strong constraints on D are provided by the core-phase SKS where it bifurcates, containing a short segment of P-wave diffractions (Pd) when crossing the CMB, called SKSd. Synthetics from models with moderate velocity drops (less than 10%) involving a layer with variable thickness, perhaps a composite of sharp small structures, with strong variation in thickness can explain both the observed SKSd waveforms and large scatter in differential times between SKKS and SKS. A smooth 3D image is obtained from inverting SKSd waveforms displaying rolling-hills with elongated dome-like structures sitting on the CMB. The most prominent one has an 80-km height, 81 length, and 41 width, thus adding still more structural complexity to the lower mantle. We suggest that these results can be explained by a dynamically-stabilized material containing small amounts ( 5%) ironrich (Mg,Fe)O providing a self-consistent physical interpretation. & 2012 Elsevier B.V. All rights reserved.