The discussion centers around a Science magazine article on seismic ultralow-velocity zones, which measure 800 km across and 15 km tall, and their potential link to rising mantle plumes. There is speculation that these zones could be liquid, although interpretations vary. The mantle is described as solid but capable of slow, convective movement, akin to a churning pot, which allows for the transmission of seismic waves. Participants clarify that while the mantle is not rigid, it deforms visco-plastically, and misconceptions about it being entirely liquid are addressed. A report from one participant indicates that seismic data suggests a slow-moving feature at the base of the Iceland plume, with interpretations leaning towards it being partially molten or composed of iron-rich solid material. The conversation emphasizes the complexity of interpreting seismic data and the importance of distinguishing between solid and liquid states in the mantle.