Barry Dawson is just right for th e first Norman L. Bowen Award in Volcanology, Geochemistry, and Petrology. Like Norman L. Bowen, he has the inspiration to combine ideas from different disciplines to obtain a higher synthesis. Consider his brilliant talk of yesterday morning (Eos 69, p. 502, abstract V11C-06, Veined and metasomatised upper mantle beneath the Eastern African Rift: Evidence from N. Tanzania xenoliths). Barry rapidly reviewed the tectonic setting of east Africa, showed some nice photographs of the volcanic cones of Pello and Oldoinyo Lengai, focused on the upper-mantle xenoliths in scoria at Pello, moved in on the microscopy and mineral chemistry of the metasomatic veins in the peridotites, snowed how the lower density of a metasomatized peridotite would fit the middle of a geophysical profile from seismic surveys, and brought off a grand finale in which the Kenya dome was interpreted to result from inflation related to metasomatization of underlying peridotite. Undoubtedly, this will lead to many further studies of doming adjacent to rift systems around the world.