Bifurcation of the Yellowstone plume driven by subduction-induced mantle flow by Christopher Kincaid and others 2026-10-25
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Nature Geoscience 6, 395–399. Laboratory slab rollback experiments generate opposite thermal progressions. The High Lava Plains branch is a passively advected thermal anomaly, distinct from the deformed conduit beneath the Snake River Plain. Author-uploaded full text: www.researchgate.net/publication/236694225_Bifurcation_of_the_Yellowstone_plume_driven_by_subduction-induced_mantle_flow
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