Comment on Philpotts and Philpotts (2005): Crystal-mush compaction in the Cohassett flood-basalt flow, Hanford, Washington

Young volcanic deposits in Kahoolawe Island, cutting up through the caldera-filling lava, colluvium and talus in the west wall of Kanapou Bay, had long been stratigraphically considered the rejuvenated-stage products. New K–Ar ages, combined with magnetic polarity data, show that young volcanism was at about 0.98–1.04 Ma and indicate no substantial quiescence between the filling of the caldera and the young volcanism. This result, and the tholeiitic characteristics of the young deposits, suggest they are a component of late shield-stage volcanism.