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Hualalai VolcanoEruption... Preferred conceptual model for the development of the magmatic system at Hualālai Volcano. Stages include (a) the shield stage, (b) the transitional period and (c) the post-shield stage. The shallow level tholeiitic magma chamber feeding shield stage volcanism is replaced by a deeper, larger chamber of differentiating transitional basalt that produced voluminous trachyte magma at ∼114 ka. Subsequent post-shield magma is dominantly alkalic basalt, originating from depths ≥∼10 km. Monzodiorite and diorite xenoliths studied here are the products of the fortuitous interception of rising alkali basalt with previously crystallized differentiates. This model is based on Wolfe et al. (1997), fig. 64.



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