Both subaerial and submarine explosive volcanic eruptions have the capacity to produce high velocity gas jets where fragmented particle-gas mixtures are ejected with significant inertia inherited from conduit processes (e.g. Woods, 1995). In this jet-thrust region, the particle-laden gas rises and loses kinetic energy through drag, gravitational deceleration, and turbulent mixing with the ambient fluid. Subaerial jet-thrust dynamics have been extensively studied through remote observations, experiments, and numerical simulations (