Lava domes comprise of core, carapace, and clastic talus components. They can grow endogenously by inflation of a core and/or exogenously with the extrusion of shear bounded lobes and whaleback lobes at the surface. Internal structure is paramount in determining the extent to which lava dome growth evolves stably, or conversely the propensity for collapse. The more core lava that exists within a dome, in both relative and absolute terms, the more explosive energy is available, both for large pyroclastic flows following collapse and particularly for lateral blast events following very rapid removal of lateral support to the dome. Knowledge of the location of the core lava within the dome is also significant for hazard assessment purposes. A spreading toe or lobe of core lava over a talus substrate may be both relatively unstable and likely to accelerate to more violent activity during the early phases of a retrogressive collapse.Soufrière Hills Volcano, Montserrat has been erupting continuously since 1995 and has produced numerous lava domes which have suffered collapse events. We consider one continuous dome