By Houben H., Boubekeur S.
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The andesitic dome-building eruption of the Soufriere Hills Volcano wreaked havoc at the small Caribbean island of Montserrat. approximately half this 'emerald Isle' was once rendered barren and uninhabitable, virtually two-thirds of the unique inhabitants needed to go away, and 19 lives have been misplaced, all as an instantaneous results of the volcanic task.
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L Contribution to Rmax Erosion OVERTOP Rmax > Bh Deposition OVERWASH Rmax >> Bh OVERTOP OVERWASH SLUICING OVERWASH CATASTROPHIC OVERWASH Wave action SLUICING OVERWASH Rmax >>> Bh CATASTROPHIC OVERWASH Rmax >>>> Bh ? ? Fig. 16 Conceptual model showing the different stages of barrier response to increasing wave and water-level conditions. Rmax and Bh refer to maximum run-up height and barrier height, respectively. For positive freeboard Rmax < Bh, and for negative freeboard Rmax > Bh. The maximum run-up height is the summation of storm surge and wave run-up, but for long timescales the relative sea-level rise also needs to be taken into consideration.
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