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Hotspot swells and the lifespan of volcanic ocean islands

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Figure

Fig. 1. Hypothesized mechanisms of swell uplift. (depth in the absence of surface loading and associated flexural isostasy
Fig. 3. Excess island subsidence following submergence. Expected thermal subsidence since submergence below sea level, based on the depths of guyot tops and/or the thickness of coral reef caps (sediment loading has been removed from the observed subsidence

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