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In this comment, we demonstrated how the shape of the seabed revealed by sonars can be valuable for working out the original shape of the island, which is commonly modified by erosion and subsidence.
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This page is a summary of: Comment on “Construction and destruction of a volcanic island developed inside an oceanic rift: Graciosa Island, Terceira Rift, Azores” by Sibrant et al. (2014) and proposal of a new model for Graciosa's geological evolution, Journal of Volcanology and Geothermal Research, September 2015, Elsevier,
DOI: 10.1016/j.jvolgeores.2015.07.007.
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