Abstract
The Canary Islands geoid anomaly shows only a short-wavelength high associated with island topography. The predicted anomaly best matches the observed geoid when we assume that the lithosphere is a very stiff plate. We find no evidence for shallow reheating or a mantle plume, since there is no evidence of a midplate swell and the corresponding elastic thickness is appropriate for the age of the seafloor on which the island group rests.
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Filmer, P.E., McNutt, M.K. Geoid anomalies over the Canary Islands Group. Mar Geophys Res 11, 77–87 (1989). https://doi.org/10.1007/BF00285659
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DOI: https://doi.org/10.1007/BF00285659