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Cape Verde is a volcanic archipelago situated above an oceanic rise that puts the base of the islands 2 kilometers above the rest of the seafloor. Cape Verde has been identified as a hotspot and the majority of geoscientists have argued that the archipelago is underlain by a mantle plume and that this plume is responsible for the volcanic activity and associated geothermal anomalies.
Evidence for a plume origin includes substantial uplift, low-velocity seismic anomalies in the upper mantle extending to depths of around 500 km, low-velocity anomalies in the lower mantle which appear to pond beneath the transition zone with branches extending to the Azores, Canary and Cape Verde hotspots, and petrological, geochemical, and isotopic evidence which are thought to indicate a deep-mantle source.
Some observations, such as a lack of age-progressive volcanism and the geochemical signatures of lavas which indicate a shallow source materials, are inconsistent with the plume model, and some scientists have argued that the Cape Verde Archipelago is a product rather of sub-lithospheric small-scale convection and instabilities arising from heterogeneities in the asthenosphere and variations in lithospheric thickness, with the geochemistry of the lavas attributed to remnants of subcontinental lithospheric mantle left in the oceanic lithosphere when the Atlantic Ocean opened.
The lack of age progression has been accounted for in the hotspot model by the suggestion it is virtually stationary relative to the lithosphere due to being situated close to the rotational pole of the slowly moving African Plate. The unusual geochemical signatures have been ascribed to recycled oceanic crust and lithosphere in the source material.