What archaeology says
The Hydrographic Institute of the Portuguese Navy, which holds detailed bathymetry of Azorean waters, reviewed the claim and concluded the feature is a natural volcanic hill, its apparently perfect geometry an artefact of the low-resolution consumer echo-sounder used to detect it. Recreational sonar interpolates sparse depth soundings into smooth surfaces, notoriously rendering rough volcanic cones as crisp geometric solids. The setting makes the natural explanation almost inevitable: the João de Castro Bank is a young, active volcano that erupted as recently as 1720, briefly building an island about a kilometre across that waves demolished within a couple of years. The seabed between Terceira and São Miguel is crowded with such cones, and none of the navy's own high-resolution surveys show anything artificial.
The wider Azorean 'pre-Portuguese' file gets similar treatment. Historical and archaeological consensus holds the islands were uninhabited when Portuguese settlers arrived in the 1430s. The pyramid-like maroiços of Pico island are explained as field-clearance cairns — generations of farmers stacking volcanic rubble as they cleared vineyard plots, a landscape UNESCO studied closely before World Heritage listing in 2004 without finding any pre-Portuguese element. Claims of rock-cut hypogea and inscriptions promoted by Nuno Ribeiro of the Portuguese Association of Archaeological Research (APIA) have not been accepted by the Regional Directorate of Culture, whose reviews found natural cavities and post-settlement features. One genuine wrinkle: a 2021 PNAS lake-sediment study led by Pedro Raposeiro found signals of livestock and land disturbance centuries before 1430, suggesting possible earlier Norse-era visits — a fascinating, legitimate debate about who reached the Azores first, but one involving mediaeval sailors, not Atlantean pyramid-builders.
- The Portuguese Navy Hydrographic Institute identified the feature as a natural volcanic hill misrendered by low-resolution sonar
- The nearby João de Castro Bank is an active volcano that built and lost an island as recently as 1720–1722
- The channel between Terceira and São Miguel is dense with natural volcanic cones of similar scale
- UNESCO's pre-2004 studies of Pico's landscape attributed the maroiços to post-settlement field clearance
- No pre-Portuguese artefact has ever been recovered in the Azores from a secure excavated context
