Claims

Post-glacial sea-level rise drowned coastal land in the Bay of Biscay

Documented · occurred What these labels mean →

The southeastern Bay of Biscay continental shelf preserves at least 12 submerged marine terraces and former shorelines, from about -13 m to about -90 m, formed at past lower sea levels since the Last Glacial Maximum and now drowned.

Evidence

RelationRecordNote
documentsfrontiersin.orgBilbao-Lasa et al., 'Submerged Marine Terraces Identification … in the Bay of Biscay', Frontiers in Earth Science 8:47 (2020): '12 submerged terraces with their shoreline angles between approximately: −13 m (T1)… −89'; strandlines preserved 'throughout the continental shelf'; scenario linked to the Last Glacial Maximum

Sources

SourceRelationAt
Basques and Atlantis (Why Files 2026)reports

Claim

The southeastern Bay of Biscay continental shelf preserves at least 12 submerged marine terraces and former shorelines, from about -13 m to about -90 m, formed at past lower sea levels since the Last Glacial Maximum and now drowned.