Geomorphological analysis of the continental slope of the Mediterranean sea, based on a 100 m Data Terrain Model (DTM). This DTM is a synthesis of data acquired during several surveys. Bibliographic references :

IOWAGA sea-states hindcast database generated by the wave model WAVEWATCH-III and forced by ECMWF winds on the North mediterranean grid over 2004-2017 period.

IOWAGA sea-states hindcast database generated by the wave model WAVEWATCH-III and forced by ECMWF winds on the Mediterranean grid over 2005-2017 period.

La donnée contient la zone d'expansion maximale de la beauxite dans le canyon de Cassidaigne et du domaine bathyal environnant.