The Azilal Formation (historically Toundute Continental Series and Wazzant Formation) is a geological unit in the Azilal and Ouarzazate provinces of the High Atlas mountains of Morocco. It covers the Latest Pliensbachian to early Aalenian stages of the Jurassic period. It is a terrestrial deposit that overlies marine dolomites of equivalent age to the Budoš Limestone of Montenegro or the Marne di Monte Serrone of Italy. Dinosaur remains, such as the sauropod Tazoudasaurus and the basal ceratosaur Berberosaurus are known from the unit, along with several undescribed genera.