Publication | Open Access

Linking Danube River activity to Alpine Ice-Sheet fluctuations during the last glacial (ca. 33–17 ka BP): Insights into the continental signature of Heinrich Stadials

GlacierHeinrich StadialsEngineeringGeomorphologyDanube River ActivityGeographyCryosphereContinental SignatureQuaternary ResearchGlacial ProcessGeochronologyEarth ScienceQuaternary Period