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Geomorphological evidence and 10Be exposure ages for the Last Glacial Maximum and deglaciation of the Velká and Malá Studená dolina valleys in the High Tatra Mountains, central Europe

Exposure AgesEngineeringPaleoenvironmental ChangeGeomorphologyCentral EuropeGeographyGeologyHigh Tatra MountainsQuaternary ResearchGeochronologyEarth ScienceQuaternary Period