David Gallinar Cañedo, J. Ruiz Fernández, Miguel Angel Poblete Piedrabuena, A. Fernández, Cristina García Hernández, Salvador Beato Bergua, J. L. Marin
This research analyzes the glacial evolution of the Asturian sector of the Ubiña Massif (Cantabrian Mountains) based on the interpretation of moraine complexes and other glacial landforms. Three main glacial stages have been identified: (1) Glacial Maximum corresponding to the Last Glaciation, (2) Internal Stage, and (3) Late Glacial. In addition, the current geomorphological dynamics of the massif is outlined.
© 2001-2025 Fundación Dialnet · Todos los derechos reservados