Jordá Pardo, Jesús FranciscoCarral, PilarDuarte, CarlosMaestro, AdolfoMaximiano, AlfredoMolina, JuanaObeso, RamónColectivo Espeleológico L´Esperteyu Cavernícola Espeleo ClubÁlvarez Fernández, Esteban2024-07-302024-07-302022-09-12Jordá Pardo, J. F., Carral, P., Duarte, C., Maestro, A., Maximiano, A., Molina, J., Obeso, R., L´Esperteyu Cavernícola Espeleo Club, C. E., and Álvarez-Fernández, E.: Cova Rosa revisited. New geoarchaeological research at the Upper Pleistocene – Lower Holocene site of Cova Rosa (Sardéu, Ribadesella, Asturias, Spain)., 10th International Conference on Geomorphology, Coimbra, Portugal, 12–16 Sep 2022, ICG2022-110, https://doi.org/10.5194/icg2022-110, 2022.https://doi.org/10.5194/icg2022-110https://hdl.handle.net/20.500.14468/23159The karstic cavity of Cova Rosa (Sardéu, Ribadesella, Asturias), developed in the La Escalada limestones (Moscovien, Carboniferous), contains an important archaeosedimentary sequence covering the Late Upper Pleistocene and the Lower Holocene. This sequence, excavated during the second half of the 20th century by Jordá Cerdá and Gómez Fuentes (1982), presents levels of Solutrense, Lower and Upper Magdalenian and Mesolithic. The sequence was studied sedimentologically by Hoyos Gómez (1979). In the last years members of a large research team are working again on this site and its materials (Álvarez-Fernández and Jordá Pardo, 2018) and in this contribution we present the new lithostratigraphic sequence that has been studied again with geoarchaeological methodology. In addition, thanks to the 22 radiocarbon dates obtained (Álvarez-Alonso et al., 2021), we can place the sequence on the Quaternary chronostratigraphic scaleesinfo:eu-repo/semantics/openAccess55 Historia55 Historia::5505 Ciencias auxiliares de la historia::5505.01 Arqueologíaactas de congreso