Poster presented at the 2023 SCAR-INSTANT Conference, TriesteKarla Rubio-Sandoval (1) Andrew Hollyday (2) Deirdre D. Ryan (3) Evan J. Gowan (4) Jordon Bright (5) Marta Pappalardo (3) Sebastian Richiano (6) Marina Aguirre (7) Michael R. Sandstrom (8) Darrell Kaufman (5) Jacqueline Austermann (2) Alessio Rovere* (1,9)* Presenting authorUniversity of Bremen, MARUM, Center for Marine Environmental Sciences, Bremen, Germany (1) - Columbia University, Lamont-Doherty Earth Observatory, Division of Seismology, Geology, and Tectonophysics and Department of Earth and Env. Sci., New York, Usa (2) - University of Pisa, Department of Earth Sciences, Pisa, Italy (3) - Kumamoto University and KIKAI institute for Coral Reef Sciences, Department of Earth and Environmental Sciences, Kumamoto and Kikaijima, Japan (4) - Northern Arizona University, School of Earth & Sustainability, Flagstaff, Usa (5) - CONICET, Instituto Patagónico de Geología y Paleontología, Puerto Madryn, Argentina (6) - Universidad Nacional de La Plata, Facultad de Ciencias Naturales y Museo, La Plata, Argentina (7) - University of North Carolina, Department of Earth, Marine and Environmental Sciences, Chapel Hill, Usa (8) - Ca' Foscari University of Bremen, Department for Environmental sciences, statistics and informatics, Venice, Italy (9)In about 20 km of coast in the proximity of the town of Camarones (Central Patagonia, Argentina), sea level has left its imprint over four interglacials. In general, these were preserved in the form of beach ridges, deposited by storm waves above modern sea level. We used high-precision GNSS to measure the elevation of these deposits, and accounted for their indicative meaning (i.e., their elevation with respect to sea level at the time of deposition) with satellite-derived wave measurements and wave runup models. Using both published (U-series, Electron Spin Resonance and Radiocarbon) and original (Amino Acid Racemization and Radiocarbon) dating constraints, we detail the information on three past local sea-level highstands.