water Article Integrating Geomorphological Data, Geochronology and Archaeological Evidence for Coastal Landscape Reconstruction, the Case of Ammoudara Beach, Crete George Alexandrakis * , Stelios Petrakis and Nikolaos A. Kampanis Coastal and Marine Research Lab, Institute of Applied & Computational Mathematics, Foundation for Research & Technology-Hellas, 70013 Heraklion, Greece;
[email protected] (S.P.);
[email protected] (N.A.K.) * Correspondence:
[email protected] Abstract: Understanding the processes that govern the transformation of the landscape through time is essential for exploring the evolution of a coastal area. Coastal landscapes are dynamic sites, with their evolution strongly linked with waves and sea level variations. Geomorphological features in the coastal area, such as beachrock formations and dune fields, can function as indicators of the coastal landscape evolution through time. However, our knowledge of the chronological framework of coastal deposits in the Aegean coasts is limited. Optically Stimulated Luminescence dating techniques are deemed to be very promising in direct dating of the coastal sediments, especially when they are linked with archaeological evidence. The dating of the sediments from different sediment core depths, determined by the method of luminosity, allowed us to calculate the rate of sediment deposition over time. More recent coastal evolution and stability were examined from 1945 to 2020 with the use of aerial photographs and satellite images. This paper presents the 6000 ka evolution of a coastal Citation: Alexandrakis, G.; Petrakis, landscape based on geomorphological, archaeological, and radio-chronological data. Based on the S.; Kampanis, N.A. Integrating results, the early stages of the Ammoudara beach dune field appears to have been formed ~9.0–9.6 ka Geomorphological Data, Geochronology and Archaeological BP, while the OSL ages from 6 m depth represented the timing of its stabilization (OSL ages ~5–6 ka).