Pau Canuda, along with Dr Alfredo Mayoral and Dr Arnau Garcia-Molsosa, have published a new open access paper on the reconstruction of palaeogeography and landscapes around the ancient Greek colony of Abdera. The paper is published in the journal “European Journal of Remote Sensing”.
Canuda, P.; Mayoral, A.; Garcia-Molsosa, A. 2024. Reconstructing palaeogeography and landscapes around the ancient Greek colony of Abdera (Thrace, NE gr.): an integrated remote sensing approach. European Journal of Remote Sensing. //doi.org/10.1080/22797254.2024.2392753
Link to free downloaded: https://www.tandfonline.com/doi/full/10.1080/22797254.2024.2392753
ABSTRACT: We developed a multi-source, integrated remote sensing approach to characterize the geomorphological features of the alluvial and coastal lowlands around the ancient Abdera (coastal Thrace, Gr.). By combining multi-temporal composites of satellite imagery, DEM-derived products, orthophotography, and different cartographic resources, more than 1000 linear km of ancient landforms have been identified and mapped. When crossed with archaeological and historical data, our results allowed to propose a reconstruction of the palaeogeographic evolution and geomorphological dynamics in the eastern lobe of the Nestos Delta, the Kosynthos plain, Lake Vistonida and the Porto Lagos coast since the Antiquity. Our results suggest that the delta developed mainly between Hellenistic times and the Late Antiquity, when it had reached a shape similar to the current. Most of the large palaeochannels visible in the delta seem to be Nestos’ short-lived avulsions occurring in late Byzantine and Ottoman periods. Eastwards progradation of the Kosynthos plain, especially during Byzantine and Ottoman periods and accelerating in the 20th c. due to river channelization, was the main cause of the silting and a significant size reduction of Lake Vistonida since the Antiquity. Lake Lafra was also partially silted in late Byzantine and Ottoman times, likely due to the sedimentary discharge of the Kosynthos after a change in its course. By contrast, other lagoons and wetlands in the coast of Porto Lagos seem relatively stable in the last millennia with only minor silting and coastline progradation. Further geomorphological and geoarchaeological research in the area will allow to draw more precisely long-term interaction of past societies with environmental dynamics and resulting landscape change.
KEYWORDS: Geomorphology; Palaeogeography; landscape change; multi-temporal imagery; digital elevation models; northern Greece
