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The Alcudia archaeological site correspond to the ancient city of Ilici (Roman Colonia Iulia Ilici Augusta). The site consists of an succession of Iberian, roman, byzantine, Visigoth and Moorish settlements (since the 5th centuries BC to the 8th century AC) on the top of a hill that in the 1st century BC was surrounded by a wall and nearby the Vinalopó river mouth in the Bajo Segura Bay. This bay was known in Roman times as the sinus Ilicitanus. Different clays of the area nearby to the site have been sampled, analysed and then compared with analysis of some pottery remains of the different periods of the Alcudia settlement. The clays have been analysed by micro-X Ray fluorescence (µXRF) and by infrared spectrometry by Fourier transformed (ATR-FTIR), as crude, mixed in different proportions, and then heated to a different temperature until 900ºC. The old remains show affinities with the clays sampled from the Eastern part indicating a W-E influence, as the northern coast of the sinus ilicitanus. During the roman period and later the pottery was made using the nearby clays located just to the north of the site clearly influenced by the via Augusta. The topography to the north of the site is formed by low but steep hills and small creeks that possibly limit the commerce to the north, so the commerce follows the marine plain coast of the northern sinus ilicitanus. The opening of the roman road via August along the Vinalopó Valley favoured the use of pottery clays from the interior of the territory.
Cite as: Jordá Guijarro, J., Cerdán Sala, M., Sánchez-Sánchez, A., Ronda Femenia A., Tendero Porras, M. and Tent-Manclús, J. E. (2021): Pottery clays quarries in the domain territory of ancient Ilici (Alicante, SE Spain). LAC1+1, Landscape archaeology conference, 8-11 june 2021 Book of Abstracts. 45 p.
Change on the coastline of the Southern Alicante region
Tent-Manclús, J. E.
The Bajo Segura Region is a plain dominated by the Segura River with the mouth towards the Mediterranean Sea on Guardamar. The Hondón and Salinas de Santa Pola lagoons inside the plain, are the remains of a major marine bay known in the Roman times as the sinus ilicitanus. Offshore the Region geophysical data has permitted to model the coastline change and study the underwater marine terraces. 183 maps have been made from the 15000 BP until Today (100 year apart the older ones and 25 years for the recent ones). The coastline has migrated between 20 and 50 km onshore and then offshore about tens of meters to 35 km shaping today coastline. The sea level at 15000 BP was located 70 m below today sea-level (btsl). During the Younger Dryas (13500 to 11700 BP) varies around 60-66 m btsl then increase until 21 m btsl and stopped during the 8.2 ka event (8500 BP to 8200 BP). Again, the level increases first fast and then slowly but moving fast horizontally (near 35 km for 1000 years) developing the sinus ilicitanus when the marine transgression enters the plain about 4200 BC. The Segura River developed a delta in the today area of Orihuela, 35 km to the East of its today river mouth in Guardamar. The river until around the year 1400 AD developed a fingering (bird-foot) quite variable delta in the center of the sinus, most of the major irrigation canals (acequias) could correspond to the ancient delta-channels. Around the XV century major events changed the sinus basin producing the river mouth move to the present location. The sinus open communication with the Mediterranean Sea was closed around the XVIII century by sand bars, first the southern of Guardamar and then the northern on Santa Pola.