Anthropogenic amplification of geomorphic processes along the Mediterranean coasts: A case-study from the Graeco-Roman town of Elea-Velia (Campania, Italy)

被引:5
作者
Amato, Vincenzo [1 ,2 ]
Cicala, Luigi [3 ]
Valente, Ettore [4 ]
Ruello, Maria Rosaria [4 ]
Esposito, Nunzia [3 ,4 ]
Ermolli, Elda Russo [4 ]
机构
[1] Univ Molise, Dept Biosci & Terr, I-86090 Pesche, IS, Italy
[2] Univ Salerno, Dept Sci Cultural Heritage, Via Giovanni Paolo II, I-84084 Fisciano, SA, Italy
[3] Univ Naples Federico II, Dept Humanist Studies, Via Nuova Marina 33, I-80133 Naples, Italy
[4] Univ Naples Federico II, Dept Earth Environm & Resources Sci, Via Cintia 21, I-80126 Naples, Italy
关键词
Alluvial-coastal plain; Morphostratigraphy; Geoarchaeology; Palaeogeographical evolution; Cilento; Southern Italy; SEA-LEVEL CHANGES; CLIMATE VARIABILITY; FLUVIAL RECORD; PLAIN CALABRIA; SOIL-EROSION; HOLOCENE; EVOLUTION; FLUCTUATIONS; TUNISIA; MARINE;
D O I
10.1016/j.geomorph.2021.107694
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Coastal areas are very dynamic environments where natural and man-induced modifications often interact. This is the case of the Graeco-Roman town of Elea-Velia, along the Cilento coast of southern Italy. The town was founded in the 6th century BCE on a hilly promontory bounded by two profound gulfs and assumed a prominent role in maritime commercial routes in the Graeco-Roman period. It declined in the Late Antiquity and was abandoned in the Middle Ages also due to serious landscape changes. In this study, the integration of geomorphology, borehole stratigraphy and analysis of archaeo-stratigraphical trenches was used to detail the relationship between geological and archaeological evidence. The huge amount of collected data allowed providing chronological constraints to the landscape modification occurred before and after the town foundation. The main environmental changes consisted in enhanced coastal progradation and alluvial fan deposition that mainly affected the lower quarters of the town. The results of this study suggest that alluvial flooding was one of the main causes of the Elea-Velia decline and subsequent abandonment. The increasing disruption of slope stability was driven by the neglect in the management of the hillslopes behind the town during periods of social economic crisis, but a concomitant climate forcing cannot be excluded. To the final abandonment also contributed the declining of harbour activities and the consequent decreased relevance of Elea-Velia as a maritime centre. (c) 2021 Elsevier B.V. All rights reserved.
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页数:17
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