Earthquake Environmental Effects: The Case of Late Classical-Hellenistic Helike, Gulf of Corinth, Greece

被引:2
作者
Katsonopoulou, Dora [1 ,2 ]
Koukouvelas, Ioannis [3 ]
机构
[1] Helike Soc, Athens 10682, Greece
[2] Helike Project, Athens 10682, Greece
[3] Univ Patras, Dept Geol, Patras 26504, Greece
关键词
Classical-Hellenistic Helike; 373; BC; earthquake effects; settlement destruction; liquefaction; environmental changes; dyeworks; Helike Fault; Gulf of Corinth; Greece; TECTONOSEDIMENTARY EVOLUTION; RIFT; FAULT; LIQUEFACTION; BASIN; STRATIGRAPHY; ARCHITECTURE; FEATURES; HISTORY; SYSTEM;
D O I
10.3390/geosciences14110311
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Human habitat is much controlled by the landscape and its ongoing processes overtime. Some of these processes occur instantaneously and are often triggered by seismic events with a major destructive impact on the human-built environment. Helike, on the southwest shore of the Gulf of Corinth, is a characteristic case of an ancient habitation site bearing witness to repetitious natural disasters from the Early Bronze Age to the Late Antiquity. The Late Classical-Hellenistic site, revived in the Helike plain after the 373 BC earthquake, has been systematically investigated thanks to the multidisciplinary research and excavations of the Helike Project in the last 35 years. This work has significantly enriched the historical seismicity of the region and shed light on past human-environment relationships. The study of the architectural remains excavated by the Helike Project, coupled with geological and soil micromorphological analysis on archaeological soils and sediments of the settlement, demonstrates a constant effort of the Helike people to reconcile with the elements of nature. Our results underline the destruction of a flourishing textile dyeworks operated at the settlement, due to a strong earthquake which triggered extensive morphological changes in a broader area. These changes include co-seismic liquefaction and lateral spreading, and post-seismic changes in the gradient of river channels. The former changes attest to an uplift in the headwater area and subsidence in the lowland plain of the ravine flowing near the ancient site.
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页数:14
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