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Palaeogeographic reconstruction of the Heraion–Vouliagmeni Lake coast since Early Helladic times1

Published online by Cambridge University Press:  27 September 2013

S. C. Stiros
S. C. Stiros
Affiliation:
Institute of Geology and Mineral Exploitation (IGME), Athens
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Abstract

The morphology of the Vouliagmeni Lake and Perachora coasts is the result of seismic uplifts with a cumulative amplitude of 3–4 m in the last 6,000 years; there is also evidence of a transient seismic subsidence at around 5,000 BP. These results are consistent with excavation data indicating a seismic destruction of an EH I site followed by land subsidence. This led to the abandonment of the site, which was reoccupied when the land was uplifted again.

Type
Articles
Information
Annual of the British School at Athens , Volume 90 , November 1995 , pp. 17 - 21
Copyright
Copyright © The Council, British School at Athens 1995

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References

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7 Some modern analogies, though not associated with seismic motions, are the barriers in Holland and at Kalochori near Thessaloniki. See Papageorgiou, S., Stiros, S., Papavasiliou, P., and Moutsoulas, M., ‘Examination of the relationship between variations of the coastal topography and inhabitation history in Macedonia and Thrace’, in Proceedings of the Second Archaeometry Symposium (Thessaloniki, 1993)Google Scholar (in press).

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10 These rocks have been used extensively in antiquity, both in underground and exposed constructions, for example Glauke Krene at Corinth. At Skaloma ancient excavations in such rocks have survived.

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14 Pirazzoli et al. (n. 3).

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