Seismic coastal uplift and subsidence in Rhodes Island, Aegean Arc: Evidence from an uplifted ancient harbour
Archaeological evidence from a 2400years old harbour, currently about 3m above sea-level, sheds light on an enigmatic sequence of coastal uplift and subsidence along the coasts of Rhodes Island, close to a >4km deep trough marking the east edge of the Aegean Arc. The tectonics of this area are no...
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| Published in | Tectonophysics Vol. 611; pp. 114 - 120 |
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| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
25.01.2014
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| Subjects | |
| Online Access | Get full text |
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| Abstract | Archaeological evidence from a 2400years old harbour, currently about 3m above sea-level, sheds light on an enigmatic sequence of coastal uplift and subsidence along the coasts of Rhodes Island, close to a >4km deep trough marking the east edge of the Aegean Arc. The tectonics of this area are not clear, because of the absence of major earthquakes in the last 80years, but are likely to be controlled by a combination of shear and compression producing strong earthquakes, some associated with tsunamis and some with thrust-uplifted notches. The latter, up to 6000years old, also show evidence of phases of subsidence.
Our study focuses on remains of shipsheds, in particular a ramp used to pull warships out of the water and keep them protected under cover during winter. This ramp was constructed between approximately 250–225BC and some decades later it was repaved, after a major earthquake destroyed the town of Rhodes and most probably the harbour and sheltered ships, as historical evidence reveals. 300years later the harbour was to a great part abandoned because of a coastal uplift. The only reasonable explanation for the ramp reconstruction was to counteract a 1m seismic subsidence at around 220BC or earlier. Several possible explanations can be proposed for the earthquake which produced seismic subsidence alternating with uplift in Rhodes, in a pattern of vertical motions different from that observed in Crete, or other convergent boundaries.
•Alternation of coastal uplift and subsidence in the Rhodes Island, Aegean Arc•Coastal subsidence-uplift recorded in remains of an uplifted ancient harbour•Refinement of ancient information for a major earthquake |
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| AbstractList | Archaeological evidence from a 2400 years old harbour, currently about 3 m above sea-level, sheds light on an enigmatic sequence of coastal uplift and subsidence along the coasts of Rhodes Island, close to a > 4 km deep trough marking the east edge of the Aegean Arc. The tectonics of this area are not clear, because of the absence of major earthquakes in the last 80 years, but are likely to be controlled by a combination of shear and compression producing strong earthquakes, some associated with tsunamis and some with thrust-uplifted notches. The latter, up to 6000 years old, also show evidence of phases of subsidence. Archaeological evidence from a 2400years old harbour, currently about 3m above sea-level, sheds light on an enigmatic sequence of coastal uplift and subsidence along the coasts of Rhodes Island, close to a >4km deep trough marking the east edge of the Aegean Arc. The tectonics of this area are not clear, because of the absence of major earthquakes in the last 80years, but are likely to be controlled by a combination of shear and compression producing strong earthquakes, some associated with tsunamis and some with thrust-uplifted notches. The latter, up to 6000years old, also show evidence of phases of subsidence. Our study focuses on remains of shipsheds, in particular a ramp used to pull warships out of the water and keep them protected under cover during winter. This ramp was constructed between approximately 250–225BC and some decades later it was repaved, after a major earthquake destroyed the town of Rhodes and most probably the harbour and sheltered ships, as historical evidence reveals. 300years later the harbour was to a great part abandoned because of a coastal uplift. The only reasonable explanation for the ramp reconstruction was to counteract a 1m seismic subsidence at around 220BC or earlier. Several possible explanations can be proposed for the earthquake which produced seismic subsidence alternating with uplift in Rhodes, in a pattern of vertical motions different from that observed in Crete, or other convergent boundaries. •Alternation of coastal uplift and subsidence in the Rhodes Island, Aegean Arc•Coastal subsidence-uplift recorded in remains of an uplifted ancient harbour•Refinement of ancient information for a major earthquake |
| Author | Stiros, Stathis C. Blackman, David J. |
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| SubjectTerms | Archaeoseismology Coastal Coasts Crete Earthquakes Harbors Harbours Historical seismology Islands Marine Radiocarbon dating Seismic phenomena Subsidence Thin-skin tectonics |
| Title | Seismic coastal uplift and subsidence in Rhodes Island, Aegean Arc: Evidence from an uplifted ancient harbour |
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