2012
DOI: 10.1016/j.quaint.2011.05.017
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A palaeogeographic reconstruction of the seafront of the ancient city of Delos in relation to Upper Holocene sea level changes in the central Cyclades

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Cited by 27 publications
(25 citation statements)
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“…This gradual sea level rise of ca. 1 mm/yr for the area is not consistent with the magnitude of submersion over the last 2000 years, the morphology of the stepped shorelines in front of the Roman fish tanks and the development in distinct phases of the extended beachrocks that require long periods of sea level stability and abrupt sea level changes between different phases (Pirazzoli, 1986;Furlani et al, 2010;Mourtzas, 1990 and2012a). Moreover the prediction of the glacio-hydro-isostatic change of sea level in an intensively active tectonic area, such as central and eastern part of Crete, is overestimated 0.26 m at least, proving, as also Pirazzoli (2005) supports, that the rapid isostatic rates of glacio-isostatic models for active tectonic regions of central and eastern Mediterranean, are unrealistic.…”
Section: Discussionmentioning
confidence: 95%
See 1 more Smart Citation
“…This gradual sea level rise of ca. 1 mm/yr for the area is not consistent with the magnitude of submersion over the last 2000 years, the morphology of the stepped shorelines in front of the Roman fish tanks and the development in distinct phases of the extended beachrocks that require long periods of sea level stability and abrupt sea level changes between different phases (Pirazzoli, 1986;Furlani et al, 2010;Mourtzas, 1990 and2012a). Moreover the prediction of the glacio-hydro-isostatic change of sea level in an intensively active tectonic area, such as central and eastern part of Crete, is overestimated 0.26 m at least, proving, as also Pirazzoli (2005) supports, that the rapid isostatic rates of glacio-isostatic models for active tectonic regions of central and eastern Mediterranean, are unrealistic.…”
Section: Discussionmentioning
confidence: 95%
“…In the area of the Cyclades, the coasts of Delos have submerged by a total of 2.15 m since the end of the Hellenistic period. This lowering occurred during two distinct successive phases of submersion, initially by 1.35 m and then by another 0.80 m (Mourtzas, 2012a).…”
Section: Discussionmentioning
confidence: 97%
“…Important aspects of these studies include geomorphological consequences and human implications. Most of the relevant research has been conducted in western Crete [31][32][33], in Rhodes [34], and in the Cyclades at Delos-Mykonos-Rhenea [35,36], Keos [37], Andros [38] and at Paros [39].…”
Section: The Aegean Basinmentioning
confidence: 99%
“…Baika, 2008;Poulos et al, 2008;Kapsimalis et al, 2009;Pavlopoulos et al, 2011;Mourtzas, 2012;Evelpidou et al, 2012a;b;. Using beachrocks in particular, the most extensive work was…”
Section: Study Areamentioning
confidence: 99%