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Open Access Article

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Mapping Shoreline Changes Over the Years: The Case Study of Navarino Bay, Pylos, Messenia, Greece

George Malaperdas, Nikolaos Panagopoulos

World Journal of Geomatics and Geosciences 1(1); 10.31586/wjgg.2021.010103 - July 21, 2021

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Abstract

This paper deals with the mapping of shorelines through existing maps. Its main purpose is not to give an accurate change of sea level and shoreline in general, but to give guidelines to a more genera... Read more

Figure 1. The different locations where Pylos was placed over the years. However, especially Pylos in pre-historic era is intertwined with the whole wider area. The placement of the red pin refers to the so-called palace of Nestor.

Figure 2. Geology and present sedimentary environments of the Navarino area [Source: Kraft, 1980].

Figure 3. Shoreline changes of Navarino Bay. Late Helladic palaeogeographic reconstructions of the Nava-rino embayment, roughly 3500 years before the present. The map depicts known Helladic ar-chaeological sites. Ancient sea cliffs are linked to Neolithic (5000 B.P.) and Mesolithic (9000 B.P.) shoreline reconstructions. On the north flank of Coryphasium, one neolithic site is indicated [Source: Kraft, 1980].

Figure 4. Shoreline changes of Navarino Bay.

Figure 5. The four different changes of Navarino Bay shoreline, (a) the Mesolithic shoreline, (b) the Neolithic shoreline, (c) Helladic shoreline, (d) Present shoreline.

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