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TINA


                                                                         Maritime Archaeology Periodical







































                                                                                     Fig. 2: 1770 yılına ait J. L.
                                                                                     Cowley’in haritası ve Vor-
                                                                                     donisi Adası.
                                                                                     Fig. 2: J. L. Cowley’s 1770
                                                                                     map and Vordonisi Island.

              A review of the evolution of the Marmara Sea, which  period .  Vordonisi  should  also  have  become  an  island
                                                                   9
             was once a lake, it appears that Marmara Sea met the  during this period. Most probably due to sea level rise
             salt water from the Aegean Sea by crossing the Darda-  and tectonic movements, it should have sunk into the wa-
             nelles  around  7000  BC.  The  connection  of  the  Sea  of  ters of Marmara Sea over time. However, it is not known
             Marmara with the Black Sea was probably around 5500  exactly when the island vanished.
             BC . Based on the elevation of the Neolithic settlement   Between 858 - 867 AD and 877 – 886 AD, photios, the
               5
             of Yenikapi, the sea level was less than minus 6 meters  patriarch of Constantinople, was sent to exile to the Ar-
             9-8 thousand years before today. Accordingly, the Sea of  monians or Armenians Monastery in Vordonos . There
                                                                                                      10
             Marmara at the beginning phase of the Fikirtepe Culture,  is a strong possibility that the rocky region known among
             which is called the Archaic phase, should have been at  the sailors as Büyük (Big) Vordonos and Küçük (Small)
             a level 15 to 20 meters lower than the present-day ele-  Vordonos was in fact the Vordonisi Island, which was
             vation . For this reason, the prince Islands should have  once above the sea level, but sank into the sea due to
                  6
             been linked to the mainland during the Neolithic peri-  massive earthquakes and floods over time. An analysis of
             od .  However,  Yarımburgaz  4-0  material  was  reported  the earthquakes that occured in the region and the tsuna-
               7
             in  Yenikapi  today  under  the  Marmara  Sea  level .  The  mis triggered by these earthquakes shows that there was
                                                      8
             settlements  between  today’s  Anatolian  coastal  borders  a tsunami in the Eastern Marmara due to an earthquake
             and prince Islands should have been flooded during this  in 989 AD .
                                                                       11
             5  ALGAN et al. 2011, 30; for relevant arguments see RYAN et al. 1997; AKSU et al. 1999; ÇAĞATAY et al. 2000; GÖRÜR et al. 2001; HIS-
            COTT et al. 2002
            6  Although the exact dating of the finds that belong to the Archaic Phase of the Fikirtepe Culture was not established, similar materials recovered
            from the Yenikapı excavations are dated to 6400-5800 BC based on C14 data (ÖZDOĞAN 2013, 173, fig. 12).
            7  ALGAN et al. 2011, 44; ÖZDOĞAN 2013, 175.
            8  For detailed information on the Yarımburgaz 4 layer and materials dating to the Chalcolithic Age, see ÖZDOĞAN et al. 1986, 12; ÖZDOĞAN
            1990, 382, Plt. 246-248, figs. 4a-b, 5b-c, 6a-b.
            9  ÖZDOĞAN 2015, 15, fig. 6.
            10  WHITE 1981, 36.
            11  SOYSAL 1985; ALTINOK et al. 2001, 530.
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