Egidio Ivetic

History of the Adriatic


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the Eastern Mediterranean. A large Adriatic existed in the tertiary period, covering the whole Po Plain as far as modern Piedmont. Unlike in any other European context, closed in by the Alps and the Apennines, the plain seems, and actually is, a continuation of the sea. There was also a second smaller Adriatic. Twelve thousand years ago, early people could walk from Marche to Dalmatia as the sea level was a hundred metres lower than it is today, and the mainland went as far as south of Ancona where the early Po River flowed into the sea. After the last ice age, between 12,000 and 8,000 years ago, the sea level rose, and the Adriatic took on its current form. On the east coast, the string of Dalmatian islands is actually the peaks of the coastal Dinaric mountains whose valleys have been submerged. Over the last 2,000 years, the mouth of the Po River has spread out in numerous branches and has moved closer to the open sea.

      Wishing to measure the states that gravitate towards the Adriatic, the 2012 demographic picture was as follows: Slovenia had 2 million inhabitants, Croatia 4.2 million, Bosnia and Herzegovina 3.8 million, Montenegro 0.6 million and Albania 2.8 million. In other words, there were 13.4 million inhabitants on the east coast.8 In the same year, the Italian Adriatic regions had a total of 17.9 million inhabitants. Nevertheless, Emilia-Romagna and Veneto alone had more than 10 million inhabitants, compared to Marche, Abruzzo and Molise, which together numbered 3.1 million, or Apulia with 4 million. This is a population of 31.3 million people, slightly less than that of Canada (35 million) and Morocco, and almost double the total populations of Norway, Sweden and Denmark. This is, however, only a tenth of the population that gravitates towards the Mediterranean, which today numbers approximately 400 million inhabitants.

      The people who live on the Adriatic divide the sea into three sections: upper, middle and lower Adriatic. The dividing lines run between Ancona and Zadar (Zara) (upper/middle), and Gargano and the Bay of Kotor (middle/lower). The criteria for these divisions are certainly geographical and historical, but they also lie in deeply rooted customs, such as the traditional familiarity in relations between the Veneto and Istrian regions, between the Romagna, Marche, Abruzzo and Dalmatian regions, and between the regions of Apulia and Albania. The features of the three sections alternate, and also complement each other in terms of coastal type of marine life. Romagna and the lagoon basins between the Po and Isonzo rivers, which were historically centred around Venice and are places in which the Po, Veneto and Friulan plains literally once lay in the sea, are offset with Istria and the Karst region, almost a central European wedge, as well as the Kvarner Gulf (Quarnero) and the 140-kilometre long Velebit mountain range, northern Dalmatia. Opposite linear Apennine middle Adriatic lies jagged Dalmatia. Opposite densely populated flat Apulia lie the scarcely populated Montenegrin and Albanian mountains.