Identita del Mediterraneo: elementi russi
In this paper the differences and the similarities of formation of legal traditions in the Medieval Europe are examined. The author analyzes the impact of these differences on the consequent development of legal mentality and legal identity in Russia and in the Western Europe.
In the last decade Russia has searched for new alternative policies to compensate for its political deficiencies and to balance its rivals in one of the key areas of the approaching geopolitical rivalry, the sea. The Russian assertiveness seen in the Black Sea-Mediterranean basin has recently been a real concern for the international community. In the six chapters of this book, contributors explain Moscow’s newly perceived assertive foreign and security behavior in the Black Sea and Mediterranean basin from their own perspectives, and reach a conclusion about the limits and validity of this new Russian ascendance in the region.
The collective works consists of 27 articles of historians and philologists on different aspects of philhellenism and its influence in European culture and thought from eighteenth till twentieth centuries.
Tsunamis in the eastern Mediterranean and Red Seas, induced by earthquakes and/or volcanic activity, pose potential hazards to shipping and fixed harbor infrastructure within the Suez Canal. Potential vulnerabilities of the Suez Canal to possible tsunami impacts are reviewed by reference to geological, historical, archeoseismological, and anecdotal data. Tsunami catalogues and databases compiled by earlier researchers are perused to estimate potential return periods for tsunami events that could directly affect the Suez Canal and operational infrastructures. Analysis of these various records indicates a centurial return period, or multiples thereof, for long-wave repetition that could generally impact the Nile Delta, whereas numerical models indicate a multidecadal frequency. It is estimated that tsunami waves 2 m high would begin to break about 4 to 10 km down-canal, whereas a 10-m wave break would occur about 0.5 to 3 km into the Canal.