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SHOGHIK TADEVOSYAN In addition to asymmetrical power and hegemonic interaction, Zeitoun and Warner offer three pillars of hydro-hegemony, including riparian position (upstream/downstream), power (all three dimensions of power mentioned above), and exploitation potential (technical capacity). It is argued that if the state is in the upstream position, technically it has more water and can dam it, in this way preventing the flow of water into the downstream country. The second and third pillars of the framework of hydro-hegemony are crucial because even if the state is on the top of a river, if it does not have the sufficient amount of money to build dams and does not know how to build them, the upstream position will not help. Namely, the state does not just need favorable geography, but it also needs exploitation potential. 41 All this becomes more complicated when talking about the environment, particularly natural resources, as it is fraught with risks and uncertainties (lack of conflict resolution mechanisms, distrust between riparian states, etc.). The rational management of transboundary natural resources requires cooperation between the parties, otherwise ‘the tragedy of commons’ may occur. In addition, political uncertainty entails the independent actions of the hegemon which are qualified as ‘unilateral environmentalism’ in order ‘to protect [themselves] unilaterally from transboundary spillover effects’. 42 If there is a (political) conflict between the riparian states, the situation of ‘environmental unilateralism’ is exacerbated by leading to more independent actions and the unilateral framing of issues by the hegemon, as in the Israeli-Palestinian conflict. Data Analysis The Jordan River Basin The Jordan River Basin, with an area of approximately 18.500 square kilometers and length of 250 kilometers, borders Jordan (40%), Israel (37%), Syria (10%), the West Bank (9%), and Lebanon (only 4%). The river originates from the convergence of three headwaters, the Dan River, the Banias River, and the Hasbani River, and their convergence point is located 5 km south of Israel’s northern border. It joins Lake Tiberias, flowing through the Hula Valley. From Lake Tiberias the Lower Jordan River outflows and, joining the Yarmouk River, flows southward                                                              41 Zeitoun and Warner, “Hydro-hegemony – a Framework for Analysis of Trans-boundary Water Conflicts.” 42 Itay Fischhendler, Shlomi Dinar and David Katz, “The Politics of Unilateral Environmentalism: Cooperation and Conflict over Water Management along the Israeli- Palestinian Border,” Global Environmental Politics 11, no. 1 (2011): 39 95