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dike is periodically opened, allowing excess water to flow into the largely dried-up Southern Aral Sea."[11] Discussions had been held on recreating a channel between the somewhat improved North and the desiccated South,[7] along with uncertain wetland restoration plans throughout the region, but political will is lacking. Uzbekistan shows no,
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was the diking and reclamation of the IJsselmeer.In the micro tidal area, (a tidal range of up to 1.35 m (4.43 ft)), such as on the Dutch or Danish coasts,[43] barrier beaches with dunes are formed. In the mesotidal area (a tidal range of between 1.35 and 2.90 m (4.43-9.5 ft)), barrier islands are formed; in the macrotidal area (above 2.90 m, 1919191919.