The Dead Sea is losing its water supply
The Dead Sea has no outlet: water flows in, but none flows onward to the ocean. Its level depends largely on inflow from the Jordan River and nearby streams, balanced against intense evaporation in the hot, dry basin. In recent decades, much less river water has reached the lake, in part because people divert it for farms and households. Mineral industries also use water from the lake and its connected system. With too little replenishing the basin, the shoreline keeps retreating.
A retreating shore leaves unstable ground
As the lake drops, the water table—the underground water level—can fall too. Fresh groundwater then moves through buried layers of salt left behind by earlier stages of the lake. When that water dissolves the salt, empty spaces form underground; eventually, the ground above can collapse into sinkholes. Roads, farmland, and visitor sites near the shore may be damaged or become unsafe, and some areas have had to close or relocate facilities.
These sinkholes are a consequence of the changing landscape, not simply holes opened by the salty lake itself. Their locations can be difficult to predict, which complicates building and tourism along the exposed shore.
The crisis is visible in the changing map
The retreat affects more than the view from a beach. It reshapes wetlands and shore habitats, shifts the places where people can safely reach the water, and puts pressure on local communities and businesses. Reversing the decline would require addressing the imbalance between water entering the basin and water being removed or lost—especially the reduced flow reaching it from the Jordan River. The striking change is that a lake famous for making visitors float is steadily moving away from the very shore they came to visit.
