Water politics in the Jordan River basin floodplain, the "zhor" (or "Zur"), with a wildly meandering course, which accounts for the excessive length of the river in comparison to the straight-line distance to reach the Dead Sea. Small dams were built along the river within the Zhor, turning the former thickets of reeds, tamarisk, willows, and white poplars into irrigated fields. After flowing through the Zur, the Jordan drains into the Dead Sea across a broad, gently sloping delta. In the upper Jordan river basin, upstream of the Sea of Galilee, the tributaries include: The lower Jordan River tributaries include: The riparian rights to the Jordan River
Dead Sea in the northern part of the Dead Sea and barely in the southern part. The Dead Sea zone's aridity is due to the rainshadow effect of the Judaean Mountains. The highlands east of the Dead Sea receive more rainfall than the Dead Sea itself. To the west of the Dead Sea, the Judaean mountains rise less steeply and are much lower than the mountains to the east. Along the southwestern side of the lake is a tall halite formation called "Mount Sodom". There are two contending hypotheses about the origin of the low elevation of the Dead Sea. The older