Mediterranean–Dead Sea Canal in 1855 in a work called 'The Dead Sea – A new route to India'. At that time it was not yet known that the Dead Sea lies below sea level, and Allen proposed this canal as an alternative to the Suez Canal. Later, many engineers and politicians picked up on the idea, including Theodor Herzl in his 1902 novel "Altneuland". Most of the early proposals used the East bank of the Jordan River, but a modified form, using the West bank, was proposed after the separation of Transjordan from the Palestine Mandate. The idea was discussed at some length
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