Wadi Mujib - Geography of Mujib

Geography of Mujib

During the last Ice Age the water level of the Dead Sea reached 180 m below sea level, about 230 m higher than it is today. It flooded the lower areas of the canyons along its banks, which became bays and begun to accumulate sediments. As the climatic conditions changed, about 20,000 years ago, the water level of the lake dropped, leaving the re-emergent canyons blocked with lake marl. Most canyons managed to cut through their plugged outlets and to resume their lower courses. However, Wadi Mujib, the biblical Arnon River, abandoned its former outlet by breaking through a cleft in the sandstone. This narrow cleft became the bottleneck of an enormously large drainage basin with a huge discharge. During the years the cleft was scoured deeper and the gorge of Wadi Mujib was formed.

The Mujib reserve consists of mountainous, rocky, and sparsely vegetated desert (up to 800 m), with cliffs, gorges and deep wadis cutting through plateaus. Perennial, spring-fed streams flow down the wadis to the shores of the Dead Sea which lies 400 m below sea-level.

The slopes of the mountaineous land are very sparsely vegetated, with a steppe-type vegetation on plateaus. Groundwater seepage does occur in places along the Dead Sea shore, for example at the hot springs of Zara, which support a luxuriant thicket of Acacia, Tamarix, Phoenix and Nerium, and a small marsh. The less severe slopes of the reserve are used by pastoralists for the grazing of sheep and goats.

The hot springs of Hammamat Ma'in lie close to the borders of the reserve are heavily used for tourism/recreation.

The Jordanian military have a temporary camp in the south of the reserve.

A large dam was recently finished at the bottom of the wadi, where the modern road crosses the river. As a result, a large lake has formed. Today, Wadi Mujib is fed by seven tributaries.