The total length of Wadi Hatta is '
, of which run in Emirati territory, and in Omani territory. Its river source is located in the territory of Oman, at an approximate altitude of , on the southern slope and a very short distance from the summit of Jabal Hatta', also known as Um Alnosoor (). From Al Khattem Dam, the Wadi Hatta continues its course from west to east, receiving the confluence of the Wadi Wahiyah on the left. Also on its left bank, on the other side of the E44 highway, in the territory of the Emirate of Dubai, and less than 300 meters from the wadi bed, there are traces of large quarries, currently abandoned, whose activity caused a great
environmental impact, with irreparable damage to the natural environment, destroying a large part of the mountain and the courses of several small wadis tributaries to Wadi Hatta. Already in the territory of the Sultanate of Oman, the Wadi Hatta receives from the right the confluence of its main tributary, the
Wadi al Qahfi, long, very popular for hosting along its course numerous natural ponds and freshwater pools, accessible by vehicle through a dirt track. Some visitors and several Emirati tourist information portals confuse this wadi with Wadi Hatta, and one of the most frequented pool areas is wrongly called
Hatta Pools. In its lower course, the Wadi Hatta converges with another important tributary, the
Wadi Khabab, long, and a minor tributary: the
Wadi Sufaydah. In the final stretch, through the wide fan that forms its extensive
alluvial plain and as often occurs in other plains of similar morphology, the Wadi Hatta branches into multiple
braided channels, intertwined and interspersed with small islands of coarse sediment. Over time, the wadi's current tends to wander between torrential rains, altering the previous courses, which nevertheless maintain their mark on the plain. == Dams and reservoirs ==