Hydromorphometric analysis as a method is considered one of the most reliable and
used methods in solving hydrological problems. Where it is possible to know the volume
of runoff and the rest of the elements that enter into the water balance. Geographical
Information System and Remote Sensing is the technique that used the hydro-morphometric
analysis of the Wadi Al-Mohammadi basin. Wadi Al-Mohammadi, located in the Western
Desert, is one of the main valleys that flow into the Euphrates River. It is considered
an important basin, because of its many characteristics, including its relatively large
area and the amount of water drained through, which is used mainly in watering livestock
and agriculture, in addition to industrial purposes such as the production of washed
sand, gravel that scattered on both sides of the valley. The hydrological analysis
included several steps, which gave the results of the flow accumulation with the highest
value in the lower part of the basin. The results represented by form characteristics
confirm that the shape of the basin is far from the round shape, which reflects the
basin’s characteristics with the regular surface flow in time and relatively low
drainages. Wadi Al-Mohammadi basin has reached the 5th order to flow into the Euphrates
River. It has two types of drainage patterns, the dendritic pattern, and the parallel
pattern. Wadi Al-Mohammadi basin is categorized as extremely low drainage density, very
low drainage frequency, very coarse drainage texture, lower infiltration number, and low
relief slope. Based on the results, the basin is characterized by an almost flat plateau
surface, with a gradual slope homogeneous and good permeable soil conditions, and in
other parts influenced by the structural phenomena under the surface, the high
permeability of sediments over which streams pass, higher the infiltration and lower
runoff.