Wadi El-Asyuti is encompassing promising areas for the futureprojects of agricultural utilization, however, its soils are occupied an area ofthe Eastern Desert of Egypt. According to the aerial photo-interpretationtechnique, the identified main landforms could be assigned to five units, i.e.,Wadi plain, Wadi bottom, Rubble terraces, Alluvial fan, River terraces andRocky area. The developed soils on these units were investigated throughoutten representative soil profiles. The obtained results indicated that the studiedsoils are characterized by texture class varies of sandy-silty clay loam, CaCO3content of 1.2-37.7 % and organic matter content of 0.05-0.61 %. Also, the soilsalinity of the investigated soils ranged between non-saline to extremely-saline,soil pH tended to alkaline side, and soluble cations were generally categorizedin an ascending order of Ca++ > Na- > Mg++ > K+ vs soluble anions of SO4-- ≥ C1,which were alternatively dominated and both exceed soluble HCO3-.Soils of coarse texture class have the highest soil bulk density values(Wadi plain and Rubble terraces soils), while the relatively fine texture soils(Alluvial fan and River terraces soils) have the lowest ones. On the contrary,soil total porosity values exhibited an opposite trend, the highest values wererecorded in case of the fine soil texture and tended to decrease with increasingcoarseness of soil texture. Also, the greatest values of hydraulic conductivityare associated with the soils of coarse texture class, and then decreased in thefine textured soils of alluvial fan and River terraces soils. In addition, availablesoil moisture range coincides very well with textural variations among soilprofile layers. Moreover, the CEC values are more related with soil textureclass, besides an exchangeable sodium percentage indicates that the studiedsoils are non-sodic.Statistical size parameters revealed that the studied soil sediments ofWadi El-Asyuti are mostly transported and deposited through an aqueousenvironment, and locally combined action of aqueous-aeolian media. Withregard to the mineralogical composition of the studied soils, the obtained datashowed that heavy minerals are detected as opaques, pyroxenes and amphibolesin high amounts. Also, the ultra stable minerals of zircon, garnet and rutile arepresent in relatively moderate amounts, while the remaining ones are detectedin less pronounced amounts. The ratios of ultra stable minerals and weatheringvalues indicate that soils of Wadi El-Asyuti are formed of either multi-origin ormulti-depositional regime, due to the heterogeneity of the parent materials priorto inception to geogenetic weathering or resulted in from the geochemicalweathering prevailed in the source sediments.