Soil structure is crumbly. Parent material is soft chalk and marl. Pinus halepensis and Pistacia palaestina . Haploxerolls Valleys and depressions Xeric moisture regime. It has dark reddish brown color with clay and with gentle slope.
Parent rocks are marl and chalk.
Quercus ithaburensis, Pistacia lentiscus, Ceratonia siliqua and Ballotetalia undulatae. Parent material is loessial sediments. Ballotetalia undulatae, Artemisietea herbae-albae. Loessial Arid Brown soils 440 Palexeralfs Haploxeralfs Xerochrepts gently sloping plateau and dissected plateau Parent rocks are conglomerate and chalk.