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. 5,354.45 Haploxeralfs Torriorthents Lithosols and Xerosols Eastern slopes Marl, chalk, limestone and conglomerates parent rocks. Parent material is loessial sediments. Haplargids Lithosols and Yermosols Steep to moderate mountain slopes Of yellowish brown or very pale brown color, coarse texture and subangular structure. Parent rocks are limestone, chalk, dolomite and flint.