Primary natural vegetation on this soil was destroyed. Today there is segetal vegetation of the Prosopis farcata scolymus maculatus. The American great group classification that represent this soil association are Xerorthents, and Haploxerolls . Parent material is loessial sediments. Ballotetelia undulatae, Artemisietea herbae.
Soil structure is crumby.
Parent material is soft chalk and marl. Pinus haleness and Pistachio palaestina. 600-700 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.