Leached cappings are limonitic bodies that form due to supergene processes at the top of porphyry copper deposits. According to the formation mechanism of these bodies, one can estimate the caracters of the hypogene porphyry stock and the intensity of supergene effects. These cappings are jarositic, goetitic and hemetitic bodies that dominance of each cappings, indicate the type and amounts of hypogene sulfide mineralization and supergene enrichment beneath the water table. Sonajil porphyry copper deposit is a porphyry body and demonstrates common hydrothermal alterations such as potassic, phyllic, argillic and propyllitic. Compositionally, sonajil porphyry is diorite, and hypogene minerals such as pyrite, chalcopyrite, bornite, solfosalts (tetrahedrite-tenentite, enargite), Molybdenite, Magnetite and hematite occur as disseminated, micro-veinlets, veinlets and veines. Varous proportions of limonitic minerals formed in these cappings. Predominantly, capping samples are brown in color and they seem to be goetitic. Also, based on chemical analysis, the majority of samples are composed of goetite and jarosite and minor hematite. The presence of goetitic capping is an evidence for lack of development of supergene enrichment and the insufficient amount of pyrite for producing acid responsible for leaching of copper from oxide zone, thus we can't expect high supergene enrichment. The results are verified by bore hole drilling.