Weathering experienced by rocks and minerals Denganthza Hill deposits have been studied by fluorescence analysis in order to assess and quantify the geochemical weathering profiles. Weathering intensity was quantified using different alteration rates (PWR, Potential Weathering Rate, WR, Weathering Rate, AR, Alteration Rate, CAR, Chemical Alteration Rate) The geochemical evolution suffered by the samples were analyzed using the Chesworth (1979, 2000) triangular diagrams and A-CN-K, the binary variation diagrams or Harker and alkali-silica (Le Maitre, 1989). Na2O, K2O, Fe2O3, TiO2 concentrations are greatly reduced in the weathering products, and instead the Al2O3, CaO y MgO concentrations increase indicating an early stage in development of soils, reflecting a poor material alteration. SiO2 versus K2O + Na2O content indicate that the samples of Denganthza Hill are dacite, andesite and mostly picrobasalto foiditas.