The mineral topsoil in 52 sites with different soil type under natural forests of Quercus petraea was studied in the northwest of the Iberian Peninsula. As a result of the anthropogenic influence, most of these forests are situated where the topography complicates their harvesting. The substrates are siliceous and the soils are mainly regosols. These soils are more frugal than soils under other oaks (Q. robur and Q. pyrenaica) that occupy the largest surface in the zone. The chemical properties were similar to those reported as the optimal for oak forests in the study area: pH very homogeneous, giving rise to typically acidic soils, disabling desirable conditions for humification, as verified by C/N ratio values and the presence of moder type humus. Although the base cations can be considered as high compared with Q. robur soils (except for copper), the phosphorus in the topsoil was clearly less (12.6 versus 21.8 ppm), indicating that these are mature forests that have not undergone changes in land use. Significant differences between soil types, chemical composition (pH, nitrogen, phosphorus, iron, and zinc) and topsoil fertility were observed. In the same way, the analysis of site conditions showed the existence of statistical differences with pH, zinc, C/N ratio, magnesium and copper content. The ecologic variables with the highest number of significant relationships with the topsoil parameters were altitude, annual precipitation and annual mean temperature.