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Developed by a geological structure similar asymmetric horst, Anieș's morph-hydrographic basin presents through its relief forms, a complex geographical unit, in terms of morphometric indicators respectively altitude, slope, depth of fragmentation and slope exposition for the entire landscape. At a taxonomic level, we can distinguish a variety of soil types and subtypes, mainly due to the physical and chemical properties and mineralogical soil deposits. This article aims to interpret some morphometric indicators and correlations supported by a GIS raster and vector database integrated in spatial analysis modules, discover quantitative and qualitative features of various types of surfaces and define morphometric parameters.The morphometric study of: slope, slope exposition and energy relief correlated with altitude by indirect mapping, have identified the following types of zone soils: luvisols, eutric cambosols distric cambosols, podzols, prepodzols , criptopodzols and humosiosols and intra-zone soils: rendzins, lithosols, hystosols and fluvisols. The indirect maping reflect the variety and complexity of soil types in Anieș's basin, each with varying surfaces, lithological substrates and specific properties.The necessity of this article is important in the achievement of studies concerning the land usefulness, in order to implement essential measures such as: correcting the soil's acidity and monitoring the lands affected by soil erosion.

Morphometric Characteristics of the Relief as a Premise in the Pedogenetic Process and Indirect Mapping of Soil Types in the Anieş Hydrographic Basin