Abstract: Pedogeochemical sampling over an area of 45 Sq.Km was initially taken up in the Chitrial outlier, which is actually detached from the main Srisailam sub basin as a result of topographic low formed through weathering and erosional processes. Pedogeochemical sampling is carried out on a grid of 1Km x 1Km and various geochemically associated trace and ore elements viz., U,Th,V,Cr,Co,Ni,Cu,Pb,Zn and As are analyzed and studied for their dispersion patterns. The pedogeochemical dispersion pattern of trace elements studied in conjunction with geology and structure has yielded an area of 11 Sq.Km which is identified with specific trends (N-S and NNE-SSW), as a potential zone for uranium mineralization and is recommended for detailed and subsurface investigations.