The aquifer which forms the main water supply for the municipalities of MalmoÈ and Lund owes its value to the deposition of coarse sands during the deglaciation of the late Weichselian ice. Spatial statistical analysis based on construction of the variogram has been applied to the hydrauli c conductivity of this aquifer. This has identiWed an anisotropic distribution of the geohydrologica l properties with the least continuity striking in a north-northwes t direction, consistent with the believed Xow direction of the Weichselian melt-water streams which deposited the coarse sands. The application of geostatistical estimation (kriging) to model the distribution of hydraulic conductivity within the aquifer has honoured the depositional controls, notably the increased hydraulic conductivity towards the ice-proximal parts of the deposit.