SpaDiS is a revolutionary approach to the spatial analysis of point data using geometry to analyse geometry! SpaDiS uses each and every spatial relationship and is not dependent on mathematical models. For n points there are n2 - n spatial relationships and, because of the square function, the method yields interpretable results for both small and large data sets. SpaDiS is an alternative to variography for directional studies. At the regional scale, the analysis can assess distribution patterns of mineralisation and potential controlling structures. At the deposit scale, the characteristics of zones of mineralisation such as direction, spacing, high-grade ore direction and grade distribution can all be deduced.