The problem of identifying and mapping local soil variations over a un
iform geological material is examined. Soil mapping units, defined geo
morphologically, are compared and classified in terms of silt and clay
contents, using a fixed-effects ANOVA model. Most of the units, forme
d on a single rock type, are significantly different in terms of topso
il or subsoil character, or both. The differences are associated with
contrasts in the genesis, relative age and geomorphological process re
lationships of the corresponding landforms. The approach is not only e
ffective in resolving variations within a soil complex, but also can p
rovide an appropriate framework for planning land suitability assessme
nts.