The suitability of a lateritic soil developed on olivine basalt in wes
tern southeast Queensland, Australia, as paving material has been inve
stigated. The particle size distribution and plasticity characteristic
s of the soil do not comply with the standard specification for paving
materials. However, the soil has a high shear strength, resulting in
a low Western Australian Confined Compression Test class number. The h
igh shear strength of the soil at its in situ moisture content is due
to its high angle of shearing resistance and its suction under in situ
moisture conditions. Volumetric shrinkage of the soil does not consti
tute a problem as its shrinkage is low. The in situ strength of a pave
ment constructed with the lateritic soil, determined using a Clegg imp
act hammer, and the field dry density, have increased with time and th
e passage of traffic since construction. The pavement performance was
good. A criteria suitable for the selection of a lateritic soil as pav
ing material under the climatic conditions prevailing in western south
east Queensland has been suggested.