Melbourne's rapid expansion into outer growth corridors like Werribee and Cranbourne has pushed development onto former floodplains and agricultural land. The city's geology is far from uniform, with Quaternary basalt flows covering the west, while eastern suburbs sit on deep Silurian mudstone profiles. This patchwork of stiff clays, sandy alluvium, and compressible silts demands a solid geocell design that can accommodate differential settlement and lateral spreading. In our experience, the most successful projects blend cellular confinement systems with proper subgrade evaluation, often coupling the geocell layout with a thorough study of infiltration rates to manage stormwater beneath the pavement structure.

Geocell design in Melbourne's swelling clays requires seasonal moisture modelling; a 150 mm cell depth on low CBR subgrades is the typical starting point.