Wollert soil: reactive basalt clay, AS 2870 and why slabs crack
Wollert sits on the Victorian Volcanic Plain. Reported soil conditions comprise a layer between 0.2 and 2.9 metres thick, averaging around a metre, of very stiff to hard high plasticity silty clay over basalt rock. High plasticity residual basaltic clay is the reactive material that drives seasonal movement, which is why edge drainage and slab design matter so much here. Wollert also contains the Wollert Resource Park, roughly 350 hectares with a basalt quarry running since the late 1970s and a landfill operating in previously quarried ground since 2000.
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The reactive layer is high plasticity silty clay, typically about a metre thick over basalt.
Thickness varies widely, from 0.2 to 2.9 metres, so neighbouring lots can differ.
Drainage against the slab edge is what controls seasonal movement in this material.
The Wollert Resource Park quarry and landfill is a documented local ground condition.
Your soil report carries the classification for your block. Nothing here substitutes for it.
More about Wollert
- Building a new home in Wollert: stages, ground and what goes wrong
- Buying a house in Wollert: prices, stock and what to check
- Wollert growth: the precinct structure plan, dwellings and infrastructure
- Building permits, the City of Whittlesea and the dispute path in Wollert
- Termite risk in Wollert: timber frames, management systems and what to check
- The defects we record most often on Wollert inspections
- Wollert site conditions: wind classification, climate zone and planning overlays
Written by our local inspection team from work carried out in Wollert. Licensed building practitioners.


