Beveridge Building
Inspections

Beveridge soil, basalt and slab movement

Beveridge sits on the volcanic plain around Mount Fraser, an extinct scoria cone that rises above the surrounding basalt country. Clay soils over basalt in Melbourne's north are often reactive, swelling when wet and shrinking when dry. The site class for your lot comes from its own soil report under AS 2870, and the slab design follows that class.

Read your soil report

The classification is lot specific. Two lots in the same street can differ, especially where fill or rock is involved.

Why slab beams matter

On reactive ground the stiffness of the slab comes from its beams. Pods pushed into beams make them narrower than the design assumed.

Water is the trigger

Uneven wetting drives movement. Downpipes discharging at the slab and garden beds that hold water against one side of the house are what start it.

Signs to look for

Doors that start to bind, cracks that open and close with the seasons and floors that drift out of level. We measure these against the tolerances guide.

Slab drains

Some Beveridge engineering includes a slab drain on the boundary side to stop water migrating under the slab. We check it is there at frame.

More about Beveridge

Written by our local inspection team from work carried out in Beveridge. Licensed building practitioners, Building & Plumbing Commission registration CDB-U 53425.

Guides

Guides for Beveridge owners and buyers

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FAQ

Beveridge soil, basalt and slab movement: common questions

What site class is Beveridge?

There is no single class for the suburb. Read the soil report for your lot, which sets the class your slab was designed for.

Will my slab crack?

Some fine shrinkage cracking is normal. Wider or growing cracks are measured and categorised to decide whether they are a defect.

Can you check slab level?

Yes. We measure level at frame and at handover against the tolerance for each room.

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