Soil, slabs and movement in Clyde VIC
Clyde sits on completely different ground to the western and northern growth corridors. Where those are Newer Volcanics basalt with highly reactive residual clay, the geotechnical study prepared for the Clyde Creek and Thompsons Road precinct structure plans maps this area as Baxter Sandstone and associated sedimentary units, with a dominant profile of silty sand or sandy silt over silty clay. That makes most of Clyde markedly less reactive than Tarneit or Melton South. The issue that replaces shrink-swell is soft, compressible ground: lagoon and swamp deposits through parts of the precinct, and numerous old farm dams whose backfill quality is unknown.
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Clyde is sedimentary ground, not basalt. Less shrink-swell than the western corridor.
The dominant profile is silty sand or sandy silt over silty clay.
Soft lagoon and swamp deposits appear through parts of the precinct.
Old farm dams were backfilled to unknown standards, which is a settlement risk.
Your own soil report still carries the classification for your lot. Nothing here replaces it.
More about Clyde
- Building a new home in Clyde VIC
- Buying an established home in Clyde VIC
- Growth and development in Clyde VIC
- Permits, council and building disputes in Clyde VIC
- Termite risk and pest inspections in Clyde VIC
- What our inspectors find in Clyde VIC
- Wind classification and site conditions in Clyde VIC
Written by our local inspection team from work carried out in Clyde. Licensed building practitioners.


