
Two geologies in one hole
Basalt clay formed 11 thousand to 2.5 million years ago, over Ordovician clay and weathered rock formed about 480 million years ago.
A soil site classification report to AS 2870 for a new home, extension, shed or pool. Tested by qualified staff who know soils and footing design, and backed by our professional indemnity and public liability insurance.
Less when combined with a feature survey, land capability assessment or bushfire assessment.
From acceptance to report, for most sites.
Subject to availability.

Ballarat has young volcanic basalt clay in some suburbs and ancient Ordovician clay and rock in others, with gold-rush mine shafts and mullock through both, and the change can happen within a single site. Our reports draw on our project history across Ballarat, historical aerial photos and geological mapping, so fill, old mine workings and reactive clay are found before your footings are designed.

Basalt clay formed 11 thousand to 2.5 million years ago, over Ordovician clay and weathered rock formed about 480 million years ago.

Mine shafts, mullock and deep fill turn up under Ballarat houses and building blocks. We dug into one house's cracking and found a mine shaft.

Fill placed over natural soil makes a site Class P. We have found fill four metres deep under one house.
Clay acts like a sponge. It shrinks when it dries and swells when it gets wet. How much your soil moves with normal seasonal moisture changes sets the class, and the class sets the footing design.
Most sand and rock sites, with little or no ground movement from moisture changes.
Slightly reactive clay sites, which may experience only slight ground movement.
Moderately reactive clay or silt sites, which may experience moderate ground movement.
Highly reactive clay sites, which may experience high ground movement.
Highly reactive clay sites, which may experience very high ground movement.
Extremely reactive sites, which may experience extreme ground movement.
Sites that cannot be given a normal class, because of fill, abnormal moisture from trees, buildings or drainage, soft or collapsing soils, past mining or slope instability.
Class P does not mean a site without solutions. AS 2870 requires it whenever a site's soil is not in its natural state, and few house blocks are. Street trees and subdivision fill in new estates, or the existing house on a renovation, are usually enough. Most Class P sites need solutions familiar to most builders, and an engineer designs the footings to suit.
Clear enough for an owner, detailed enough for the engineer who designs your footings. In most cases the person who tests your site also designs or helps design your footings, so nothing is lost between the report and the drawings.
Your site class and the site constraints, explained briefly and clearly.
Historical aerial photos of your site, including before and after subdivision, plus Geovic, Council, subdivision and archive records where they help.
An excerpt of the geological map of Victoria locating your site.
The recommended foundation soil, bearing capacity, and minimum and typical founding depths for each footing type.
Design responses to the site constraints, for example an H1 equivalent slab on a moderately reactive site affected by trees, or a fully suspended slab on bored piers where there is fill or mining.
Combining site services in one visit costs less than booking them separately.
Call during business hours, or send the details and a few photos and we will be in touch to talk it through.
Mon to Fri, 9am to 5pm
mail@mcclellands.com.au
201 Armstrong St North, Soldiers Hill, Ballarat VIC 3350