Foundation Repair

What Happens When a House Is Built on Fill Dirt

Some Metro Atlanta homes are not sitting on natural ground. Here is why filled lots settle, how to spot it, and what a real repair has to reach.

An Anglin's operator working the ground beside a Metro Atlanta home with a compact excavator.

Topics: Foundation Repair

Not every house is built on the ground that was always there.

Across Metro Atlanta, a lot of lots were made rather than found. A sloped parcel gets cut on the high side and filled on the low side to produce a flat building pad. A ravine or an old creek bed gets filled in. Occasionally a site was used as a dump long before anybody thought about houses, and the fill went in over the top of it.

If your house sits on the filled half of that arrangement, and it has started to move, this is very likely why.

Fill is not automatically bad

Worth saying plainly, because this scares people more than it needs to.

Engineered fill, placed in controlled layers and compacted as it goes, can be excellent ground. Plenty of houses sit on it for decades with nothing to report. The distinction that matters is not fill versus no fill. It is whether the fill was engineered, how deep it runs, and what got buried in it.

Fill that was pushed into a low spot to make a lot look level, without being compacted in layers, is a different thing entirely. So is fill with organic material in it: stumps, brush, construction debris, household waste. Soil does not lose volume as it ages. Buried organic material does, continuously, for years, as it breaks down.

Why filled ground settles unevenly

Natural ground under a Metro Atlanta house has usually been sitting there getting compressed for a very long time. The U.S. Geological Survey describes the soils of the Southern Piedmont as ultisols, "deeply weathered soils derived from underlying acid crystalline and metamorphic rock."[1] That is a thick, settled column of clay and decomposed rock over granite, and it has had geological time to reach equilibrium.

Fill has had none of that. It is loose material placed recently, and it consolidates under load on its own schedule.

The uneven part is the important bit. Fill is almost never the same depth across a lot. On a cut-and-fill pad, one side of the house may sit on undisturbed ground while the other sits on a considerable depth of fill. That is a recipe for differential settlement: one part of the house goes down, another does not, and the structure has to absorb the difference. Cracks are the house absorbing the difference.

Georgia's clay makes it worse rather than better, because clay is not a stable material even where it has not been disturbed. Swelling clay "expands or contracts in response to changes in environmental factors," and hydration and dehydration "can vary the thickness of a single clay particle by almost 100 percent."[2] Fill made of Georgia clay does the seasonal swelling and shrinking that all our clay does, on top of consolidating from its own weight.

Signs the ground, not the house, is the problem

Settlement on fill has a shape to it that is worth recognizing.

It is usually one-sided. Cracks concentrate at one corner or along one wall rather than appearing evenly around the house. That corner is generally the one over the deepest fill.

The lot tells on itself. A building pad noticeably flatter than the land around it, a house on the low side of a graded slope, a flat area between two hills, a driveway that has separated from the garage on the downhill side.

It keeps going. Clay movement is seasonal, so it tends to open and close a little through the year. Consolidating fill mostly goes one direction, and the crack that was there last spring is wider now rather than different.

Additions move separately. Additions, porches and garages are often built on shallower footings than the main house, and on fill they can go their own way while the original structure stays put.

If you are seeing any of this, the general list in foundation warning signs is worth reading alongside this.

The repair has to get past the fill

This is the whole point, and it is where a lot of money gets wasted.

Anything that stabilizes the house inside the fill layer is resting on the same material that has been moving. It may hold for a while. It has not solved anything.

A real repair transfers the weight of the house through the fill and onto the dense natural ground underneath it. We drive steel piers down until they reach ground that will carry the load, then transfer the structure onto that steel. After that the fill can continue consolidating and it stops being the house's problem, because the house is no longer standing on it.

On a filled lot the depth question matters more than almost anywhere else, and it is genuinely unknown until we drive. That is also why nobody honest can quote this over the phone. If you want the longer version of how piers work and when each kind is right, we wrote push piers vs helical piers, and what foundation repair costs in Georgia covers why depth drives the price.

If you are buying

Ask directly whether the lot was cut and filled, and ask for the grading plan if there is one. County and city records often hold more than the seller does.

A house on fill with documented, completed pier work and a transferable warranty is frequently a better buy than an identical house on undisturbed ground with unexplained cracks. Known and fixed beats unknown.

If you are mid-purchase and something is worrying you, get it looked at before closing rather than after. Buying a house with foundation problems goes through how to think about that.

What to do now

If your house is on a filled lot and it is moving, the movement is not going to talk itself out of it. Fill consolidates, organic material keeps breaking down, and Georgia clay keeps doing what Georgia clay does.

We will come out and look at no charge, tell you what we find in plain language, and tell you if we think it can wait. Call 770-422-2924 or ask for an inspection.

Sources

  1. U.S. Geological Survey, "The Apalachicola-Chattahoochee-Flint River NAWQA Program study: Soils" — ga.water.usgs.gov
  2. U.S. Geological Survey, "Environmental Characteristics of Clays and Clay Mineral Deposits" — pubs.usgs.gov/info/clays

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