Slab Foundation Repair Cedar Park, TX.
Cedar Park sits where limestone ridges meet graded fill, so two corners of the same slab can rest on completely different ground. We measure that difference first, then anchor your home to rock with galvanized steel piers.
Much of Cedar Park was carved out of caliche-capped limestone ridges and built back up with borrowed fill to make the flat pads homes sit on today. That history is exactly why a slab here can behave so strangely: one end may rest a foot above near-surface bedrock while the other spans compacted fill that keeps consolidating long after the house is finished. The result is uneven bearing, and when that fill settles or dries, the movement passed into a slab can exceed half an inch across a single room, enough to crack masonry, bind a door frame, and pull cabinet runs away from the ceiling.
The drought years of 2022 and 2023 made the pattern obvious across Williamson County. Slabs that had ridden quietly for a decade started cracking for the first time as the fill beneath them finally dried past its shrinkage limit. The fix isn't more concrete sitting in the same restless soil, it's reaching past it. We drive galvanized steel piers hydraulically through the active zone and lock them onto competent limestone, which ends the slab's dependence on what the surface dirt does next season.
How a Cedar Park repair actually goes
Free elevation survey to 1/64 in.
We map your slab to ±0.01 in. (1/64 in.), pinpoint the high and low corners, and show you in writing which beams have moved and in which direction.
Engineered pier plan for your lot
Because bedrock depth can shift several feet across one footprint here, we set pier count, spacing, and lift points to a structural spec rather than a square-footage guess.
Drive, lift, and lock onto rock
Each galvanized pier is advanced hydraulically until the strata itself resists it, then the slab is raised back toward plan and the load is transferred onto steel.
Re-survey and warranty
We document the final elevation, confirm the correction held, and back the stabilization with a lifetime transferable warranty before the crew leaves.
Why the ground under Cedar Park moves the way it does
The driving force here is differential support, not the deep, churning clay you find on the Blackland Prairie east of the Balcones Escarpment. Soil depth changes sharply over the irregular limestone, so a slab can be solidly carried on one side and effectively unsupported on the other where fill has consolidated over time. That's a different problem with a different repair sequence than a uniform clay platform that swells and shrinks evenly.
The active soil zone, the depth over which seasonal moisture swings turn into actual volume change, tends to be shallower in Cedar Park. Shallower does not mean inert. The thin clays and clayey loams trapped between limestone layers still hold real plasticity, and cut-and-fill lots often blend materials that retain moisture unpredictably. Add fractured and solution-weathered seams in the bedrock itself, and bearing capacity becomes something you have to confirm pier by pier rather than assume.
Many Cedar Park homes built from the late 1980s onward sit on post-tensioned slabs with unbonded tendons. Those need careful handling: lift points have to dodge the tendon paths, and the lift has to be sequenced so one span isn't overloaded while another is still sitting low. It's one more reason a measured plan beats a generic pier count on these lots.
Signs your Cedar Park slab is telling you something
Most calls we take here start with one or two of these, and they almost always trace back to what's happening under the slab:
- Stair-step cracks climbing through the exterior brick or block
- Doors and windows that stick, drag, or quit latching as the frame racks out of square
- Cracks fanning from door and window corners in the drywall
- Sloping or bouncy floors, often worse toward one corner of the house
- A new crack in the slab or garage floor, or a gap opening between trim and the ceiling
- Movement that showed up suddenly after a long dry stretch, a classic Williamson County drought tell
Where the movement is matters as much as how much
A perimeter beam that has dropped while the interior stays level usually points to edge drying, a drainage or irrigation issue. An interior low spot with a stable perimeter more often means fill consolidation or a void beneath the slab.
Those two findings call for different scope and sequence, which is why we measure the whole slab before quoting anything. Most homes stay occupied throughout, and typical projects land between $4,500 and $14,000 with financing available.
Cedar Park slab repair, answered
My lot is cut-and-fill on a slope, does that change the repair?
How deep will the steel piers actually go on my property?
Half my slab feels fine and the other half slopes, why?
My house has a post-tension slab, can you still pier it?
Cracks appeared after the 2022 to 2023 drought, is that the cause?
What keeps the repair stable after you finish?
Do we have to move out, and how long does it take?
Will a documented repair help when I sell?
Book your free
foundation inspection.
Tell us where you are and what you’re seeing. A GroundLock structural advisor confirms within one business hour.
All foundation services in Cedar Park
Every GroundLock service, available throughout Cedar Park and the surrounding area:
Get your free foundation inspection.
A licensed inspector measures your slab elevation to ±0.01 in. (1/64 in.) and gives you a written, engineer-backed plan with zero pressure.