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Colorado's most significant geologic hazard
The Colorado Geological Survey (CGS) calls expansive, or swelling, soil Colorado's most significant geologic hazard, and says these clays cause more property damage than any other natural hazard in the state. Among the damage it lists: cracked driveways, sidewalks and basement floors. That's not a Castle Rock quirk; it's how much of the Front Range is built. But Douglas County has more than its share.
The culprit is clay minerals, mainly montmorillonite (often called bentonite), that pull water in between microscopic, plate-shaped particles. As the clay gets wet, the plates are pushed apart and the soil swells. When it dries, it shrinks. The CGS says expansive soil can grow by 10 percent or more in volume as it gets wet and push with pressures of 20,000 pounds per square foot or more, and that engineers generally consider a volume increase of just 3 percent potentially damaging.
What's under Castle Rock and the north county
Much of the Castle Rock area sits on the Dawson Formation, a mix of sandstone, conglomerate and claystone, with the harder Castle Rock Conglomerate on top in places. Farther north, the Denver Formation joins it. In a study of north-central Douglas County (Highlands Ranch, Lone Tree, Parker and the surrounding area), the CGS analyzed 4,900 samples from 4,200 test borings drawn from geotechnical reports for 185 subdivisions. A few of its findings matter for anyone with a driveway or patio:
- Claystone is the main problem. Claystone and interbedded sandstone and claystone, and the soils weathered from them, posed the greatest risk of swelling.
- Almost everything can swell. Nearly all the surficial deposits and bedrock in the study area appeared to contain highly expansive clays.
- Some soil settles instead. Windblown silt and sand deposits can collapse or settle significantly when wetted or loaded, and creek-valley alluvium varied widely: Piney Creek alluvium samples ranged from as much as 10.5 percent swell to as much as 5.7 percent consolidation.
- Conditions change within a few feet. Engineering properties varied significantly both sideways and with depth, which is why one corner of a driveway can rise while another sinks.
Along the foothills, there's a separate hazard. The CGS mapped a Dipping Bedrock Overlay District in western Douglas County, including the Roxborough Park area and the mouth of Jarre Canyon near Sedalia, and the Perry Park area west of Larkspur, where steeply tilted layers of expansive bedrock can heave unevenly. The same report notes that some of the tilted rock there, such as the Fountain and Lyons Formations, isn't expansive, so it really is lot by lot.
Why flatwork takes the hit
The CGS points out that lightly loaded structures, like single-family homes, are especially vulnerable to soil movement. Driveways, sidewalks and patios are lighter still. A 4-inch slab sitting on the ground has almost no weight to hold swelling clay down, so it rides whatever the soil does. And unlike a house, flatwork usually doesn't get a soils report, piers or a structural floor.
Water is the trigger. Expansive soil under Colorado homes usually starts out fairly dry. The CGS says construction, irrigation and poor drainage add water, and in many cases the soil never returns to its original dryness. It lists inadequate surface drainage and irrigated plantings next to a foundation among the most common aggravating factors. The same applies at the edge of a slab: a downspout emptying onto the driveway, a sprinkler head spraying the side of a walk, or a patio that pitches toward the house all feed water to the clay underneath.
Freeze-thaw adds a second force. Water that gets into cracks and the base freezes and expands, widening cracks a little more each winter. On clay, the two work together: a crack lets water in, the clay swells, the slab moves, and the crack gets bigger.
Reading the damage: heave, settlement or shrinkage?
Not every crack means the same thing, and the fix depends on the cause.
- Thin cracks at regular spacing, often at or near control joints, are usually normal shrinkage as the concrete cured. They're cosmetic, but filling them keeps water out of the base.
- A panel or edge that has risen, or a slab that has domed or tilted up, points to heave from swelling soil, often near a water source.
- A panel that has dropped, such as a garage apron below the garage floor, a step pulling away from the porch, or a patio sinking at one corner, points to settlement: soil that compressed, collapsed when wetted, or washed out.
- Long, straight ridges or offsets on foothills lots may be tilted bedrock heaving and deserve a soils engineer's look before you replace anything.
What helps on a new slab
No contractor can make a slab immune to clay, and be wary of anyone who promises that. What good work does is reduce the water reaching the soil and give the concrete a better chance of moving without breaking up:
- Base preparation. Removing soft or organic material and placing and compacting a granular base. On known problem sites, a geotechnical engineer may recommend removing and replacing more of the expansive soil.
- Drainage. Slope the slab so water runs off it and away from the house, extend downspouts past the concrete, and keep sprinklers off the edges. The CGS notes clay shouldn't be allowed to dry out excessively before concrete is poured, either.
- Joints. Control joints spaced to guide where cracks form, and isolation joints where the slab meets the foundation, steps or other concrete, so one piece can move without dragging the next.
- Reinforcement and thickness suited to the load, especially for heavy vehicles.
- A freeze-resistant mix. Ask whether exterior concrete is air-entrained, and how a fresh pour will be protected if a hard freeze is forecast. The American Concrete Institute treats air temperatures at or expected to fall below 40°F as cold weather for concrete.
What to do about existing concrete
- Fix the water first. Redirect downspouts, adjust sprinklers and regrade soil that slopes toward the slab. Otherwise any repair is fighting the same problem.
- Fill cracks so water and grit can't get into the base. It won't stop a slab that's actively moving, but it slows freeze-thaw damage.
- Lift a sunken slab that's still in one piece. Mudjacking or foam lifting raises it from below, usually for far less than new concrete. Lifting fixes the symptom, so ask what caused the settling.
- Replace sections that are broken into many pieces, crumbling, or heaving in several places. See driveway replacement.
- Call a geotechnical engineer if movement is large, keeps coming back, shows up as long ridges, or is also cracking the house. Concrete contractors fix concrete; engineers diagnose soil.
Before you hire
Ask any contractor about base prep, thickness, joints, edge drainage and who pulls the right-of-way permit. Rules differ by town; see our pages for Castle Rock, Castle Pines, Parker, Highlands Ranch, Lone Tree, Larkspur and Sedalia. When you're ready, request a free quote and a local contractor will come look at it in person.
Sources
- Colorado Geological Survey, Expansive Soil and Rock
- Colorado Geological Survey, OF-02-08 Soil and Bedrock Conditions and Construction Considerations, North-Central Douglas County
- Colorado Geological Survey, SP-42 Heaving-Bedrock Hazards Associated with Expansive, Steeply Dipping Bedrock in Douglas County
- Colorado Geological Survey, OF-04-05 Geologic Map of the Castle Rock South Quadrangle
- American Concrete Institute, ACI 306R Guide to Cold Weather Concreting