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How does erosion leave voids under a foundation or slab?

Reviewed by Preston, Oklahoma foundation repair consultant ยท Updated 2026-10-14

In short: Erosion and washout happen when moving water carries soil away from beside or beneath a foundation, leaving an empty space (a void) where support used to be. The water can come from concentrated roof and yard runoff, flooding, or a leaking pipe under the slab. Once support is lost, the concrete above can crack or settle into the void.

How does water remove soil from under a foundation?

Water that is concentrated, such as at a downspout outlet, along a low spot against the house, or at a broken pipe, can pick up soil particles and move them. The Oklahoma Geological Survey describes sinkholes forming when water flowing underground erodes sediment and creates voids that the ground above eventually collapses into 1.

After the heavy rains of April 2025, the OGS expected more sinkholes in the hardest-hit parts of Oklahoma, most of them small and located where water flowed beneath roads and driveways 1. The same process can work under slab edges, footings, porches and flatwork.

Three common routes

Which soils erode easily?

Some soils are far more erodible than others. USDA soil surveys rate surface erodibility with the K factor, which ranges from 0.02 to 0.69, with higher values meaning greater susceptibility to sheet and rill erosion; it depends mainly on silt, sand and organic matter content, structure and permeability 4.

A special case is dispersive clay, a clay whose particles break apart and wash away readily in water because sodium dominates its pore water 2. In dispersive soils, a small leak through a crack can enlarge into a pipe or tunnel, and if the tunnel grows large enough its roof can collapse 2. The USDA Natural Resources Conservation Service documented Oklahoma flood-control dams, including Owl Creek Site 13 and Upper Red Rock Site 20, that failed by this kind of tunnel erosion 2. Standard index tests do not identify dispersive clays; specialized tests such as the crumb test, double hydrometer and pinhole test are used 2.

What are the signs of erosion voids?

How do erosion voids differ from karst sinkholes?

Karst sinkholes form when soluble bedrock such as limestone, gypsum or salt dissolves and the ground above collapses into the cavity 7. Erosion voids form in the soil itself, close to the surface, where water carries particles away 1. The USGS notes that human changes to natural drainage can also contribute to sinkhole formation 7. See karst subsidence and sinkholes for the bedrock-driven version.

How are erosion voids typically addressed?

Free, plain-English answers. It asks a few questions and walks you to the repair that fits.

Common questions

Can water wash soil out from under a slab?

Yes. Water moving through or along the soil can carry particles away and leave voids. After the heavy April 2025 rains, the Oklahoma Geological Survey expected most new sinkholes to be small and to appear where water had flowed beneath roads and driveways.

What is a dispersive soil?

A dispersive soil is a clay whose particles break apart and wash away easily in water, usually because sodium dominates its pore water. Small leaks through dispersive soil can enlarge into pipes or tunnels, and at least two Oklahoma flood-control dams have failed this way.

How is an erosion void different from a karst sinkhole?

An erosion void forms in the soil near the surface where runoff or leaking water carries particles away. A karst sinkhole forms when soluble bedrock such as gypsum or limestone dissolves and the material above it collapses into the cavity.

How do I know if a leak is washing out soil under my house?

A whole-house meter test can reveal a supply leak: read the meter, use no water for two hours and read it again. Drain lines need separate testing, which Texas engineering guidelines call for before any foundation lifting.

Sources

  1. Hazard Mapping Oklahoma Geological Survey, University of Oklahoma
  2. Dispersive Clays - Experience and History of the NRCS (Formerly SCS) USDA Natural Resources Conservation Service (D. McCook, Tri-Service Infrastructure Conference)
  3. WaterSense Challenges Homeowners: Take 10 Minutes to Find and Fix a Leak this Week U.S. Environmental Protection Agency
  4. Physical Properties of the Soils (Field Office Technical Guide, Section II) USDA Natural Resources Conservation Service
  5. Guidelines for the Evaluation and Repair of Residential Foundations, Version 3 American Society of Civil Engineers, Texas Section
  6. Geologic Hazards in Oklahoma Geological Society of America (abstract by K. V. Luza, Oklahoma Geological Survey)
  7. Sinkholes U.S. Geological Survey Water Science School
  8. Inspecting Under-Floor Crawl Spaces: A Guide for Home Inspectors (2024 IRC Section R408) InterNACHI

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