TerraBrain

How deep do foundation piers need to go in Oklahoma shale?

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

In short: Oklahoma shale weathers from the top down: hard rock at depth grades upward into softer, broken shale and then into clay soil. The upper clay and weathered layers are the ones that shrink and swell, so repair piers are meant to reach firmer material below them. Typical push pier depths in Oklahoma installation records run about 8 to 16 feet, but each site differs.

What does the shale weathering profile look like?

From the surface down, a typical shale profile looks like this:

  1. Topsoil or fill: organic, loose surface material or soil brought in during construction.
  2. Residual clay: shale that has fully broken down into clay. This is the expansive, moisture-sensitive layer.
  3. Weathered shale: soft, blocky rock that can still be dug and still reacts to water. Soil surveys call its top a paralithic contact.
  4. Competent rock: firmer shale, sandstone or limestone. Soil surveys call the top of hard rock a lithic contact.

USDA soil descriptions show how variable this is in Oklahoma:

Soil series Parent rock Depth to rock Source
Collinsville Pennsylvanian sandstone Hard sandstone at about 4–20 in. 4
Eram Shale with thin sandstone beds Soft shale at 20–40 in. (about 30 in. typical) 1
Kirkland Clayey sediments over Permian shale Weakly cemented siltstone at about 82 in. in the typical profile 3
Dennis Pennsylvanian shale Soil layers more than 60 in. thick; no rock depth given 2

Eram's weathered layer is described as gray or olive shale or compacted clay beds with thin sandstone 1, and Kirkland's bedrock is described as weakly consolidated shale, clay or siltstone 3. In other words, the transition from soil to rock is often gradual.

The Oklahoma Geological Survey notes that the state's thickest accumulation of strata is of Pennsylvanian age, mainly river, delta and shallow-marine deposits 5; Pennsylvanian shales and sandstones underlie the Tulsa area. See Pennsylvanian shales and Bedrock - Tulsa Metro.

Where does the active zone sit?

The active zone, the depth of soil whose moisture changes seasonally, mostly lies in the clay and weathered layers. At four studied Houston clay sites it was about 8–10 feet before the 2011 drought and 10–12 feet during it 7. A structural engineering article on expansive clay describes pier bearing strata as lying below the zone of seasonal moisture variation, typically a minimum of 15 feet or deeper 6. More detail is on shrink-swell and the active zone.

Why does bearing depth matter for each pier type?

Typical Oklahoma depths

Oklahoma steel push pier installation records show depths of roughly 8 to 16 feet, with a median of about 12 feet in Tulsa, at installation pressures around 9,000 psi and a 6,000 psi minimum 8. These are field records rather than a design rule; each pier's depth and final pressure are normally logged so they can be compared with nearby borings and with the soil series.

A pier that stops shallow in known expansive clay may be resting within the active zone rather than below it, which is why refusal depth is compared against site data. See loads, pier spacing and capacity.

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

Common questions

What is a bearing stratum?

It is the soil or rock layer strong enough to carry a foundation's load without settling. For repair piers, it is the layer the pier is driven or drilled down to.

How deep do foundation piers go in Tulsa?

Oklahoma steel push pier installation records show typical depths of about 8 to 16 feet, with a median of about 12 feet in Tulsa. Depth at any one house depends on its soil and rock.

Why does it matter if a pier stops in dry clay?

Clay within the active zone changes volume with moisture. A pier that reaches resistance in stiff, dry clay during a drought may still be in soil that swells or softens when it rewets.

What is the difference between soft and hard rock in soil surveys?

USDA soil descriptions call the top of soft, weathered rock that can still be dug a paralithic contact, and the top of hard rock a lithic contact.

Sources

  1. Official Series Description - ERAM Series USDA Natural Resources Conservation Service
  2. Official Series Description - DENNIS Series USDA Natural Resources Conservation Service
  3. Official Series Description - KIRKLAND Series USDA Natural Resources Conservation Service
  4. Official Series Description - COLLINSVILLE Series USDA Natural Resources Conservation Service
  5. Structural / Tectonic Map of Oklahoma (GM-46) Oklahoma Geological Survey
  6. Expansive Soils (The Mystery) STRUCTURE magazine
  7. Ground Conditions in the 2011 Drought CIGMAT Conference, University of Houston
  8. Oklahoma steel push pier installation records, 2025 (unpublished field data) TerraBrain field data

Was this page helpful?