Frost Heave: What It Does to Footings and How Deep Foundations Avoid It

Cut-away of a frost heave in forest soil showing needle ice beneath a layer of ice-rich soil, about 15 cm thick
A frost heave thawing in Norwich, Vermont, in March 2010. The cut face shows needle ice growing up from the freezing front under a lifted layer of ice-rich soil. Photo: HopsonRoad, via Wikimedia Commons · Source · CC BY-SA 3.0 · Resized

Frost heave is the upward movement of the ground when water in the soil freezes into layers of ice, called ice lenses, that keep growing by drawing more water up from the unfrozen soil below. Anything resting in that freezing zone, like a shallow footing, a deck post or a slab edge, gets lifted, often unevenly, and doesn’t always settle back where it was. Foundations avoid it by bearing below the frost line, by insulating the ground so it doesn’t freeze, or by sitting on something frost can’t move, such as rock or a deep pile.

Here’s how the process works, which soils are worst, and what that means for a new build in Colorado.

What causes frost heave

Three things have to be present at once. The FHWA’s geotechnical pavement manual lists them as frost-susceptible soil, subfreezing temperatures in the soil, and a source of water (FHWA NHI-05-037, Ch. 7). Take away any one and heave doesn’t happen.

The common explanation, that water expands when it freezes, is only a small part of it. The bigger effect is water migrating. As the freezing front moves down, unfrozen water is pulled up toward it and freezes onto growing ice lenses. In one 2023 lab study on silty clay, the water content near the freezing front climbed to 53.4 percent in untreated soil, from a starting water content of 25 percent (Ji et al., 2023). That extra water, now ice, is what pushes the ground up.

The photo above shows it clearly: needle ice growing up from the freezing front, with a lifted layer of ice-rich soil on top.

Which soils heave the most

Fine soils with the right pore size are the worst. They’re tight enough to pull water up by capillary action but open enough to let it move. The FHWA manual groups soils into four frost-susceptibility classes based on fines content:

ClassFrost susceptibilityTypical soils
F1Negligible to lowGravelly soils with 3 to 10 percent fines
F2Low to mediumGravelly soils with 10 to 20 percent fines; sands with 3 to 15 percent fines
F3HighGravelly soils over 20 percent fines; sands over 15 percent fines; clays with PI over 12
F4Very highAll silts; very fine silty sands over 15 percent fines; clays with PI under 12

Source: FHWA NHI-05-037, Ch. 7. “Fines” means material passing the 0.075 mm sieve, and PI is the plasticity index.

The same manual treats a water table within about 3 meters (10 feet) of the surface as a high frost hazard, since it keeps feeding the ice lenses. Clean, free-draining gravel barely heaves; a silty yard next to a downspout heaves a lot.

What frost heave does to a foundation

There are two ways it gets hold of a structure.

Heave under the footing. If the bottom of a footing sits in soil that freezes, the ice lenses form underneath it and lift it. A light structure’s weight won’t hold it down, so the practical defense is to keep the bearing surface out of the freezing zone.

Adfreeze on the sides. Frozen soil can bond to the side of a post, pier or pile and drag it upward as the frozen layer heaves. The Chance design manual names adfreeze from seasonally frozen ground as one of the uplift forces deep foundations must resist, and notes that on expansive clay the swelling pressure can far exceed it (CHANCE Technical Design Manual). It’s why a deck post set in a shallow concrete plug can “jack” a little higher every winter: the plug gets gripped, lifted, and never quite drops back.

The damage shows up as doors and windows that bind in winter and free up in spring, deck boards that hump at a post, garage slabs that crack near the edge, and fence posts that lean.

How the code protects foundations from frost

Denver’s residential code, like the IRC it’s based on, requires foundation walls, piers and other permanent supports to be protected from frost by one of four methods (Denver Residential Code 2025, R403.1.4.1):

  1. Extending below the frost line in Table R301.2.
  2. Building a frost-protected shallow foundation under Section R403.3, which uses insulation to keep the ground under the footing from freezing.
  3. Designing to ASCE 32, the engineering standard for frost-protected shallow foundations.
  4. Bearing on solid rock.

The same section says footings must not bear on frozen soil unless the frozen condition is permanent, and it exempts small free-standing accessory buildings (600 square feet or less for light-frame construction, 400 for other construction, with walls 10 feet tall or less). Separately, exterior footings have to be at least 12 inches below undisturbed ground.

Frost depths in Colorado

Frost depth is set locally, so the number on your plans depends on where you’re building:

JurisdictionFrost depthSource
City and County of Denver36 inDenver Residential Code 2025, Table R301.2
Larimer County (countywide)30 inLarimer County Structural Design Information
Summit County40 inSummit County Building Inspection Matrix

Check with your local building department before you design. Mountain towns, counties and Front Range suburbs each publish their own design criteria.

How deep foundations avoid frost heave

A deep foundation sidesteps the problem by bearing well below the freezing zone and giving frozen soil as little to grab as possible.

For helical piles, the Chance manual recommends the top helix plate sit at least three helix diameters below the maximum frost depth, or below the active zone of expansive soil if that’s deeper. Its example uses a 4-foot frost depth and a 12-inch helix, which puts the top helix at 7 feet. With Denver’s 36-inch frost line and a 10-inch helix, the same rule gives 5.5 feet as a floor before any other design check. On Front Range clay, the swelling-soil active zone usually pushes piles deeper than frost does anyway; our post on why helical piers suit Colorado soil explains that side.

The manual also says ice lenses in frost-susceptible soil should be penetrated and not relied on for end bearing, and that capillary breaks, vapor barriers and drainage do a lot to control heave at the surface.

A pile’s slim steel shaft gives adfreeze a small surface to grip compared with a wide concrete pier. The connection at the top still needs to be designed for any uplift the engineer expects, and on decks the pile replaces the shallow concrete plug that tends to jack.

Practical steps for a new build

  • Find your jurisdiction’s frost depth before footings are designed.
  • Read the soils report for silts, fine sands and groundwater depth. Those are the frost-heave flags.
  • Keep roof and surface water away from footings and posts. No water, no ice lenses.
  • For decks, sheds and other light structures, don’t rely on shallow concrete plugs in silty, wet ground. Bear below the frost line. Our post on helical piles for decks covers the options.
  • If you’re building in winter, don’t pour footings on frozen ground. Steel piles can go in through a frozen crust, but the caps and beams still need cold-weather concrete practice.

Talk to us about frost-proof foundations

Site Safe Helical Piers installs helical piles that bear below the frost line for new homes, additions, decks and commercial projects across Denver and the Colorado Front Range. Call 970-673-5615 or contact us with your plans, and see our services for the project types we handle.

FAQ

What is frost heave?

The upward movement of the ground when ice lenses form in freezing soil. Water is drawn up from the unfrozen soil below and freezes onto the lenses, which keep growing and lift the ground and anything sitting in it.

Will frost heave go down?

The ground usually settles as it thaws, but not always back to where it started, and soil is often weak and wet during the thaw. Posts and shallow footings gripped by frozen soil can creep upward a little each winter.

What does frost heave look like?

Bulges in lawns and pavement, deck boards humped at a post, fence posts leaning or lifted, slab edges cracking, and doors that stick in winter and free up in spring.

How do you stop frost heave under a foundation?

Bear the foundation below the local frost line, insulate the ground with a frost-protected shallow foundation design, bear on solid rock, or use a deep foundation such as helical piles. Controlling surface water and using free-draining fill also reduces heave.

How deep is the frost line in Denver?

Denver’s residential code sets it at 36 inches in Table R301.2. Larimer County uses 30 inches and Summit County 40 inches, so check your own jurisdiction.

Sources

  1. FHWA NHI-05-037, Geotechnical Aspects of Pavements Reference Manual, Chapter 7 (frost action and frost susceptibility)
  2. Ji et al. (2023), Effect of Anionic Polyacrylamide Polymer on Frost Heave Mitigation and Its Implication for Frost-Susceptible Soil, Polymers (PMC10181066)
  3. Hubbell Power Systems, CHANCE Technical Design Manual (2023), seasonally frozen ground and minimum bearing depth
  4. Denver Residential Code 2025 (2024 IRC with Denver amendments), Chapter 4 Foundations, R403.1.4.1 Frost protection
  5. Denver Residential Code 2025, Chapter 3 Table R301.2
  6. Larimer County Community Development, Structural Design Information
  7. Summit County Building Inspection Department Matrix (revised January 2023)

Topics: frost heave, frost depth, foundations, Colorado, helical piles, building codes

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