The Foundation Repair Network · Ground Science Library

The ground
is not still.

Every cracked slab, leaning wall and sinking floor has a geologic address. FRN maps the soils, rock, water and storms that move buildings, region by region and event by event, with the engineering research behind it.

FIG. 1 GENERALIZED SUBSURFACE SECTION WEST CENTRAL FLORIDA KARST SETTING. ILLUSTRATIVE, NOT TO SCALE HORIZONTALLY WT STAIR STEP CRACK FIN. FLR. THICKENED EDGE FOOTING 6 IN CHANNEL LOCK PIPES SQ TUBE BEARING PLATE, WELDED MECHANICAL COUPLER B-1 SP FINE SAND SC CLAYEY SAND CH FAT CLAY LS LIMESTONE RAVELING ZONE SOLUTION CAVITY FM-PP25 PUSH PIER 3 IN SCH 40 SHAFT, ASTM A252 GR 2 6 x 18 IN CHANNEL DIRECTLY UNDER FOOTER (2) 2 IN LOCK PIPES, 6x6x1/4 SQ TUBE HYDRAULIC ADVANCEMENT TO REFUSAL 20 TON WORKING, 25 TON ULTIMATE FM-PP30 PIPE PILE 3.5 IN OD SCH 40, ASTM A252 GR 2 INTERNAL MECHANICAL COUPLERS STEEL BEARING PLATE WELDED AT HEAD PNEUMATIC, THEN DROP HAMMER TO REFUSAL 30 TON ALLOWABLE COMPRESSION BOTH SYSTEMS BYPASS SAND, CLAY AND RAVELED SOIL TO BEAR ON ROCK BELOW THE ACTIVE ZONE BORING LOG B-1 STANDARD PENETRATION TEST ASTM D1586 140 LB HAMMER 30 IN DROP 2 IN SPLIT SPOON DRILLING METHOD MUD ROTARY GROUND SURFACE 0.0 FT FT LOG DESCRIPTION BLOWS/6 IN N VALUE 01020304050 0510152025303540 Tan to gray FINE SAND loose to medium dense (SP) WT 6.0 FT Brown CLAYEY FINE SAND loose (SC) Green-gray FAT CLAY soft, high plasticity (CH) Very loose SILTY SAND raveled, weight of hammer (SM) Weathered LIMESTONE refusal, lost circulation 2-3-3 3-4-4 4-5-6 5-6-7 2-2-3 1-2-2 2-1-2 WOH-WOH-1 18-50/4 IN 50/3 IN REF N=1 N = BLOWS FOR LAST 12 IN. ILLUSTRATIVE PROFILE, NOT A SITE RECORD.
01 · The Atlas

Foundation failure is regional.

A slab in Houston fails for a different reason than a slab in Tampa, Denver or Tucson. The soil, the rock below it and the water moving through it decide how a building moves and what a real repair has to reach. Start with the ground you live on.

Florida Karst

Limestone dissolving under sand and clay. Sinkholes, raveling and cover collapse.

Explore →

Texas & Gulf Coast Clays

Expansive clays that swell when wet and shrink in drought, lifting and dropping slabs.

Explore →

Front Range Bentonite

Some of the most aggressive swelling soils in North America, along the Rockies.

In development

Arizona & Desert Southwest

Collapsible soils, caliche and earth fissures. Dry ground that holds until water reaches it.

Explore →

Pacific Coast

Saturated sands and bay fill that lose strength when the ground shakes.

In development

Pacific Northwest

Steep slopes, heavy rain and glacial deposits. Landslides and creep.

In development

Midwest Frost & Loess

Frost heave, wind blown silt and basement walls pushed in by saturated soil.

In development

The World

Mexico City, Jakarta, Venice, Pisa, Christchurch. Cities built on ground that moves.

In development
02 · Three States, Three Grounds

Florida. Texas. Arizona.

Three of the most active foundation states in the country, and three completely different reasons buildings move. The repair that works on one ground can fail on the next, which is why the diagnosis has to start with the geology.

Florida
Water and Rock

Most of the state sits on limestone that groundwater slowly dissolves. Sand and clay cover the rock, the water table is shallow, and the coasts are built on dredged fill. Voids open below long before anything shows at the surface.

The ground
Sand and clay over karst limestone
What moves it
Sinkholes, raveling soil, high water, storm surge
What a repair must reach
Competent bearing below the weak and raveled zone
Florida karst →
Texas
Clay That Breathes

Texas is one of the busiest foundation repair markets in the United States, and the reason is in the soil. Expansive clays under Houston, Dallas, Fort Worth, Austin and San Antonio swell when they take on water and shrink hard in drought, lifting and dropping slabs season after season.

The ground
High plasticity expansive clay
What moves it
Wet and dry cycles, drought, trees, leaking lines
What a repair must reach
Below the active moisture zone of the clay
Texas clays →
Arizona
Dry Ground That Moves
Arizona library expanding

Desert soils can stand firm for decades and then collapse the first time water reaches them, from irrigation, roof runoff or a broken line. Caliche and clay pockets add to it. Groundwater pumping has also lowered whole basins: the Arizona Geological Survey has mapped about 169 miles of earth fissures, and land near Eloy dropped 15.4 feet between 1952 and 1985.

The ground
Collapsible desert soil, caliche, clay pockets
What moves it
Wetting collapse, basin subsidence, earth fissures
What a repair must reach
Stable soil below the zone water can reach
Arizona ground →
03 · The Mechanisms

How ground moves a building.

Cracks are symptoms. The cause is almost always one of a handful of physical processes in the soil and rock. Name the process and the right repair usually becomes obvious.

Settlement

Soil compresses under load. Uneven settlement, not total settlement, is what cracks walls.

Heave

Expansive clay takes on water and swells, pushing slabs and footings upward.

Liquefaction

Shaking drives up pore water pressure in loose saturated sand until it behaves like a fluid.

Karst Collapse

Acidic groundwater dissolves limestone. The soil above ravels into the void until the surface gives.

Scour & Surge

Storm water strips soil from beneath slabs, piles and seawalls faster than any other force.

Subsidence

Pumping groundwater or draining organic soil lowers the land itself, sometimes across whole cities.

04 · The Events Record

What catastrophe teaches.

Disasters are the largest foundation tests ever run. Each one left a lesson that changed how engineers investigate and repair the ground.

1981
Winter Park, Florida

A sinkhole roughly an acre across opened in May, taking a house, a swimming pool and part of a car dealership. It filled with water and is now a lake.

Florida’s limestone can hold a void for years before the cover above it fails. Surface fixes do nothing about what is happening below.

1989
San Francisco, California

The magnitude 6.9 Loma Prieta earthquake hit the Marina District hardest, a neighborhood built largely on fill placed in the bay.

Two buildings on the same street can perform completely differently. What lies beneath matters more than distance from the fault.

2001
Pisa, Italy

After more than a decade closed, the Leaning Tower reopened. Engineers had reduced its lean by carefully removing soil from beneath the high side.

The most famous foundation failure in the world was fixed by understanding the soil, not by fighting the structure.

2011
Christchurch, New Zealand

The February earthquake triggered widespread liquefaction in the eastern suburbs. Whole neighborhoods were later abandoned.

Some ground cannot be economically repaired. Knowing that before you build is the cheapest engineering there is.

2013
Seffner, Florida

A sinkhole opened beneath a bedroom at night and a man was lost. The house was demolished and the hole filled.

Cover collapse sinkholes give little warning. Investigation, not appearance, is what separates a sound lot from a dangerous one.

2022
Fort Myers Beach, Florida

Hurricane Ian’s storm surge swept across the island, leaving many shallow homes as bare slabs while elevated structures on deep foundations stood.

On the coast, scour is a foundation design load. Depth of support decides what is still standing after the water leaves.

06 · Ask the Network

Tell us what the ground is doing.

Send the basics and we will point you toward what to check, what to ask and who should look at it. Florida questions go to the network’s engineering and waterproofing teams.

  • 01Property city and state
  • 02What you are seeing: cracks, sloping floors, sticking doors, water, a depression in the yard
  • 03How long it has been happening and whether it is getting worse
  • 04Any inspection report, soil boring or contractor proposal you already have
SideBar
07 · From Ground Truth to Repair

When the science is your problem.

FRN is informational. When the ground under your Florida property is moving or water is getting in, these are the network’s engineering and waterproofing resources.

The Foundation Repair Network publishes general educational information about geology, soils and foundation performance. It is not an engineering evaluation of any specific property. Conditions vary site by site; consult a qualified engineer before making repair decisions.