When Soil Becomes Water.
Understanding the phenomenon that transforms solid ground into a fluid trap.
Beneath our feet, loose soil particles are often held together by friction. It feels solid. It supports buildings, bridges, and cities. But this stability is fragile.
During an earthquake, seismic waves shake the ground violently. In water-saturated soils, this shaking pushes water particles apart, increasing the pressure between them.
When the water pressure exceeds the weight of the soil above it, contact between soil grains is lost.
Friction vanishes. The soil structure collapses. Instantly, what was once solid earth behaves like a heavy liquid. Heavy structures sink. Buried tanks float to the surface.
Liquefaction causes billions in damage, often without a single crack in the building's own structure. The foundation simply fails.
Tilting
Buildings tip over as the ground beneath them loses bearing capacity.
Lateral Spreading
Soil layers slide horizontally, tearing apart pipelines and roads.
Sand Boils
Pressurized sand and water erupts to the surface like mini volcanoes.
Prediction is Prevention.
GeoLiquefy provides the intelligence to foresee these risks.