Groundwater pressure heads can exceed elevation heads and, in those cases, result in water flowing out on the ground surface as artesian flows or springs or swampy wetlands. Changes in groundwater surfaces can be slow as they can change seasons, or they can be relatively rapid such as in tidal basins or storm water detention basins. Groundwater tables can fluctuate with time. These characteristics come into effect below the groundwater surface or table.
When soil is saturated, the soil media takes on very specific physical characteristic due to the relative incompressibility of water. The flow of groundwater below the surface is a fundamental property that controls the strength and compressibility of soil impacting soil's ability hold up on structural loads. Groundwater is found beneath the Earth's surface in soil pore spaces and rock formation fractures.
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