The subsurface conditions beneath Arlington vary dramatically between the floodplains of the Trinity River and the upland terraces near the Parks Mall. Landfill geotechnics in Arlington must account for the high-plasticity clays (CH) that dominate the eastern half of the city, while the western sectors overlie the Woodbine Formation with interbedded sandstones. A proper geotechnical investigation for a landfill in Arlington requires understanding both the low-permeability clay liners that can be sourced locally and the need for infiltration testing to verify the natural barrier performance. The contrast between these two geologic settings directly influences liner design, leachate management, and long-term settlement predictions.

High-plasticity clays in East Arlington provide natural low-permeability barriers, but only if the desiccation cracking is controlled during dry-season construction.