Little Rock's expansion westward from the Arkansas River has pushed development into the foothills of the Ouachita Mountains, where the geological transition from alluvial plains to shale and sandstone formations creates unique slope challenges. The city’s population of over 200,000 continues to grow, and with it, the demand for construction on terrain that demands rigorous geotechnical evaluation. A slope failure in this region isn't just a construction delay—it can threaten property, disrupt the watershed feeding into Fourche Creek, and trigger costly regulatory setbacks. Our team integrates decades of regional drilling data with in-situ permeability assessments to model how water moves through these weathered rock interfaces, which is often the primary driver of instability in Pulaski County. We combine this understanding with seismic refraction surveys to map bedrock depth, a critical factor when designing cuts along the city's expanding western corridors.
In Little Rock's weathered shale terrain, a 5-degree misinterpretation of the bedding plane orientation can reduce the factor of safety by 30 percent.
