Airborne geophysical surveys of the lower Mississippi Valley demonstrate system-scale mapping of subsurface architecture

Integration of large-scale airborne geophysical surveys can enable the system-scale assessment of aquifer characteristics and improved mapping of shallow subsurface structures, according to a comprehensive investigation of the Mississippi Alluvial Plain The Mississippi Alluvial Plain hosts one of the most prolific shallow aquifer systems in the United States but is experiencing chronic groundwater decline. The Reelfoot rift and New Madrid seismic zone underlie the region and represent an important and poorly understood seismic hazard. Despite its societal and economic importance, the shallow subsurface architecture has not been mapped with the spatial resolution needed for effective management. Here, we present airborne electromagnetic, magnetic, and radiometric observations, measured over more than 43,000 flight-line-kilometers, which collectively provide a system-scale snapshot of the entire region. We develop detailed maps of aquifer connectivity and shallow geologic structure, infer relationships between structure and groundwater age, and identify previously unseen paleochannels and shallow fault structures. This dataset demonstrates how regional-scale airborne geophysics can close a scale gap in Earth observation by providing observational data at suitable scales and resolutions to improve our understanding of subsurface structures.

Automated summary

The integration of large-scale airborne geophysical surveys can provide valuable insights into aquifer characteristics and shallow subsurface structures, improving our understanding of the region's geological features.