Abstract

Summary The primary objective of the work-in-progress reported here is to compare near-surface imaging results using ultra-shallow (upper 3 m) seismic-reflection techniques and ground-penetrating radar (GPR) at an alluvial site near Great Bend, Kansas. Although various seismic and GPR surveys have been used for near-surface imaging, little i s known about how the two techniques might work i n concert for very-high-resolution surveys at depths where both techniques work well. We show examples from the test site demonstrating that imaging is possible in the 1- to 6-m range using both seismic and GPR techniques and then discuss the implications of each.

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