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Ground Penetrating Radar, (GPR) is a noninvasive electromagnetic geophysical technique that produces profiles showing a virtual cross-section of soil, sediment and bedrock layers. Can also be used to profile stream and lake bottoms and sandy sub-bottom sediment layers. Works well in electrically-resistive materials such as quartz sand, limestone, sandstone, coal and most igneous and metamorphic rocks. Depth of penetration up to 100 feet in clean dry sand, 300 feet in unweathered granite. Radar is absorbed by clay, most shales, saltwater and other electrically-conductive materials. Compare X-RAY here. Applications:
Experience includes:
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