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  2. Ground-penetrating radar - Wikipedia

    en.wikipedia.org/wiki/Ground-penetrating_radar

    Ground-penetrating radar (GPR) is a geophysical method that uses radar pulses to image the subsurface. It is a non-intrusive method of surveying the sub-surface to investigate underground utilities such as concrete, asphalt, metals, pipes, cables or masonry. [ 1 ]

  3. Near-surface geophysics - Wikipedia

    en.wikipedia.org/wiki/Near-surface_geophysics

    Ground-penetrating radar is one of the most popularly used near-surface geophysics in forensic archaeology, forensic geophysics, geotechnical investigation, treasure hunting, and hydrogeology, with typical penetration depths down to 10 m (33 ft) below ground level, depending upon local soil and rock conditions, although this depends upon the ...

  4. RIMFAX - Wikipedia

    en.wikipedia.org/wiki/RIMFAX

    RIMFAX is a ground-penetrating radar, its antenna is located on the lower rear of the Perseverance rover. It is able to image different ground densities, structural layers, buried rocks, meteorites, and detect underground water ice and salty brine at 10 m (33 ft) depth.

  5. US Radar - Wikipedia

    en.wikipedia.org/wiki/US_Radar

    The depth range of GPR is limited by the electrical conductivity of the ground, the transmitted frequency range and the radiated power. [2] Unlike metal detectors, which can only detect specific materials, ground penetrating radar images the entirety of the subsurface within range.

  6. Geophysical imaging - Wikipedia

    en.wikipedia.org/wiki/Geophysical_imaging

    The types of geophysical imaging used include: diffusive electromagnetic, geoelectric, seismic tomography, and ground-penetrating radar. In fact, the first use of ground-penetrating radar was to determine a glacier's depth in 1929. [3] Two dimensional geophysical imaging techniques have recently allowed for 2D imaging of mountain permafrost. [6]

  7. Forensic geophysics - Wikipedia

    en.wikipedia.org/wiki/Forensic_geophysics

    Ground-penetrating radar (or GPR) has a typical maximum depth below ground level (bgl) of 10 m, depending upon the antennae frequencies used, typically 50 MHz to 1.2 Gz. The higher the frequency the smaller the object that can be resolved but also penetration depths decrease, so operators need to think carefully when choosing antennae ...

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  9. Reflection seismology - Wikipedia

    en.wikipedia.org/wiki/Reflection_seismology

    A method similar to reflection seismology which uses electromagnetic instead of elastic waves, and has a smaller depth of penetration, is known as Ground-penetrating radar or GPR. Hydrocarbon exploration

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