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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. Geophysical survey (archaeology) - Wikipedia

    en.wikipedia.org/wiki/Geophysical_survey...

    The chief limitation of magnetometer survey is that subtle features of interest may be obscured by highly magnetic geologic or modern materials. GPR survey. Ground-penetrating radar (GPR) is perhaps the best known of these methods (although it is not the most widely applied in archaeology). The concept of radar is familiar to most people.

  5. 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

  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. Radar signal characteristics - Wikipedia

    en.wikipedia.org/wiki/Radar_signal_characteristics

    Consider the following example : if the radar antenna is located at around 15 m above sea level, then the distance to the horizon is pretty close, (perhaps 15 km). Ground targets further than this range cannot be detected, so the PRF can be quite high; a radar with a PRF of 7.5 kHz will return ambiguous echoes from targets at about 20 km, or ...

  8. Radar engineering - Wikipedia

    en.wikipedia.org/wiki/Radar_engineering

    Radar sensors are classified by application, architecture, radar mode, platform, and propagation window. Applications of radar include adaptive cruise control , autonomous landing guidance, radar altimeter , air traffic management , early-warning radar , fire-control radar , forward warning collision sensing , ground penetrating radar ...

  9. Remote sensing in geology - Wikipedia

    en.wikipedia.org/wiki/Remote_sensing_in_geology

    Richat Structure by Shuttle Radar Topography Mission (SRTM). Instead of being a meteorite impact, the landform is more likely to be a collapsed dome fold structure.. Remote sensing is used in the geological sciences as a data acquisition method complementary to field observation, because it allows mapping of geological characteristics of regions without physical contact with the areas being ...