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  2. Depth sounding - Wikipedia

    en.wikipedia.org/wiki/Depth_sounding

    Depth sounding, often simply called sounding, is measuring the depth of a body of water. Data taken from soundings are used in bathymetry to make maps of the floor of ...

  3. Fishfinder - Wikipedia

    en.wikipedia.org/wiki/Fishfinder

    A fishfinder or sounder (Australia) is a sonar instrument used on boats to identify aquatic animals, underwater topography and other objects by detecting reflected pulses of sound energy, usually during fishing activities.

  4. Echo sounding - Wikipedia

    en.wikipedia.org/wiki/Echo_sounding

    Echo sounding or depth sounding is the use of sonar for ranging, normally to determine the depth of water . It involves transmitting acoustic waves into water and recording the time interval between emission and return of a pulse; the resulting time of flight , along with knowledge of the speed of sound in water, allows determining the distance ...

  5. Kelvite sounding machine - Wikipedia

    en.wikipedia.org/wiki/Kelvite_sounding_machine

    Thomson noted that no depth-sounding apparatus was available on the ship to assist the operation. [4] During 1872, on board his own sailing yacht Lalla Rookh and the cable-laying ship CS Hooper , Thomson conducted trials of a sounding machine, with the main improvement over existing practice being the use of piano wire instead of hemp rope for ...

  6. Sound velocity probe - Wikipedia

    en.wikipedia.org/wiki/Sound_Velocity_Probe

    Firstly, the surveyor can use an air filled metal bar lowered below the transducer, attached at each end by a rope marked with depth values. If the values on the rope can be assumed to be correct, then the bar is lowered at set depth intervals and observed on the echo sounder trace. The values of echo sounder depth can be plotted against the ...

  7. Multibeam echosounder - Wikipedia

    en.wikipedia.org/wiki/Multibeam_echosounder

    A multibeam echosounder is a device typically used by hydrographic surveyors to determine the depth of water and the nature of the seabed. Most modern systems work by transmitting a broad acoustic fan shaped pulse from a specially designed transducer across the full swathe acrosstrack with a narrow alongtrack then forming multiple receive beams (beamforming) that are much narrower in the ...

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