partially buried geophone - definitie. Wat is partially buried geophone
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Wat (wie) is partially buried geophone - definitie

DEVICE THAT CONVERTS GROUND MOVEMENT (VELOCITY) INTO VOLTAGE, WHICH MAY BE RECORDED AT A RECORDING STATION. THE DEVIATION OF THIS MEASURED VOLTAGE FROM THE BASE LINE IS CALLED THE SEISMIC RESPONSE AND IS ANALYZED FOR STRUCTURE OF THE EARTH.
Geophone (instrument)
  • Geosource Inc. MD-79—8 Hz, 335 Ω geophone
  • Geophone (SM-24), frequency band 10 Hz to 240 Hz, standard resistance 375 Ω
  • Man using a geophone
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  • Source Receivers single fold-3 Fold

Geophone         
A geophone is a device that converts ground movement (velocity) into voltage, which may be recorded at a recording station. The deviation of this measured voltage from the base line is called the seismic response and is analyzed for structure of the earth.
Geophone (musical instrument)         
  • Oberlin]], Ohio
MUSICAL INSTRUMENT
Geophone (percussion instrument)
The geophone is a percussion instrument, invented by the French composer Olivier Messiaen for use in his large composition for piano and orchestra entitled Des canyons aux étoiles… ("From the canyons to the stars…"). It consists of a drum filled with thousands of small lead pellets, and is played by swirling it around slowly so that the noise of the pellets resembles the sound of dry shifting earth.
Eveready Harton in Buried Treasure         
1929 FILM
Eveready Harton; Pecker Island; Eveready harton in buried treasure; Eveready Harton In Buried Treasure; "Buried Treasure" Featuring Eveready Harton; Buried Treasure (1929 film)
"Buried Treasure" Featuring Eveready Harton, also known as Pecker Island, is an American adult animated pornographic cartoon short film made in the United States in 1928 or 1929. It depicts the sexual adventures of Eveready Harton (a pun on "ever-ready hard-on"), whose perpetually aroused, comically oversized penis at times detaches and acts on its own.

Wikipedia

Geophone

A geophone is a device that converts ground movement (velocity) into voltage, which may be recorded at a recording station. The deviation of this measured voltage from the base line is called the seismic response and is analyzed for structure of the earth.