The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
An ocean-bottom seismometer goes over the side of R/V Oceanus in early 2001, off Barbados. It will record long-period, low-frequency seismic waves for
An ocean-bottom seismometer goes over the side of R/V Oceanus in early 2001, off Barbados. It will record long-period, low-frequency seismic waves for up to a year before the ship returns to retrieve the instrument. (Photo by John Whitehead, Woods Hole Oceanographic Institution)
Ocean Bottom seismometer
Ocean Bottom seismometer
This shows a P wave (red) converting into an S wave (blue), with the P wave having the ability to travel through the ocean and reflect bown off of the
This shows a P wave (red) converting into an S wave (blue), with the P wave having the ability to travel through the ocean and reflect bown off of the surface into the seismometer. This creates water multiples that do not exist when the seismometer has free-air above it.
Geophone
Geophone (SM-24), frequency band 10 Hz to 240 Hz, standard resistance 375 Ω
Geophone (SM-24), frequency band 10 Hz to 240 Hz, standard resistance 375 Ω
Geosource Inc. MD-79—8 Hz, 335 Ω geophone
Geosource Inc. MD-79—8 Hz, 335 Ω geophone
Man using a geophone
Man using a geophone
Single End Spread & Split Stread
Single End Spread & Split Stread