Acoustic Monitoring Ocean Seismicity
http://www.pmel.noaa.gov/vents/acoustics/seismicity/seismicity.html
This link is to the Deep Ocean Seismicity from Hydroacoustic Monitoring - specifically the NW Pacific ocean. Info for the current underwater volcanic activity. Really good information here. Click on the Gorda Ridge, NE Pacific adn Endeavour Ridgem NE Pacific links.
The Acoustic Monitoring Project of the VENTS Program began continuous monitoring of north Pacific Ocean seismicity in August 1991 using the U.S. Navy's SOund Surveillance System (SOSUS) In May, 1996, monitoring was extended to the eastern equatorial Pacific using moored autonomous hydrophones, with the North Atlantic added in March, 1999. The hydroacoustic method allows detection of low-magnitude seismicity and volcanic activity and provides more accurate source locations than land seismic networks.
Informant: Anna Webb
This link is to the Deep Ocean Seismicity from Hydroacoustic Monitoring - specifically the NW Pacific ocean. Info for the current underwater volcanic activity. Really good information here. Click on the Gorda Ridge, NE Pacific adn Endeavour Ridgem NE Pacific links.
The Acoustic Monitoring Project of the VENTS Program began continuous monitoring of north Pacific Ocean seismicity in August 1991 using the U.S. Navy's SOund Surveillance System (SOSUS) In May, 1996, monitoring was extended to the eastern equatorial Pacific using moored autonomous hydrophones, with the North Atlantic added in March, 1999. The hydroacoustic method allows detection of low-magnitude seismicity and volcanic activity and provides more accurate source locations than land seismic networks.
Informant: Anna Webb
Starmail - 9. Mär, 08:48
