Short-period ocean-bottom seismometers (OBSSP) detect vibrations from small earthquakes ranging from 0.1 Hz to 100 Hz. These earthquakes are caused by local phenomena, such as melt movement beneath Axial Seamount and upward flow of hydrothermal fluids in the conduits that feed the black smoker chimneys. These Guralp CMG-6TF instruments enable imaging of the seismic energy traveling through the seafloor.
Five short period seismometers are now installed at the summit of Axial Seamount at the Eastern Caldera subsite (MJ03E), and near the ASHES (MJ03B) hydrothermal field, the Central Caldera, and at the International District Hydrothermal Field (MJ03D). Three short-period ocean-bottom seismometers are also installed at Southern Hydrate Ridge Summit (LJ01B), a methane seep site off of Newport Oregon.
All instruments are streaming data live to IRIS (Incorporated Research Institutions for Seismology) and are available to the public. Daily and hourly updates on the number, locations, depths, and magnitudes of earthquakes occurring at Axial Seamount can be accessed through Dr. William Wilcock’s web site.