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About:
This website displays near-real-time, high-precision
hypocenter locations for earthquakes recorded by the Ocean Observatories Initiative (OOI) cabled OBS array at Axial Seamount. The continuous waveform data is processed using machine-learning methods for detection, discrimination, phase arrival-time picking, and association [click here]. New events are then located relative to a high-resolution background (base) catalog using waveform cross-correlation and double-differences [click here]. For more details see here.
Archived DDRT solutions: Analysis: |
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Most recent events (events in queue = 0):
Events last re/processed:
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