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About:
This website displays near-real-time, machine-learning based, double-difference
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, phase arrival-time picking, and association. New events are then located relative to a high-resolution background (base) catalog using waveform cross-correlation and double-differences. For more details see here.
Archived DDRT solutions: Analysis: |
Most recent events (events in queue = 0):
Events last re/processed:
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