The Magnitude 8.8 Chile earthquake of 2010 triggered icequakes (cryoseisms or frost-quakes); vibrations from rapid fracture in large ice fields, frozen soil, or rocks interlaced with frozen water. Seismic data sped up 100x produces the sound.
The Magnitude 8.8 Chile earthquake of 2010 triggered icequakes (cryoseisms or frost-quakes); vibrations from rapid fracture in large ice fields, frozen soil, or rocks interlaced with frozen water. Seismic data sped up 100x produces the sound.
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