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Booms came later relative to burps, 15 to 17 seconds after the avalanche starting point. Booms were primarily composed of fast-moving P-waves that traveled internally through the sand dune. During an earthquake, P-waves are the first to reach and be recorded by a seismograph. In contrast to the wave responsible for burps, these P-waves were linear and non-dispersive, showing a more regular and harmonious pattern. Slower S-waves were also detected, but faintly.
