AUDIO-010Recorded evidenceDocumented · probable iceberg grounding

The Train — Iceberg Grounding

A quasi-steady 32–35 Hz signal recorded in March 1997. NOAA considers a very large iceberg grounding and dragging its keel on the seafloor the most likely mechanism.

The Train — Iceberg Grounding
Documented · probable iceberg grounding
The NOAA playback is speeded up ×16.
Record status: A quasi-steady 32–35 Hz signal recorded in March 1997. NOAA considers a very large iceberg grounding and dragging its keel on the seafloor the most likely mechanism.

What NOAA says

The arrival azimuth points toward the Ross Sea near Cape Adare. The sound is interpreted as the acoustic result of a large grounded iceberg moving slowly and scraping the seafloor.

Archive logic

The name “The Train” survives as a historical nickname. The page now separates that memorable label from the present physical interpretation.

Record parameters

Recorded4 March 1997
FrequencyApprox. 32–35 Hz
Likely regionRoss Sea / Cape Adare
ClassificationLarge grounded iceberg