The Underground Recording That Three Scientists Heard and Refused to Describe
In the spring of 1989, a geological survey team drilling exploratory boreholes in the Ural Mountains of Russia lowered a series of microphones to a depth of approximately 9,000 meters as part of a study into deep-crustal acoustic properties.
They were not expecting to record anything of interest. At that depth, the anticipated sounds were geological — rock stress, thermal fracturing, the slow mechanical noise of the Earth's crust under pressure. Baseline data. Useful for calibration.
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