Scientists record mysterious voices in the depths of the Indian Ocean

There have been attempts to capture the sound of low frequencies since 1959, although Japanese scientists have finally recorded it on earth until 1998. The noise is caused by our planet's <x0).

No one knows exactly where these fluctuations come from. One theory says that it is the force of ocean waves that rests on the seabed. Another point for acoustic resonancer when the frequency of a vibratory object matches another's natural frequency, causing even the second object to tremble.

Some scientists believe that atmospheric turbulence can cause noise.

A team of scientists led by Martha Deen, a geophysicist at the Earth Physical Institute in Paris, for 11 months collected data from 57 seismometer stations in the Indian Ocean Sea, east of Madagascar, reports “RT” Transmission Periscope. Seismographers were first established to study volcanic activity.

The low noise level is required to monitor the small sound signal amplitude,” said Deen. “On the ocean bottom, the noise level in long periods is generally much higher than on land stations”.

After the sound of the ocean and electronic interventions, they referred to their records by a land - based station in Algeria.

Scientists then discovered that the earth's noise of shaking shines at frequencies between 2.9 and 4.5 millillihertc, which is about 10,000 times lower than what the human ear, which is 20 hertz, can hear. The team's success in recording these low-frequency noises may also have more interesting studies.

The Earth's “Man can be used to study the deep inside of Earth”, says on paper. As scientists usually study the planet's internal levels using seismic waves generated by earthquakes, data from noise sounds can help determine the inner Earth, as the noise is constant as earthquakes erupt from time to time.

What exactly lies behind the illustrations, however, remains a mystery./Periscopi/