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- Bloop - Wikipedia
Bloop was an ultra-low-frequency, high amplitude underwater sound detected by the U S National Oceanic and Atmospheric Administration (NOAA) in 1997 [1]
- What is the bloop? - NOAAs National Ocean Service
"The Bloop" is the given name of a mysterious underwater sound recorded in the 90s Years later, NOAA scientists discovered that this sound emanated from an iceberg cracking and breaking away from an Antarctic glacier
- The Bloop, A Short Film About the Loudest Underwater Sound Ever . . .
In 1997, the National Oceanic and Atmospheric Administration discovered an unusual, ultra-low-frequency sound emanating from a point off the southern coast of Chile It was the loudest unidentified
- The Bloop: A Mysterious Sound from the Deep Ocean | NOAA SOSUS
Although Bloops are some of the loudest sounds of any type ever recorded in Earth's oceans, their origin remains unknown The Bloop sound was placed as occurring several times off the southern
- Is the Bloop Real? Well, Yes and No | HowStuffWorks
Is the Bloop real? This mysterious underwater sound recorded in the Pacific Ocean in 1997 was so loud that underwater microphones detected it from over 3,000 miles away
- The Unsolved Mystery of the Bloop - YouTube
Usually, researchers would use the sounds recorded to learn about seismic activity and marine animals, but the mysterious bloop was something different The NOAA described the noise as rising
- What Is the Bloop? Unveiling the Mystery of Piercing Sound Deep in the . . .
Not only is it loud, but the sound also had a unique characteristic that came to be known as ' The Bloop ' Underwater microphones called hydrophones positioned more than 3,000 miles (4,828
- The Bloop: Mysterious Underwater Sound Finally Explained - American Oceans
In 1997, a sound was detected by hydrophones located over 5,000 kilometers apart in the Pacific Ocean The sound was named “The Bloop” due to its distinctive sound profile Scientists initially thought that the sound was produced by a large sea creature, such as the giant squid
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