What Does an Earthquake Sound Like?

In 1953, audio engineer Emory Cook released a unique album titled Out of this World. Upon playing it, listeners heard a reverberating boom and a narrator informing them: “This is a record of actual earthquakes.” Narration continued over a strange soundscape, explaining how tapes of earthquakes were sped up to make them audible. Those tapes came from the experiments of Victor Hugo Benioff, a seismologist who helped bring both seismological and musical instruments into the electronic age.

According to historian Matthias Dörries, these projects were deeply intertwined. Benioff had started in astronomy in 1917, working at both the Mount Wilson and Lick observatories. During downtime, Benioff practiced violin and tried to reconcile his love of music with his understanding of science.

In 1932, Benioff invented a new way of listening to the Earth: the strain seismometer.

Over the next couple of decades, Pasadena became “a major worldwide center for geophysical research,” Dörries explains. By 1926, Caltech was running the Seismo Lab with the Carnegie Institution, where seismologists like Beno Gutenberg and Charles Richter would deepen our understanding of earthquakes.

Benioff began work in seismology at Caltech in 1924. While Gutenberg and Richter focused primarily on theory, Benioff concentrated on instrumentation. At the time, seismometers primarily used weighted pendulums connected to pens or light beams that recorded vibrations on photosensitive paper. But these instruments had limited sensitivity.

Benioff began to experiment with electromechanical sensors, using a suspended weight connected to a transducer and a galvanometer. Then, in 1932, Benioff invented a new way of listening to the Earth: the strain seismometer.

More to Explore

Why Does Music in Science Fiction Sound Like That?

Angelica Frey April 28, 2026 Imagining the sound of other worlds has a long past—and persistent creative limits.

Dörries describes the first instrument, installed “in the basement of the laboratory in the San Rafael Hills, with piers firmly fixed to the granite underneath the laboratory and cemented in with concrete.” The piers were 24 meters apart, with an iron pipe between them. Benioff left a tiny gap between one of the piers and the pipe. As vibrations and other changes in the Earth altered the size of the gap, Benioff recorded the changes with a transducer.

Greater sensitivity meant the instruments picked up other sources of vibration and strain: ocean surf, storms, traffic, and even sunrises. Benioff learned to “listen” to earthquakes, separating signal from noise.

“Benioff became an expert on how to materially transform the physical quantities of vibrational energy into electrical energy,” Dörries writes, “and then to record them over time in seismograms, which he read like musical scores.” He would soon use similar principles to experiment with electric instruments.

Weekly Newsletter

"*" indicates required fields

He experimented with transducers to create electric violins and cellos and filed patents in 1938. A concert at Caltech that June featured an “electro-cello” and a violin that the Los Angeles Times referred to as a “seismographic fiddle.” Benioff would later work on electric grand pianos, establishing a partnership with pianist Rosalyn Tureck.

Benioff used these “technologies of enchantment,” Dörries writes, “to bring unity and wholeness to technological and human culture.” He spent decades “listening” to earthquakes, including the largest ever recorded, in Chile in 1960. Dörries quotes seismologist Stewart Smith: “Benioff could finally hear the ‘music of the earth.’”

The post appeared first on JSTOR Daily.

添加评论
点赞收藏
点踩分享查看原文
评论
?
参与讨论