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When receiving the noise signal, the amplifier and subwoofers responded with sound pressures ranging from 100 dB to 120 dB. The resulting rumble could be felt by audience members as well as heard. [1] For the film Earthquake, Sensurround was activated during the quake scenes to augment the conventional soundtrack. [5]
From about 1900 to the 1950s, the "lowest frequency in practical use" in recordings, broadcasting and music playback was 100 Hz. [9] When sound was developed for motion pictures, the basic RCA sound system was a single 8-inch (20 cm) speaker mounted in straight horn, an approach which was deemed unsatisfactory by Hollywood decisionmakers, who hired Western Electric engineers to develop a ...
John Williams' music for Earthquake was the second of his trio of scores for large-scale disaster films, having previously scored The Poseidon Adventure and following with The Towering Inferno. [12] Williams scored Earthquake and The Towering Inferno during the summer of 1974, with both scores showing similarities to one another (notably ...
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Aftershock: Earthquake in New York is a 1999 miniseries that was broadcast in the United States on CBS in two parts, with the first part aired on November 14 and the second on November 16. It was released to VHS in 2000, and on DVD in 2001.
The magnitude 4.4 earthquake that rattled Los Angeles on Monday was centered within one of the region's most potentially destructive fault systems, one capable of producing a magnitude 7.5 ...
Earthquake started his career in the Airforce in the talent show “Tops and Blues”. [5] In 2002, Earthquake joined Latham Entertainment Presents Comedy Tour. [ 5 ] In 2004, he signed a deal with ABC to create his own sitcom called “Earthquake,” which later fell through, [ citation needed ] although in 2005 he performed one of his most ...
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according ...
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