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English: How earthquake early warning systems work. Upon a fault rupture, fast primary and slow secondary waves travel through the ground. The P-wave information is collected from seismometers and analyzed at a central station, and alerts on estimated magnitude, intensity, epicenter, and time til shaking are transmitted via sirens, phones, computers, television, radio, and other warning systems.
Masomi https://www.usgs.gov/media/images/earthquake-early-warning-basics
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Public domain
This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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na yanzu18:13, 9 Disamba 2019Wadar sufa ta zubin 18:13, 9 Disamba 20191,140 × 684 (20.19 MB)Awesome Aasim{{Information |description ={{en|1=How earthquake early warning systems work. Upon a fault rupture, fast primary and slow secondary waves travel through the ground. The P-wave information is collected and analyzed at a central station, and alerts on estimated magnitude, intensity, epicenter, and time til shaking are transmitted via sirens, phones, computers, television, radio, and other warning systems.}} |date = |source =https://www.usgs.gov/media/images/earthquake-early-...

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