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  1. Magnitude is the size of the earthquake. An earthquake has a single magnitude. The shaking that it causes has many values that vary from place to place based on distance, type of surface material, and other factors. See the Intensity section below for more details on shaking intensity measurements. Types of Magnitudes

  2. Richter scale of earthquake magnitude. At the present time a number of different magnitude scales are used by scientists and engineers as a measure of the relative size of an earthquake. The P -wave magnitude ( Mb ), for one, is defined in terms of the amplitude of the P wave recorded on a standard seismograph.

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  4. Apr 5, 2024 · The quake had a magnitude of 4.8, according to the U.S. Geological Survey, and it was followed by several aftershocks, including one with a magnitude of 4.0. No major damage was reported as of...

    • kerry.breen@paramount.com
    • 10 min
    • News Editor
  5. Events with magnitudes greater than 4.5 are strong enough to be recorded by a seismograph anywhere in the world, so long as its sensors are not located in the earthquake's shadow. The following describes the typical effects of earthquakes of various magnitudes near the epicenter.

  6. Earthquake intensity is very different from earthquake magnitude. Earthquake intensity is a ranking based on the observed effects of an earthquake in each particular place. Therefore, each earthquake produces a range of intensity values, ranging from highest in the epicenter area to zero at a distance from the epicenter.

  7. To locate the epicenter of an earthquake, we need to look at seismograms from three different recording stations. Experts compare the difference in arrival times of the P waves at the different stations. Then they compare the difference in arrival times of the S waves. This enables them to calculate the distance the earthquake is from the ...

  8. en.wikipedia.org › wiki › EarthquakeEarthquake - Wikipedia

    Intensity is the measure of shaking at different locations around the earthquake. Intensity values vary from place to place, depending on the distance from the earthquake and the underlying rock or soil makeup. The first scale for measuring earthquake magnitudes was developed by Charles Francis Richter in 1935.

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