What Is The Richter Scale

Learn what the Richter scale is, how it measures earthquake magnitude, and why it's a logarithmic scale. Understand how seismic wave amplitude determines a quake's power.

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What Is the Richter Scale?

The Richter scale is a logarithmic scale used to measure the magnitude, or strength, of an earthquake. It quantifies the amount of energy released at the earthquake's source (hypocenter) by measuring the amplitude of the largest seismic wave recorded on a seismograph.

Section 2: How the Logarithmic Scale Works

Because the Richter scale is logarithmic, each whole number increase represents a tenfold increase in the measured wave amplitude. This means the shaking produced by a magnitude 6.0 earthquake is ten times greater than that of a magnitude 5.0 earthquake.

Section 3: A Practical Example

A magnitude 3.0 earthquake is often felt by people, but it rarely causes any damage. In contrast, a magnitude 7.0 earthquake is considered a major event. Its seismic waves have an amplitude 10,000 times larger than a magnitude 3.0 quake, and it can cause widespread, catastrophic damage over large areas.

Section 4: Importance and Modern Usage

The Richter scale was revolutionary for creating a standard way to compare the sizes of earthquakes globally. While still popularly referenced, seismologists today often use the Moment Magnitude Scale (MMS) because it provides a more accurate measurement for larger earthquakes (typically above magnitude 8) and better reflects the total energy released.

Frequently Asked Questions

Who invented the Richter scale?
Is a magnitude 10 earthquake possible?
What's the difference between magnitude and intensity?
How much more energy is released for each number increase on the Richter scale?