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.