Richter scale

From Simple English Wikipedia, the free encyclopedia

The Richter magnitude scale is a scale of numbers used to tell the size of earthquakes. Charles Richter developed the Richter Scale in 1935.

Earthquakes that are 4.5 or higher on the Richter scale can be measured by tools all over the world.

The scale is logarithmic, with a base of 10. This means that an earthquake which scores 3.0 on the scale is ten times as powerful that one that scores 2.0.

Descriptor Richter Magnitude number Damage caused by the earthquake Frequency of occurence
Micro Less than 2.0 Micro (very small) earthquakes, people cannot feel these. About 8,000 each day
Very minor 2.0-2.9 People do not feel these, but seismographs are able to detect them. About 1,000 per day
Minor 3.0-3.9 People often feel these, but they rarely cause damage. About 49,000 each year
Light 4.0-4.9

Objects inside houses are disturbed, causing noise. Nothing is damaged.

About 6,200 each year
Moderate 5.0-5.9

Buildings that are not built well may be damaged. Light objects inside a house may be moved.

About 800 per year
Strong 6.0-6.9 Moderately powerful. May cause a lot of damage in a larger area. About 120 per year
Major 7.0-7.9 Can damage things seriously over larger areas. About 18 per year
Great 8.0-9.9 Massive damage is caused. Heavy objects are thrown into the air and rents appear on the ground, as well as visible shockwaves. Overhead highways may be destroyed, and buildings are toppled. About 1 per year
Meteoric 10.0+ There are no records of anything of this size. The vibration is about the same as that of a 20km meteor. Unknown

(Adapted from U.S. Geological Survey documents.)

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