Reuters Photojournalism
Our day's top images, in-depth photo essays and offbeat slices of life. See the best of Reuters photography. See more | Photo caption
Olympic torch relay
A look at the relay for the Olympic torch as it makes its way from Greece to England. Slideshow
SpaceX lifts off
A privately owned unmanned rocket blasted off on a mission to be the first commercial flight to the International Space Station. Slideshow
FACTBOX: Earthquakes and magnitude
(Reuters) - A powerful quake measuring 7.9 struck near Indonesia's Sumatra island on Wednesday triggering tsunami warnings in Indonesia, Malaysia, India and Sri Lanka, officials said.
Following are details about measuring the strength of earthquakes and related issues.
* Magnitude measures the size of an earthquake by the energy released at the source of the quake, and is determined from readings on seismographs.
Richter-type formulas, the most commonly used, read the frequency and amplitude of the seismic waves, which are vibrations from earthquakes.
* The Richter scale was named after seismologist Charles Richter, who first developed this method of measuring quakes in 1935.
The scale is logarithmic. Each whole number step in the magnitude scale corresponds to the release of about 31 times more energy than the amount associated with the preceding whole number value. So a magnitude 7.0 quake releases about 900 times more energy than a magnitude 5.0 tremor.
The scale is also open-ended. A quake of magnitude 2 is usually said to be the smallest normally felt by humans.
* The largest recorded earthquake occurred in Chile on May 22, 1960. It measured 9.5 and triggered a tsunami that swept across the Pacific Ocean, killing scores of people in Hawaii, Japan and elsewhere.
The quake that triggered the 2004 Indian Ocean tsunami was magnitude 9.15.
* Among other measurements is moment magnitude, which is a measure of the amount of energy released -- an amount that can be estimated from seismograph readings.
* Japan also uses a seismic intensity scale from 1 to 7 that measures the strength of seismic motion, and usually gets stronger the closer you get to the epicenter of an earthquake.
An earthquake that is 1 on the Japanese scale is felt by only some people in a building. At 7, people find it impossible to move at will and most furniture moves violently.
* The epicenter is the point on the earth's surface vertically above the focus, or hypocenter, the point in the earth's crust where the earthquake is triggered.
(Source: U.S. Geological Survey (www.usgs.gov)
- Tweet this
- Link this
- Share this
- Digg this
- Reprints





Follow Reuters