Approximately 10-15% of all earthquakes have a magnitude greater than 6. This category includes significant earthquakes that can cause considerable damage, although they represent a small fraction of the total number of seismic events. Most earthquakes are of lower magnitude, with many occurring daily around the world.
An earthquake with a magnitude of 3.0 is 10 times stronger than an earthquake with a magnitude of 2.0 on the Richter scale. This means that the release of energy during a magnitude 3.0 earthquake is 10 times greater than that of a magnitude 2.0 earthquake.
Spreading center earthquakes are always shallow, subduction zone earthquakes can be very deep.Spreading center earthquakes are typically of lower magnitude than subduction zone earthquakes.
These are known as magnitude scales. The most commonly known is the Richter magnitude scale which can be calculated from the amplitude of seismic waves measured by a seismometer. However it was not designed for use with larger earthquakes (greater than magnitude 7.0) or for ones a long way from the seismometer station (greater than around 650 km). As such the moment magnitude scale was developed which is calculated from the cross sectional area of the slipped fault, the elastic properties of the rock mass around the fault and the size of the fault movement. This is harder to derive than the Richter magnitude but can be used for larger earthquakes.
An earthquake with a magnitude of 9 is 10,000 times larger in amplitude than an earthquake with a magnitude of 4 on the Richter scale. This means that the energy released by a magnitude 9 earthquake is significantly greater than that of a magnitude 4 quake.
The magnitude of an earthquake is measured on a logarithmic scale, so a magnitude 7.0 earthquake is 10 times stronger than a magnitude 6.0 earthquake in terms of the energy released. This means that the amplitude of ground shaking in a magnitude 7.0 earthquake would be significantly greater than in a magnitude 6.0 earthquake.
For earthquakes world-wide from 2000 to 2012 there were ~ 2092 quakes with a magnitude 6.0 or higher or less than 1% of the total 332,723 recorded earthquakes according to the USGS National Earthquake Information Center.
Earthquakes with a magnitude greater than or equal to 6 are termed strong earthquakes. 7 or larger are termed major earthquakes. Earthquakes greater than or equal to 8 are termed great earthquakes. The term "large" is not actually used.However based on the above it could be argued that any earthquake with a magnitude greater than 6 is a large earthquake.
The Richter scale. For larger earthquakes (magnitude greater than 7) and for those with an epicentral distance greater than 700 km from the seismometer station, the Moment magnitude scale is used.
On average, more than 10 earthquakes less than 4.5 (Richter Scale) happen on a daily basis.Also, 5 earthquakes greater than or equal to 6.5 in magnitude occur every 4 years.Finally, an earthquake with magnitude greater than or equal to 7.5 is expected every 10 years.
Large earthquakes (magnitudes greater than 8) are measured using the MMS (moment magnitude) scale. Small and moderate strength earthquakes (those with magnitudes less than 7) are measured using the Richter magnitude scale and earthquakes with magnitudes between 7 and 8 are measured using the Surface Wave magnitude scale.
Magnitude means size. The magnitude of 8 is greater than the magnitude of 4. The magnitude of 1023209138109283 is greater than the magnitude of 12. =)) .... enjoyy... =D
The moment magnitude scale (MW) provides an estimate of the total energy released in an earthquake and is currently the preferred magnitude scale in use by seismologists for measuring large (magnitude greater than 7) earthquakes.
can a vector have a component greater than the vector magnitude
One statement you could write is that "Earthquakes of higher magnitudes are much rarer than those of lower magnitudes". The magnitude of earthquakes is a logarithmic scale, so a magnitude of 8 is TEN TIMES more powerful than a magnitude 7. This is why earthquakes of higher magnitudes are so much rarer than those of lower magnitudes.
There are far more magnitude 2 or 3 earthquakes than magnitude 4 earthquakes. The small quakes just don't get noticed as much because they typically do little or no serious damage.
no a vector cannot have a component greater than the magnitude of vector
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