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 .
It is calculated from the seismic moment (M0 - which has the unit of dynes/cm =where 1 dyne/cm = 1x10-7 N/m) which is a measure of the total energy released during an earthquake and is derived based on the elastic moduli of the crust where the earthquake occurred, the length of the slip surface and the cross sectional area of the slip surface as follows:
M0 = G x AFx DF
Where:
G = Shear modulus of the rock mass
AF = Area of the rupture along the fault
DF = average displacement on AF
In order to make the moment magnitude scale (Mw) consistent with older magnitude scales such as the Local Moment (or "Richter") scale the seismic moment (M0) is converted into a logarithmic scale using the following equation:
Mw = 2/3 x log10 x (M0) - 10.7
This ultimately yields a dimensionless number and as such, Moment Magnitude has no units.
Please see the related question.
The magnitude of earthquakes is calculated using a logarithmic scale called the Richter scale or the moment magnitude scale. This scale measures the energy released by an earthquake at its source. The magnitude is determined based on the amplitude of seismic waves recorded on seismographs.
1) Analyzing the seismic waves recorded by a seismograph.
The amplitude recorded by the seismograph can be used to find the magnitude of the earthquake.
The depth of the earthquake faulting is can give you the distance from the focus to the epicenter and how far the earthquake occurred from the fault boundary.
Finding when the earthquake occurred gives you...when the earthquake occurred =P
Comparing the speed of P-waves and S-waves can be used to determine how far the epicenter is from where you currently are.
The two locations with the highest magnitude earthquakes are the Valdivia region in Chile with a magnitude of 9.5 in 1960 and the Prince William Sound region in Alaska with a magnitude of 9.2 in 1964.
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.
Plate boundaries that have the largest magnitude earthquakes are convergent boundaries where two tectonic plates collide, such as subduction zones. These boundaries can produce megathrust earthquakes, which are some of the most powerful earthquakes on Earth. Transform boundaries, where plates slide past each other, can also produce large earthquakes.
The Richter scale was originally developed to measure the strength or magnitude of moderate earthquakes (magnitudes less than 7). The surface wave magnitude scale was then developed by Richter and Guttenburg to allow larger earthquake magnitudes to be measured (up to 8). To measure large earthquakes the moment magnitude scale must be used. To measure the severity of earthquakes, the Modified Mercalli intensity scale is used in the US and the Macroseismic scale is used in Europe.
The highest magnitude ever recorded for an earthquake was the Great Chilean Earthquake of 1960, which had a magnitude of 9.5.
High magnitude earthquakes are seismic events with a magnitude of 7.0 or greater on the Richter scale. These earthquakes can cause widespread damage to buildings, infrastructure, and the environment, as well as posing significant risks to human life. Proper preparedness and response measures are crucial in mitigating the impact of high magnitude earthquakes.
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.
The word magnitude (in the context of earthquakes) is used to describe the amount of energy released when one occurs.
An earthquake's magnitude can go as high as 10 or above on the Richter scale. Magnitude 10 earthquakes are extremely rare and are considered to be the strongest earthquakes ever recorded. The majority of earthquakes are of lower magnitude, with the average being around magnitude 4.
No only middle and big magnitude earthquakes do.
Magnitude
The moment magnitude scale can be used to rate earthquakes of all sizes, near or far.
There were no earthquakes over magnitude 8 recorded in 1981.
magnitude of past earthquakes in the area
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.
The largest recorded earthquake to date, the 1960 Valdivia earthquake, was calculated to be 9.5 MW (moment magnitude scale). The scale has no boundaries, though the chance of earthquakes of increasingly greater magnitude occurring diminishes rapidly.
magnitude