The amplitude of seismic waves from an earthquake is is measured by a seismometer. From this an estimate can be made of the amount of energy released by an earthquake (this is known as magnitude).
The magnitude of an earthquake is controlled by the amount of energy stored within the deformed rocks of the crust. This is in turn a function of the elastic moduli of the crust, the cross sectional area of the fault rupture zone and the amplitude of the displacement on the fault.
We determine the scaling relationships between earthquake stress drop and recurrence.
The two main factors that help determine earthquake risk are the movement of seismic waves along faults, and friction.
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the magnitude and the intensity
Magnitude.
Magnitude is another term for the strength of an earthquake.
You use a seismograph to measure the strength of an earthquake.
Magnitude.
Magnitude
Magnitude.
Magnitude is another term for the strength of an earthquake.
You use a seismograph to measure the strength of an earthquake.
Magnitude.
An earthquake's magnitude is a measure of its strength.
Depends on it's magnitude which can range. Seisometers are used to measure the Magnitude of an earthquake. Magnitude is it's strength.
The Richter magnitude scale is used to measure the strength of an earthquake.
9.5
Magnitude.
The Seismograph is used to measure the Magnitude of an earthquake.
a seismograph can find the severity of an earthquake by graphing the measures of distances and strength of an earthquake.
The basis for forecasting strength is gap hypothesis.