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.
The strength of an earthquake is measured by its magnitude, which indicates the amount of energy released at the earthquake's source. Earthquake magnitude is typically reported on the Richter scale or the moment magnitude scale.
Magnitude is another term for the strength of an earthquake.
That term is liquefaction. It occurs when saturated soil loses its strength due to shaking during an earthquake, causing it to behave like a liquid.
The term that describes the point on the Earth's surface above the area where an earthquake originates is it's epicenter.
The strength of an earthquake is typically measured using the moment magnitude scale (Mw), which takes into account the seismic energy released by the earthquake. This scale provides a single number that represents the overall size of the earthquake. Another commonly used scale is the Richter scale, which measures the amplitude of seismic waves.
The strength of an earthquake is measured by its magnitude, which indicates the amount of energy released at the earthquake's source. Earthquake magnitude is typically reported on the Richter scale or the moment magnitude scale.
Magnitude is another term for the strength of an earthquake.
Magnitude.
An earthquake's magnitude is a measure of its strength.
Another word for an earthquake's strength is magnitude. Magnitude is a measure of the size of the seismic waves produced by an earthquake.
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.
That term is liquefaction. It occurs when saturated soil loses its strength due to shaking during an earthquake, causing it to behave like a liquid.
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The Seismograph is used to measure the Magnitude of an earthquake.
magnitude of an earthquake
a seismograph can find the severity of an earthquake by graphing the measures of distances and strength of an earthquake.