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the strength and frequency is the same
a seismograph can find the severity of an earthquake by graphing the measures of distances and strength of an earthquake.
a seismographic flow
the strength of an earthquake.
The strength (or more correctly the frequency and amplitude) of an earthquake is measured using a device known as a seismometer. Estimates of the energy released by an earthquake (described as it's magnitude) are made using the Moment Magnitude scale. Estimates of this may also be derived from the amplitude of the seismic waves recorded on the seismometer using the now obsolete Richter or Local Magnitude scale as well as the Moment Magnitude scale. Please see the related questions for more information.
the strength and frequency is the same
The Strength and Frequency Method only predicts how often an earthquake of a particular magnitude will occur. The Gap Hypothesis only predicts where another earthquake is most likely to occur along a fault line. Neither method will predict where the next earthquake will occur in the world, or predict an earthquake happening in a random spot, or predict both the location and strength of an earthquake.
The scientific device used to detect earthquakes is a Seismograph. They're necessary for detecting small earthquakes and for determining their strength. An earthquake that's at least 2.0 on the Richter scale can be felt by some people, and a 3.0 can be felt by most people.
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.