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The measure of energy released by an earthquake depends on its magnitude. If its a high magnitude earthquake, there is a lot of energy. If there is a low magnitude, then there is little energy.
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A magnitude scale is simply a metric for quantifying the energy released in an earthquake and the amplitude of the waves the earthquake emits. The most well-known magnitude scale in America is the Richter scale, which is equated in base 10 (that is, an earthquake that scores 5.0 on the Richter scale will have an Amplitude ten times greater than that of an earthquake that scores a 4.0 on the Richter scale).
The energy released by an earthquake increases by 10x for every 1.0 increase in magnitude on the Richter scale. A 6.2 quake is 2.0 higher than a 4.2 quake. The increase in energy output would be calculated as such: 10x10=100. A 6.2 magnitude earthquake is 100 times more powerful than a 4.2 magnitude earthquake.
The instrument that is used to measure the magnitude of an earthquake is a seismometer.
The Richter Scale measures the magnitude of an earthquake which is another way of describing the energy released in the earthquake.
The Richter scale measures the magnitude of an earthquake which is another way of describing the energy released in the earthquake.
An earthquake's magnitude is a measure of how strong it is
The Richter scale is a magnitude scale - it measures the amount of energy released by an earthquake. As such tit is a way of quantifying earthquake magnitude and comparing it to other earthquakes.
magnitude a measure of the energy of an earthquake specified on the richter scale.
The Richter scale expresses the relative magnitude of an earthquake, which is a measure of the energy released at the focus of an earthquake.
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A 3.0 earthquake releases 1,000 times more energy than a 1.0 earthquake.
The Richter magnitude scale (ML) scale, assigns a single number to quantify the amount of seismic energy released by an earthquake. It is a logarithmic scale based upon the horizontal amplitude of the largest displacement from zero on a seismometer. Each whole unit (i.e., 1.0) corresponds to an approximate energy increase of 32 time (e.g., a 6.0 M earthquake has 32 time the energy release of a 5.0 M).
The measure of energy released by an earthquake depends on its magnitude. If its a high magnitude earthquake, there is a lot of energy. If there is a low magnitude, then there is little energy.
Invented in 1935 by Charles F. Richter, the Richter Scale measures the magnitude of earthquakes.
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