The Richter magniude scale is logorithmic. As such the size (amplitude) of the largest seismic waves produced by a magnitude 7 earthquake are 102 (or 100) times larger than those produced by a magnitude 5 earthquake. However the amount of energy released by a magnitude7 earthquake is 1000 times greater (102)^3/2 than a magnitude 5 earthquake and so it is likely to be much more destructive.
An earthquake with a magnitude of 7 is 10 times more powerful than an earthquake with a magnitude of 6. This is because the magnitude scale is logarithmic, meaning that for each whole number increase in magnitude, the amplitude of the earthquake's waves increases tenfold.
A magnitude 8.0 earthquake is 10 times stronger than a magnitude 7.0 earthquake and 100 times stronger than a magnitude 6.0 earthquake. It releases significantly more energy compared to smaller magnitude earthquakes.
An earthquake with a magnitude of 7 releases about 32 times more energy than an earthquake with a magnitude of 6 on the Richter scale. The Richter scale is logarithmic, so each whole number increase represents a tenfold increase in amplitude and approximately 32 times more energy released.
The 1960 Chile earthquake, also known as the Valdivia earthquake, released energy equivalent to about 1,000 megatons of TNT, making it the most powerful earthquake ever recorded.
There are many factors. One would be the distance a person is from the epicenter. A person who is further from a magnitude 7 earthquake would be less affected by the shockwaves than a person nearer to the epicenter of a magnitude 6 earthquake. The place the person is in at the time of the earthquake also may affect the intensity of what he feels. If one is in a tall and stable building during an earthquake, he would not feel the vibrations as much as one standing on the streets. The scale measuring the intensity of earthquakes should be considered too. A Mercalli Intensity Scale measuring magnitude 6 may possibly be more powerful than a Richter Scale measuring a magnitude 7, as more damage is caused.
To my best calculation it will be around 32-35 times bigger and powerful.
An earthquake with a magnitude of 7 is 10 times more powerful than an earthquake with a magnitude of 6. This is because the magnitude scale is logarithmic, meaning that for each whole number increase in magnitude, the amplitude of the earthquake's waves increases tenfold.
A magnitude 8.0 earthquake is 10 times stronger than a magnitude 7.0 earthquake and 100 times stronger than a magnitude 6.0 earthquake. It releases significantly more energy compared to smaller magnitude earthquakes.
An earthquake with a magnitude of 7 releases about 32 times more energy than an earthquake with a magnitude of 6 on the Richter scale. The Richter scale is logarithmic, so each whole number increase represents a tenfold increase in amplitude and approximately 32 times more energy released.
3.0 more
100 times
The 2010 Christchurch earthquake was of magnitude 7.1. The 2011 Christchurch earthquake was of magnitude 6.3. The 2011 Japan earthquake was of magnitude 9.0. The formula for comparing the energy released by two earthquakes using the moment magnitude scale (which is what I assume those numbers are in, since it's the most common scale for large earthquakes) is D=103*(m1 - m2)/2 So compared to the more recent Christchurch earthquake, we get that the Japan earthquake was about 103*(9.0-6.3)/2 = 103*2.7/2 = 104.05 which we can tell even without actually doing the calculations is a bit over 10,000 times more powerful in terms of total energy released. (this does not, however, mean 10,000 times more damage).
D
More than 50 aftershocks all measuring about 4.9
100 times larger
A 9.0 earthquake is 100 times larger in magnitude than a 7.0 earthquake on the Richter scale. This means that the amplitude of ground motion and energy release is significantly higher in a 9.0 earthquake compared to a 7.0 earthquake.
Typically, at least three seismometers are needed to accurately determine the location and magnitude of an earthquake. By measuring the arrival times of earthquake waves at different locations, seismologists can triangulate the epicenter and assess the seismic activity more effectively.