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Charles Francis Richter [1900-1985] American
Rank: 102
Scientist, Seismologist


Charles Francis Richter was an American seismologist and physicist.
Richter is most famous as the creator of the Richter magnitude scale, which, until the development of the moment magnitude scale in 1979, quantified the size of earthquakes. 

Experience, Science, Strength



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As seismologists gained more experience from earthquake records, it became obvious that the problem could not be reduced to a single peak acceleration. In fact, a full frequency of vibrations occurs. Experience
101
Emphasis was usually put on the horizontal acceleration factor, for the simple reason that ordinary structures have a built-in safety factor for the vertical component; that is, gravity.
102
Nothing is less predictable than the development of an active scientific field. Science
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Intensity like signal strength will generally fall off with distance from the source, although it also depends on the local conditions and the pathway from the source to the point. Strength
104
This is very similar to astronomy where different magnitudes are assigned to the brightness of an astronomical object, depending on the range of wavelengths being measured.
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Logarithmic plots are a device of the devil.
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If one introduces the concept of energy of an earthquake then that is a theoretically derived quantity.
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By moving them vertically, a representative mean curve could be formed, and individual events were then characterized by individual logarithmic differences from the standard curve.
108
I suggested that we might compare earthquakes in terms of the measured amplitudes recorded at these stations, with an appropriate correction for distance.
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In every area of the world where there is earthquake risk, there are still many buildings of this type; it is very frustrating to try to get rid of them.
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My amateur interest in astronomy brought out the term 'magnitude', which is used for the brightness of a star.
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Don't wait for extraordinary circumstance to do good; try to use ordinary situations.
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Incidentally, the usual designation of the magnitude scale to my name does less than justice to the great part that Dr. Gutenberg played in extending the scale to apply to earthquakes in all parts of the world.
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Refining is inevitable in science when you have made measurements of a phenomenon for a long period of time.
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I usually point out that most loss of life and property has been due to the collapse of antiquated and unsafe structures, mostly of brick and other masonry.
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I was lucky because logarithmic plots are a device of the devil.
116
There is another common misapprehension that the magnitude scale is itself some kind of instrument or apparatus. Visitors will frequently ask to 'see the scale.'
117
We would have been happy if we could have assigned just three categories, large, medium, and small; the point is, we wanted to avoid personal judgments. It actually turned out to be quite a finely tuned scale.
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What emerged, of course, was that the magnitude scale presupposed that all earthquakes were alike except for a constant scaling factor. And this proved to be closer to the truth than we expected.
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I'm glad to see the press now referring to the open-ended Richter scale.
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For example, some stars put out large amounts of energy in the infrared part of the spectrum, so that this can produce a different relative magnitude rating than using light energy from the middle of the spectrum.
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From here, it becomes an engineering problem; the engineer considers the ground motion that will occur and evaluates the requirements of the proposed structure in the light of the local foundation conditions.
122
I repeatedly have to correct this belief. In a sense, magnitude involves steps of 10 because every increase of one magnitude represents a tenfold amplification of the ground motion. But there is no 'scale of 10' in the sense of an upper limit.
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If the assumptions used in calculating energy are changed, then this seriously affects the final result, even though the same body of data might be used.
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