Richter magnitude scale

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The Richter scale – also called the Richter magnitude scale and Richter's magnitude scale – is a measure of the strength of
earthquake An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth Earth is the third planet from the Sun and the only astronomical object known t ...

s, developed by
Charles Francis Richter Charles Francis Richter (); April 26, 1900 – September 30, 1985) was an United States, American seismology, seismologist and physics, physicist. Richter is most famous as the creator of the Richter magnitude scale, which, until the development ...
and presented in his landmark 1935 paper, where he called it the "magnitude scale". This was later revised and renamed the local magnitude scale, denoted as ML or . Because of various shortcomings of the scale, most seismological authorities now use other scales, such as the
moment magnitude scale The moment magnitude scale (MMS; denoted explicitly with or Mw, and generally implied with use of a single M for magnitude) is a measure of an earthquake An earthquake (also known as a quake, tremor or temblor) is the shaking of the surfac ...
(), to report earthquake magnitudes, but much of the news media still refers to these as "Richter" magnitudes. All magnitude scales retain the
logarithm In mathematics Mathematics (from Ancient Greek, Greek: ) includes the study of such topics as quantity (number theory), mathematical structure, structure (algebra), space (geometry), and calculus, change (mathematical analysis, analysis). ...

ic character of the original and are scaled to have roughly comparable numeric values (typically in the middle of the scale).

Development

Prior to the development of the magnitude scale, the only measure of an earthquake's strength or "size" was a subjective assessment of the intensity of shaking observed near the
epicenter The epicenter, epicentre () or epicentrum in seismology is the point on the Earth's surface directly above a hypocenter, hypocenter or focus, the point where an earthquake or an underground explosion originates. Surface damage In most earthqua ...

of the earthquake, categorized by various
seismic intensity scales Seismic intensity scales categorize the intensity or severity of ground shaking (quaking) at a given location, such as resulting from an earthquake An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the ...
such as the Rossi-Forel scale. ("Size" is used in the sense of the quantity of energy released, not the size of the area affected by shaking, though higher-energy earthquakes do tend to affect a wider area, depending on the local geology.) In 1883 John Milne surmised that the shaking of large earthquakes might generate waves detectable around the globe, and in 1899 E. Von Rehbur Paschvitz observed in Germany seismic waves attributable to an earthquake in Tokyo. In the 1920s Harry O. Wood and John August Anderson, John A. Anderson developed the ''Wood–Anderson seismometer, Seismograph'', one of the first practical instruments for recording seismic waves. Wood then built, under the auspices of the California Institute of Technology and the Carnegie Institution for Science, Carnegie Institute, a network of seismographs stretching across Southern California. He also recruited the young and unknown Charles Richter to measure the seismograms and locate the earthquakes generating the seismic waves. In 1931 Kiyoo Wadati showed how he had measured, for several strong earthquakes in Japan, the amplitude of the shaking observed at various distances from the epicenter. He then plotted the logarithm of the amplitude against the distance and found a series of curves that showed a rough correlation with the estimated magnitudes of the earthquakes. Richter resolved some difficulties with this method and then, using data collected by his colleague Beno Gutenberg, he produced similar curves, confirming that they could be used to compare the relative magnitudes of different earthquakes. To produce a practical method of assigning an absolute measure of magnitude required additional developments. First, to span the wide range of possible values, Richter adopted Gutenberg's suggestion of a
logarithm In mathematics Mathematics (from Ancient Greek, Greek: ) includes the study of such topics as quantity (number theory), mathematical structure, structure (algebra), space (geometry), and calculus, change (mathematical analysis, analysis). ...

ic scale, where each step represents a tenfold increase of magnitude, similar to the magnitude scale used by astronomers Apparent magnitude, for star brightness. Second, he wanted a magnitude of zero to be around the limit of human perceptibility. Third, he specified the Wood–Anderson seismograph as the standard instrument for producing seismograms. Magnitude was then defined as "the logarithm of the maximum trace amplitude, expressed in microns", measured at a distance of . The scale was calibrated by defining a magnitude 0 shock as one that produces (at a distance of ) a maximum amplitude of 1 micron (1 µm, or 0.001 millimeters) on a seismogram recorded by a . Finally, Richter calculated a table of distance corrections, in that for distances less than 200 kilometers the attenuation is strongly affected by the structure and properties of the regional geology. When Richter presented the resulting scale in 1935, he called it (at the suggestion of Harry Wood) simply a "magnitude" scale. "Richter magnitude" appears to have originated when Perry Byerly told the press that the scale was Richter's and "should be referred to as such." In 1956, Gutenberg and Richter, while still referring to "magnitude scale", labelled it "local magnitude", with the symbol , to distinguish it from two other scales they had developed, the surface wave magnitude (MS) and body wave magnitude (MB) scales.

Details

The Richter scale was defined in 1935 for particular circumstances and instruments; the particular circumstances refer to it being defined for Southern California and "implicitly incorporates the attenuation, attenuative properties of Southern California crust and mantle." The particular instrument used would become saturated by strong earthquakes and unable to record high values. The scale was replaced in the 1970s by the
moment magnitude scale The moment magnitude scale (MMS; denoted explicitly with or Mw, and generally implied with use of a single M for magnitude) is a measure of an earthquake An earthquake (also known as a quake, tremor or temblor) is the shaking of the surfac ...
(MMS, symbol ); for earthquakes adequately measured by the Richter scale, numerical values are approximately the same. Although values measured for earthquakes now are , they are frequently reported by the press as Richter values, even for earthquakes of magnitude over 8, when the Richter scale becomes meaningless. The Richter and MMS scales measure the energy released by an earthquake; another scale, the Mercalli intensity scale, classifies earthquakes by their ''effects'', from detectable by instruments but not noticeable, to catastrophic. The energy and effects are not necessarily strongly correlated; a shallow earthquake in a populated area with soil of certain types can be far more intense in effects than a much more energetic deep earthquake in an isolated area. Several scales have historically been described as the "Richter scale", especially the ''local magnitude'' and the surface wave scale. In addition, the ''body wave magnitude'', , and the ''moment magnitude'', , abbreviated MMS, have been widely used for decades. A couple of new techniques to measure magnitude are in the development stage by seismologists. All magnitude scales have been designed to give numerically similar results. This goal has been achieved well for , , and . The scale gives somewhat different values than the other scales. The reason for so many different ways to measure the same thing is that at different distances, for different hypocenter, hypocentral depths, and for different earthquake sizes, the amplitudes of different types of elastic waves must be measured. is the scale used for the majority of earthquakes reported (tens of thousands) by local and regional seismological observatories. For large earthquakes worldwide, the moment magnitude scale (MMS) is most common, although is also reported frequently. The seismic moment, ', is proportional to the area of the rupture times the average slip that took place in the earthquake, thus it measures the physical size of the event. is derived from it empirically as a quantity without units, just a number designed to conform to the scale. A spectral analysis is required to obtain , whereas the other magnitudes are derived from a simple measurement of the amplitude of a specifically defined wave. All scales, except , saturate for large earthquakes, meaning they are based on the amplitudes of waves which have a wavelength shorter than the rupture length of the earthquakes. These short waves (high frequency waves) are too short a yardstick to measure the extent of the event. The resulting effective upper limit of measurement for is about 7 and about 8.5 for . New techniques to avoid the saturation problem and to measure magnitudes rapidly for very large earthquakes are being developed. One of these is based on the long-period P-wave; the other is based on a recently discovered channel wave. The energy release of an earthquake, which closely correlates to its destructive power, scales with the power of the shaking amplitude. Thus, a difference in magnitude of 1.0 is equivalent to a factor of 31.6 ($=\left(\right)^$) in the energy released; a difference in magnitude of 2.0 is equivalent to a factor of 1000 ($=\left(\right)^$) in the energy released. The elastic energy radiated is best derived from an integration of the radiated spectrum, but an estimate can be based on because most energy is carried by the high frequency waves.

Richter magnitudes

The Richter magnitude of an earthquake is determined from the
logarithm In mathematics Mathematics (from Ancient Greek, Greek: ) includes the study of such topics as quantity (number theory), mathematical structure, structure (algebra), space (geometry), and calculus, change (mathematical analysis, analysis). ...

of the amplitude of waves recorded by seismographs (adjustments are included to compensate for the variation in the distance between the various seismographs and the
epicenter The epicenter, epicentre () or epicentrum in seismology is the point on the Earth's surface directly above a hypocenter, hypocenter or focus, the point where an earthquake or an underground explosion originates. Surface damage In most earthqua ...

of the earthquake). The original formula is: :$M_\mathrm = \log_ A - \log_ A_\mathrm\left(\delta\right) = \log_ \left[A / A_\mathrm\left(\delta\right)\right],\$ where A is the maximum excursion of the Wood–Anderson seismograph, the empirical function A0 depends only on the epicentral distance of the station, $\delta$. In practice, readings from all observing stations are averaged after adjustment with station-specific corrections to obtain the value. Because of the logarithmic basis of the scale, each whole number increase in magnitude represents a tenfold increase in measured amplitude; in terms of energy, each whole number increase corresponds to an increase of about 31.6 times the amount of energy released, and each increase of 0.2 corresponds to approximately a doubling of the energy released. Events with magnitudes greater than 4.5 are strong enough to be recorded by a seismograph anywhere in the world, so long as its sensors are not located in the earthquake's Seismic shadowing, shadow. The following describes the typical effects of earthquakes of various magnitudes near the epicenter. The values are typical only. They should be taken with extreme caution since intensity and thus ground effects depend not only on the magnitude but also on the distance to the epicenter, the depth of the earthquake's focus beneath the epicenter, the location of the epicenter, and geological conditions (certain terrains can amplify seismic signals). (''Based on U.S. Geological Survey documents.'') The intensity and death toll depend on several factors (earthquake depth, epicenter location, and population density, to name a few) and can vary widely. Minor earthquakes occur every day and hour. On the other hand, great earthquakes occur once a year, on average. The largest recorded earthquake was the 1960 Valdivia earthquake, Great Chilean earthquake of May 22, 1960, which had a magnitude of 9.5 on the
moment magnitude scale The moment magnitude scale (MMS; denoted explicitly with or Mw, and generally implied with use of a single M for magnitude) is a measure of an earthquake An earthquake (also known as a quake, tremor or temblor) is the shaking of the surfac ...
. Seismologist Susan Hough has suggested that a magnitude 10 quake may represent a very approximate upper limit for what the Earth's tectonic zones are capable of, which would be the result of the largest known continuous belt of faults rupturing together (along the Pacific coast of the Americas). A research at the Tohoku University in Japan found that a magnitude 10 earthquake was theoretically possible if a combined of faults from the Japan Trench to the Kuril–Kamchatka Trench ruptured together and moved by (or if a similar large-scale rupture occurred elsewhere). Such an earthquake would cause ground motions for up to an hour, with tsunamis hitting shores while the ground is still shaking, and if this kind of earthquake occurred, it would probably be a 1-in-10,000 year event.

Magnitude empirical formulae

These formulae for Richter magnitude are alternatives to using Richter correlation tables based on Richter standard seismic event ($M_\mathrm=0$, $A=0.001\mathrm$, $D=100\mathrm$). Below, $\textstyle \Delta$ is the epicentral distance (in kilometers unless otherwise specified). The Lillie empirical formula is: :$M_\mathrm = \log_A - 2.48+ 2.76\log_\Delta$ where $A$ is the amplitude (maximum ground displacement) of the P-wave, in micrometers, measured at 0.8 Hz. For distances $D$ less than 200 km, :$M_\mathrm = \log_ A + 1.6\log_ D - 0.15$ and for distances between 200 km and 600 km, :$M_\mathrm = \log_ A + 3.0\log_ D - 3.38$ where $A$ is seismograph signal amplitude in mm and $D$ is in km. The Bisztricsany (1958) empirical formula for epicentral distances between 4˚ to 160˚ is: :$M_\mathrm = 2.92 + 2.25 \log_ \left(\tau\right) - 0.001 \Delta^$ where $\tau$ is the duration of the surface wave in seconds, and $\Delta$ is in degrees. is mainly between 5 and 8. The Tsumura empirical formula is: :$M_\mathrm = -2.53 + 2.85 \log_ \left(F-P\right) + 0.0014 \Delta^$ where $F-P$ is the total duration of oscillation in seconds. is mainly between 3 and 5. The Tsuboi, University of Tokyo, empirical formula is: :$M_\mathrm = \log_A + 1.73\log_\Delta - 0.83$ where $A$ is the amplitude in micrometers.

* 1935 in science * Rohn Emergency Scale for measuring the magnitude (intensity) of any emergency * Seismic intensity scales * Seismic magnitude scales * Timeline of United States inventions (1890–1945)#Great Depression and World War II (1929–1945), Timeline of United States inventions (1890–1945)

Sources

*. * *, NUREG/CR-1457. *. *. *. *. *. *.