There are a number of differing scales used to rate earthquakes depending on whether you are interested in their magnitude (the amount of energy released when they occur) or their intensity (a measurement of the amount of damage caused and severity of ground shaking in a given area).
There are two primary magnitude scales currently in use, the Richter (or local) magnitude scale and the moment magnitude scale. The Richter magnitude scale estimates earthquake magnitude based on the amplitude of seismic waves as recorded by a seismometer. The Richter scale is logarithmic and each single increment relates to a ten times increase in detected seismic wave amplitude and a 31 times increase in energy.
The Richter magnitude scale was originally developed for deriving the magnitude of small and medium sized earthquakes (those with magnitudes less than 7) at epicentral distances relatively close to a seismometer station (less than 600 km). As such it is poor at resolving large earthquakes as it relies on the detection of high frequency seismic waves that have wavelengths which are shorter than the rupture lengths of large earthquakes.
To attempt to improve the Richter scale for use in larger earthquakes and at greater epicentral distances, Charles Richter and Beno Guttenberg developed the surface and body wave magnitude scales. The surface wave magnitude scale derives magnitudes from the measured amplitude of Rayleigh surface waves at long distances. The Body wave magnitude scale is intended to be used to derive the magnitude of deep-focus earthquakes. Both scales are designed so that they produce magnitude numbers that are consistent with those from the Richter Local magnitude scale, and these improvements extended it's validity to earthquakes with magnitudes up to 8, however to measure earthquakes with magnitudes beyond this a new magnitude scale was required.
This new scale was developed in the 1970s and is known as the moment magnitude scale and derives the magnitude based on an earthquakes seismic moment. This is a calculation based on the length of the fault zone which ruptured, the amplitude of the fault movement when the rupture occurred (the length and amplitude giving a rupture cross sectional area) and the elastic modulus of the rock mass around the fault zone. It was decided that the familiar logarithmic scale produced by the Richter methodology be maintained to allow direct comparisons to be made and so the moment magnitude is also reported on the familiar scale.
Although more accurate at treating larger earthquakes the seismic moment and hence moment magnitude of an earthquake is more difficult to derive than the Richter magnitude and so initial estimates are most commonly made using the Richter scale. The common range of magnitudes and their relative effects are described below:
Less than 2.0: Micro - not felt.
2.0-2.9: Minor - not felt, but recorded.
3.0-3.9: Minor - felt, but rarely causes damage.
4.0-4.9: Light - noticeable shaking of items, damage unlikely.
5.0-5.9: Moderate - damage to poorly constructed buildings, unlikely damage to specially designed buildings.
6.0-6.9: Strong - destructive for up to 100 miles across populated areas.
7.0-7.9: Major - serious damage over large areas.
8.0-8.9: Great - serious damage over areas of several hundred miles.
9.0-9.9: Great - devastating damage in areas thousands of miles across.
10.0+: Great - yet to be recorded.
The intensity of an earthquake is currently most commonly measured using the
Modified Mercalli Intensity scale.
The scale indicates the perceived intensity of ground shaking based on the damage caused by an earthquake to buildings and infrastructure and the opinions of witnesses as to the severity of the felt ground movement.
In order to attempt to quantify the Mercalli scale and decrease it's reliance on the subjective opinion of witnesses, the USGS also include data of measured ground accelerations taken from seismometers in the formulation of the Mercalli value. In Europe earthquake intensity is derived using the Macroseismic scale which is essentially a further modification to the Modified Mercalli scale but essentially works the same way and in Japan and Taiwan, the Japan Meteorological Agency seismic intensity scale is used. This again is similar in concept to the Mercalli scale although the values and descriptions of damage used are somewhat different.
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The Richter scale was originally developed to measure the strength or magnitude of moderate earthquakes (magnitudes less than 7). The surface wave magnitude scale was then developed by Richter and Guttenburg to allow larger earthquake magnitudes to be measured (up to 8). To measure large earthquakes the moment magnitude scale must be used. To measure the severity of earthquakes, the Modified Mercalli intensity scale is used in the US and the Macroseismic scale is used in Europe.
The name given to multiple small earthquakes that are now occurring in southern California is a "swarm." Swarms are characterized by a sequence of seismic events in a particular region within a short period of time. They can help scientists monitor and study the behavior of faults in the area.
Earthquake intensity is measured using the Modified Mercalli Scale. The scale indicates the perceived damage from an earthquake. These parameters are subjective: they depend on the conditions of buildings and the opinions of witnesses. To make the scale more objective, the US Geological Survey also use measurements of ground accelerations to measure earthquake intensity. Earthquake magnitude is measured using the Richter magnitude scale and is widely reported as a measurement of earthquake strength (derived from the peak amplitude of the seismic wave from an earthquake as measured on a seismometer), but it has largely been replaced by the moment magnitude scale (derived based on the elastic moduli of the crust where the earthquake occurred, the length of the slip surface and the cross sectional area of the slip surface) which estimates the total energy released in an earthquake.
The name of a person that predicts an earthquake is a mineralogist.
The temperature scale used to measure Earth's heat is called the Celsius scale.
Richter scale
The name of the CalTech seismologist who invented the scale used to measure the magnitude of earthquakes is Charles F. Richter. The scale is called the Richter scale and measures the energy released by an earthquake at its source.
The Rickter (RICK-tur) scale has been popular for decades to measure the intensity of earthquakes, yet it had its issues. These days the Mercalli scale is most often used by geologists and vulcanologists.
Charles F. Richter and German-born seismologist Beno Gutenberg, developed the scale that bears his name the Richter scale. and measures the magnitude of earthquakes.
The Richter scale was originally developed to measure the strength or magnitude of moderate earthquakes (magnitudes less than 7). The surface wave magnitude scale was then developed by Richter and Guttenburg to allow larger earthquake magnitudes to be measured (up to 8). To measure large earthquakes the moment magnitude scale must be used. To measure the severity of earthquakes, the Modified Mercalli intensity scale is used in the US and the Macroseismic scale is used in Europe.
There are three: Mercalli, for intensity ergo the damages it produce and how it fells; Richter, to know the energy that is released in the epicenter; Moment Magnitude Scale, is a modern version of the Richter scale. I also think there is other version of the mercalli scale, with obviously other name, but I am not totally sure.
There are a number of earthquake magnitude scales, including the moment magnitude scale (the scale currently favoured by seismologists), the Richter or local magnitude scale and the surface wave magnitude scale.
# Earthquake Measurement Earthquake measurement is not a simple problem. It is hampered by many things. Few people are capable of observing carefully what is happening around them when they are experiencing an earthquake. # Measuring an Earthquake The first practical scale for measuring earthquakes was developed by geologist Charles Richter at the California Institute of Technology in the 1930s, and the scale that most scientists use today still bears his name. # How do scientists measure earthquakes? With a really big ruler? No, not quite. There are two ways in which scientists quantify the size of earthquakes: magnitude and intensity. # Seismograph In the history of the innovations surrounding earthquake study, we have to look at two things: the devices that recorded earthquake activity and the measurement systems written to help interpret that data. Remember that the Richter scale is not a physical device, but a mathematical formula. # Measuring, Monitoring, and Predicting Scientists have long been using seismometers to measure the shaking of earthquakes. At its most basic, a seismometer is simply a needle or a pen suspended in the air, which makes a mark on a moving roll of paper. When the needle shakes, the pen makes a squiggle on the paper; the larger the shaking, the larger the squiggle.
Earthquake can be also called a tectonic slip,macro-seism or microseism depending on its impact according to the Richter scale.
The graph used to measure earthquakes is called a seismogram. It records the ground motion during an earthquake and helps seismologists analyze the earthquake's characteristics, such as magnitude and duration.
The Richter Magnitude Scale is a system used to measure the quantity of energy released during an earthquake. It measures the earthquakes magnitude- energy released. It was Developed in 1935 by Charles F Richter of the California Institute of Technology. As his creation, it was named after him. And that's how it got the name 'Richter Scale'. Hope that helped. yea
Not exactly, aftershocks are (as the name suggests) after the earthquake and their magnitude is only 1-2 on the scale (normally a lot less than the earthquake it self) :)