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The Richter And Mercalli Scales
The strength of an earthquake is usually measured on one of two scales, the Modified Mercalli Scale and the Richter Scale. The Mercalli
Scale is a rather arbitrary set of definitions based upon what people in the area feel, and their observations of damage to buildings
around them. These scales are important to business and property owners in earthquake affected areas. Several of them use various
forms of facility maintenance software to record intesity levels and make other notes if an earthquake does occur.
The scale goes from 1 to 12, ( I to XII) or using the descriptive titles of the levels, from Instrumental to Catastrophic.
Modified Mercalli Scale
Intensity
Verbal
Description
Magnitude Witness Observations
I Instrumental 1 to 2 Detected only by seismographs
II Feeble 2 to 3 Noticed only by sensitive people
III Slight 3 to 4 Resembling vibrations caused by heavy traffic
IV Moderate 4 Felt by people walking; rocking of free standing objects
V
Rather
Strong
4 to 5 Sleepers awakened and bells ring
VI Strong 5 to 6 Trees sway, some damage from overturning and falling object
VII Very Strong 6 General alarm, cracking of walls
VIII Destructive 6 to 7 Chimneys fall and there is some damage to buildings
IX Ruinous 7 Ground begins to crack, houses begin to collapse and pipes break
X Disasterous 7 to 8
Ground badly cracked and many buildings are destroyed.There are
some landslides
XI
Very
Disasterous
8
Few buildings remain standing; bridges and railways destroyed;water,
gas, electricity and telephones out of action.
XII Catastrophic
8 or
greater
Total destruction; objects are thrown into the air,much heaving,shaking
and distortion of the ground
Whilst this scale is fine if you happen to experience an earthquake in an inhabited area of a developed country, it is of no use whatsoever
in the middle of a desert or in any other place without trees, houses and railways! Descriptions such as "Resembling vibrations caused by
heavy traffic." depend very much upon the observer having felt heavy traffic in the past. Even then, what one person in a small town
considers to be 'heavy' will most certainly differ from what a person living adjacent to a major urban road system would describe as
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'heavy'.
Clearly this scale has advantages, but something else is required if we are to be able to compare the magnitude of earthquakes wherever
they occur. The Intensity Scale differs from the Richter Magnitude Scale in that the effects of any one earthquake vary greatly from place
to place, so there may be many Intensity values (e.g.: IV, VII) measured for the same earthquake. Each earthquake, on the other hand,
should have only one Magnitude, although the various methods of calculating it may give slightly different values (e.g.: 4.5, 4.6).
The Richter Scale is designed to allow easier comparison of earthquake magnitudes, regardless of the location.
C.F.Richter was a geologist living and working in California, U.S.A, an area subjected to hundreds of 'quakes every year. He took the
existing Mercalli scale and tried to add a 'scientific' scale based on accurate measurements that could be recorded by seismographs (
instruments used to measure vibration) regardless of their global location.
By measuring the speed, or acceleration, of the ground when it suddenly moves, he devised a scale that reflects the 'magnitude' of the
shock.
The Richter scale for earthquake measurements is logarithmic. This means that each whole number step represents a ten-fold increase in
measured amplitude. Thus, a magnitude 7 earthquake is 10 times larger than a 6, 100 times larger than a magnitude 5 and 1000 times
as large as a 4 magnitude.
This is an open ended scale since it is based on measurements not descriptions.
An earthquake detected only by very sensitive people registers as 3.5 on his scale, whilst the worst earthquake ever recorded reached
8.9 on the 'Richter Scale'.
When trying to understand the forces of an earthquake it can help to concentrate just upon the up and down movements. Gravity is a force
pulling things down towards the earth. This accelerates objects at 9.8 m/s2. To make something, such as a tin can, jump up into the air
requires a shock wave to hit it from underneath travelling faster than 9.8m/s2. This roughly corresponds to 11 (Very disastrous) on the
Mercalli Scale, and 8.1 or above on the Richter Scale. In everyday terms, the tin can must be hit by a force that is greater than that which
you would experience if you drove your car into a solid wall at 35 khp (22 mph).
Richter Scale
Richter
Scale
Approximate
Acceleration
Approximate
Mercalli equivalent
<3.5 < 1 cm/s2 I
3.5
2.5 cm/s2
II
4.2 III
4.5 10 cm/s2 IV
4.8 25 cm/s2 V
5.4 50 cm/s2 VI
6.1 100 cm/s2 VII
6.5
250 cm/s2
VIII
6.9 IX
7.3 500 cm/s2 X
8.1 750 cm/s2 XI
> 8.1 980 cm/s2 XII
d
We value your ideas and suggestions. Please contact the maintainer of this site.
This site can be found at:http://www.geography-site.co.uk
Last Modified on: March 26, 2013
© Geography Site

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Richter scale and mercalli scale

  • 1. d d d The Richter And Mercalli Scales The strength of an earthquake is usually measured on one of two scales, the Modified Mercalli Scale and the Richter Scale. The Mercalli Scale is a rather arbitrary set of definitions based upon what people in the area feel, and their observations of damage to buildings around them. These scales are important to business and property owners in earthquake affected areas. Several of them use various forms of facility maintenance software to record intesity levels and make other notes if an earthquake does occur. The scale goes from 1 to 12, ( I to XII) or using the descriptive titles of the levels, from Instrumental to Catastrophic. Modified Mercalli Scale Intensity Verbal Description Magnitude Witness Observations I Instrumental 1 to 2 Detected only by seismographs II Feeble 2 to 3 Noticed only by sensitive people III Slight 3 to 4 Resembling vibrations caused by heavy traffic IV Moderate 4 Felt by people walking; rocking of free standing objects V Rather Strong 4 to 5 Sleepers awakened and bells ring VI Strong 5 to 6 Trees sway, some damage from overturning and falling object VII Very Strong 6 General alarm, cracking of walls VIII Destructive 6 to 7 Chimneys fall and there is some damage to buildings IX Ruinous 7 Ground begins to crack, houses begin to collapse and pipes break X Disasterous 7 to 8 Ground badly cracked and many buildings are destroyed.There are some landslides XI Very Disasterous 8 Few buildings remain standing; bridges and railways destroyed;water, gas, electricity and telephones out of action. XII Catastrophic 8 or greater Total destruction; objects are thrown into the air,much heaving,shaking and distortion of the ground Whilst this scale is fine if you happen to experience an earthquake in an inhabited area of a developed country, it is of no use whatsoever in the middle of a desert or in any other place without trees, houses and railways! Descriptions such as "Resembling vibrations caused by heavy traffic." depend very much upon the observer having felt heavy traffic in the past. Even then, what one person in a small town considers to be 'heavy' will most certainly differ from what a person living adjacent to a major urban road system would describe as WaveRadar REX rsaqua.co.uk The King of wave measuring sensors. Offshore, coastal and renewable.
  • 2. 'heavy'. Clearly this scale has advantages, but something else is required if we are to be able to compare the magnitude of earthquakes wherever they occur. The Intensity Scale differs from the Richter Magnitude Scale in that the effects of any one earthquake vary greatly from place to place, so there may be many Intensity values (e.g.: IV, VII) measured for the same earthquake. Each earthquake, on the other hand, should have only one Magnitude, although the various methods of calculating it may give slightly different values (e.g.: 4.5, 4.6). The Richter Scale is designed to allow easier comparison of earthquake magnitudes, regardless of the location. C.F.Richter was a geologist living and working in California, U.S.A, an area subjected to hundreds of 'quakes every year. He took the existing Mercalli scale and tried to add a 'scientific' scale based on accurate measurements that could be recorded by seismographs ( instruments used to measure vibration) regardless of their global location. By measuring the speed, or acceleration, of the ground when it suddenly moves, he devised a scale that reflects the 'magnitude' of the shock. The Richter scale for earthquake measurements is logarithmic. This means that each whole number step represents a ten-fold increase in measured amplitude. Thus, a magnitude 7 earthquake is 10 times larger than a 6, 100 times larger than a magnitude 5 and 1000 times as large as a 4 magnitude. This is an open ended scale since it is based on measurements not descriptions. An earthquake detected only by very sensitive people registers as 3.5 on his scale, whilst the worst earthquake ever recorded reached 8.9 on the 'Richter Scale'. When trying to understand the forces of an earthquake it can help to concentrate just upon the up and down movements. Gravity is a force pulling things down towards the earth. This accelerates objects at 9.8 m/s2. To make something, such as a tin can, jump up into the air requires a shock wave to hit it from underneath travelling faster than 9.8m/s2. This roughly corresponds to 11 (Very disastrous) on the Mercalli Scale, and 8.1 or above on the Richter Scale. In everyday terms, the tin can must be hit by a force that is greater than that which you would experience if you drove your car into a solid wall at 35 khp (22 mph). Richter Scale Richter Scale Approximate Acceleration Approximate Mercalli equivalent <3.5 < 1 cm/s2 I 3.5 2.5 cm/s2 II 4.2 III 4.5 10 cm/s2 IV 4.8 25 cm/s2 V 5.4 50 cm/s2 VI 6.1 100 cm/s2 VII 6.5 250 cm/s2 VIII 6.9 IX 7.3 500 cm/s2 X 8.1 750 cm/s2 XI > 8.1 980 cm/s2 XII
  • 3. d We value your ideas and suggestions. Please contact the maintainer of this site. This site can be found at:http://www.geography-site.co.uk Last Modified on: March 26, 2013 © Geography Site