Location via proxy:   [ UP ]  
[Report a bug]   [Manage cookies]                
SlideShare a Scribd company logo
1
WHAT ARE
MAGNITUDE
AND INTENSITY
2
3
Measuring A Quake
Magnitude – estimates the amount of energy released at the
source of the earthquake. The Richter Magnitude Scale
Intensity – a measure of the degree of earthquake shaking
at a given location based on the amount of damage. The
Mercalli Intensity Scale
4
Magnitude
Magnitude is a quantitative measure of the actual size of the
earthquake.
An increase in magnitude (M) by 1.0 implies 10 times higher
waveform amplitude and about 31 times higher energy
released.
For instance, energy released in a M7.7 earthquake is
about 31 times that released in a M6.7 earthquake, and is
about 1000 (31×31) times that released in a M5.7
earthquake.
(Did you know? The energy released by a M6.3
earthquake is equivalent to that released by the 1945 Atom
Bomb dropped on Hiroshima!!)
Source: http::/www.nicee.org/nicee/EQReports/Bhuj/isoseismal.html
5
What is Richter Magnitude?
Seismologists use a Magnitude scale to express the seismic
energy released by each earthquake. Here are the typical
effects of earthquakes in various magnitude ranges:
Earthquake Severity
Richter Magnitudes Earthquake Effects
Less than 3.5 Generally not felt, but recorded.
3.5-5.4 Often felt, but rarely causes damage.
Under 6.0 At most slight damage to well-designed buildings.
Can cause major damage to poorly constructed
buildings over small regions.
6.1-6.9 Can be destructive in areas up to about 100
kilometers across where people live.
7.0-7.9 Major earthquake. Can cause serious damage over
larger areas.
8 or greater Great earthquake. Can cause serious damage in
areas several hundred kilometers across.
6
Intensity
Although each earthquake has a unique Magnitude, its effects will vary
greatly according to distance, ground conditions, construction standards, and
other factors.
Intensity should not be confused with magnitude. It is an arbitrary ranking
based on observed effects.
Intensity is a qualitative measure of the actual shaking at a location during
an earthquake, and is assigned as Roman Capital Numerals.
7
Isoseismal Map of the 2001 Bhuj (India) Earthquake (MSK Intensity)
Source: http::/www.nicee.org/nicee/EQReports/Bhuj/isoseismal.html
8
I. Not felt except by a
very few under especially
favorable conditions.
II. Felt only by a few persons
at rest, especially on upper
floors of buildings.
III. Felt quite noticeably by persons
indoors, especially on upper floors
of buildings. Many people do not
recognize it as an earthquake.
Standing motor cars may rock
slightly. Vibrations similar to the
passing of a truck. Duration
estimated.
Earthquake intensities are rated with Roman numerals ranging
from I (not felt) to XII (buildings nearly destroyed). The
abbreviated description of the 12 levels of Modified Mercalli
intensity is shown as follows……..
Source: Poster MMI Scale – NSET, Nepal
9
IV. Felt indoors by many, outdoors
by few during the day. At night,
some awakened. Dishes, windows,
doors disturbed; walls make
cracking sound. Sensation like
heavy truck striking building.
Standing motor cars rocked
noticeably.
V. Felt by nearly everyone; many
awakened. Some dishes, windows
broken. Unstable objects
overturned. Pendulum clocks may
stop.
VI. Felt by all, many frightened.
Some heavy furniture moved; a few
instances of fallen plaster. Damage
slight.
Source: Poster MMI Scale – NSET, Nepal
10
VII. Damage negligible in buildings of good design and construction; slight to
moderate in well-built ordinary structures; considerable damage in poorly built
or badly designed structures; some chimneys broken.
VIII. Damage slight in specially designed structures; considerable damage in
ordinary substantial buildings with partial collapse. Damage great in poorly built
structures. Fall of chimneys, factory stacks, columns, monuments, walls. Heavy
furniture overturned. Source: Poster MMI Scale – NSET, Nepal
11
IX. Damage considerable in specially designed structures; well-designed frame
structures thrown out of plumb. Damage great in substantial buildings, with
partial collapse. Buildings shifted off foundations.
X. Some well-built wooden structures destroyed; most masonry and frame
structures destroyed with foundations. Rails bent.
Source: Poster MMI Scale – NSET, Nepal
12
XI. Few, if any (masonry) structures remain standing. Bridges destroyed.
Rails bent greatly.
XII. Damage total. Lines of sight and level are distorted. Objects
thrown into the air.
Source: Poster MMI Scale – NSET, Nepal
13
The Modified Mercalli and Richter Scale – side by side
Text Source: Microsoft Encarta Encyclopedia
14
Earthquake Occurrence
15
Frequency of Occurrence of Earthquakes
Descriptor Magnitude Average Annually
Great 8 and higher 1 ¹
Major 7 - 7.9 17 ²
Strong 6 - 6.9 134 ²
Moderate 5 - 5.9 1319 ²
Light 4 - 4.9
13,000
(estimated)
Minor 3 - 3.9
130,000
(estimated)
Very Minor 2 - 2.9
1,300,000
(estimated)
¹ Based on observations since 1900.
² Based on observations since 1990.
The US Geological Survey (USGS) estimates that several million earthquakes occur in
the world each year
Source: http://neic.usgs.gov/neis/eqlists/eqstats.html
16

More Related Content

Lecture-4 EQ.pdf

  • 2. 2
  • 3. 3 Measuring A Quake Magnitude – estimates the amount of energy released at the source of the earthquake. The Richter Magnitude Scale Intensity – a measure of the degree of earthquake shaking at a given location based on the amount of damage. The Mercalli Intensity Scale
  • 4. 4 Magnitude Magnitude is a quantitative measure of the actual size of the earthquake. An increase in magnitude (M) by 1.0 implies 10 times higher waveform amplitude and about 31 times higher energy released. For instance, energy released in a M7.7 earthquake is about 31 times that released in a M6.7 earthquake, and is about 1000 (31×31) times that released in a M5.7 earthquake. (Did you know? The energy released by a M6.3 earthquake is equivalent to that released by the 1945 Atom Bomb dropped on Hiroshima!!) Source: http::/www.nicee.org/nicee/EQReports/Bhuj/isoseismal.html
  • 5. 5 What is Richter Magnitude? Seismologists use a Magnitude scale to express the seismic energy released by each earthquake. Here are the typical effects of earthquakes in various magnitude ranges: Earthquake Severity Richter Magnitudes Earthquake Effects Less than 3.5 Generally not felt, but recorded. 3.5-5.4 Often felt, but rarely causes damage. Under 6.0 At most slight damage to well-designed buildings. Can cause major damage to poorly constructed buildings over small regions. 6.1-6.9 Can be destructive in areas up to about 100 kilometers across where people live. 7.0-7.9 Major earthquake. Can cause serious damage over larger areas. 8 or greater Great earthquake. Can cause serious damage in areas several hundred kilometers across.
  • 6. 6 Intensity Although each earthquake has a unique Magnitude, its effects will vary greatly according to distance, ground conditions, construction standards, and other factors. Intensity should not be confused with magnitude. It is an arbitrary ranking based on observed effects. Intensity is a qualitative measure of the actual shaking at a location during an earthquake, and is assigned as Roman Capital Numerals.
  • 7. 7 Isoseismal Map of the 2001 Bhuj (India) Earthquake (MSK Intensity) Source: http::/www.nicee.org/nicee/EQReports/Bhuj/isoseismal.html
  • 8. 8 I. Not felt except by a very few under especially favorable conditions. II. Felt only by a few persons at rest, especially on upper floors of buildings. III. Felt quite noticeably by persons indoors, especially on upper floors of buildings. Many people do not recognize it as an earthquake. Standing motor cars may rock slightly. Vibrations similar to the passing of a truck. Duration estimated. Earthquake intensities are rated with Roman numerals ranging from I (not felt) to XII (buildings nearly destroyed). The abbreviated description of the 12 levels of Modified Mercalli intensity is shown as follows…….. Source: Poster MMI Scale – NSET, Nepal
  • 9. 9 IV. Felt indoors by many, outdoors by few during the day. At night, some awakened. Dishes, windows, doors disturbed; walls make cracking sound. Sensation like heavy truck striking building. Standing motor cars rocked noticeably. V. Felt by nearly everyone; many awakened. Some dishes, windows broken. Unstable objects overturned. Pendulum clocks may stop. VI. Felt by all, many frightened. Some heavy furniture moved; a few instances of fallen plaster. Damage slight. Source: Poster MMI Scale – NSET, Nepal
  • 10. 10 VII. Damage negligible in buildings of good design and construction; slight to moderate in well-built ordinary structures; considerable damage in poorly built or badly designed structures; some chimneys broken. VIII. Damage slight in specially designed structures; considerable damage in ordinary substantial buildings with partial collapse. Damage great in poorly built structures. Fall of chimneys, factory stacks, columns, monuments, walls. Heavy furniture overturned. Source: Poster MMI Scale – NSET, Nepal
  • 11. 11 IX. Damage considerable in specially designed structures; well-designed frame structures thrown out of plumb. Damage great in substantial buildings, with partial collapse. Buildings shifted off foundations. X. Some well-built wooden structures destroyed; most masonry and frame structures destroyed with foundations. Rails bent. Source: Poster MMI Scale – NSET, Nepal
  • 12. 12 XI. Few, if any (masonry) structures remain standing. Bridges destroyed. Rails bent greatly. XII. Damage total. Lines of sight and level are distorted. Objects thrown into the air. Source: Poster MMI Scale – NSET, Nepal
  • 13. 13 The Modified Mercalli and Richter Scale – side by side Text Source: Microsoft Encarta Encyclopedia
  • 15. 15 Frequency of Occurrence of Earthquakes Descriptor Magnitude Average Annually Great 8 and higher 1 ¹ Major 7 - 7.9 17 ² Strong 6 - 6.9 134 ² Moderate 5 - 5.9 1319 ² Light 4 - 4.9 13,000 (estimated) Minor 3 - 3.9 130,000 (estimated) Very Minor 2 - 2.9 1,300,000 (estimated) ¹ Based on observations since 1900. ² Based on observations since 1990. The US Geological Survey (USGS) estimates that several million earthquakes occur in the world each year Source: http://neic.usgs.gov/neis/eqlists/eqstats.html
  • 16. 16