Title: History of Seismology
1History of Seismology
- Early science
- seismology before computers
- 1880-1960
- Seismology since computers
- 1960-present
2Earthquake mythology ancient beliefs
- India The earth is held up by 4 elephants that
stand on the back of a turtle. The turtle is
balanced on top of a cobra. When the animals
move, the earth trembles and shakes - Siberia The Earth rests on a sled driven by the
god named Tuli. The dogs have fleas, When they
stop to scratch, the Earth shakes - Japan A great catfish, or namazu, lies curled up
under the sea, with the islands of Japan resting
on its back. A demigod, or daimyojin, holds a
heavy stone over his head to keep him from
moving. Once in a while, though, the daimyojin is
distracted, the namzu moves and the earth
trembles - New Zealand Mother Earth has a child in its
womb, the young god Ru. When he stretches and
kicks as babies do, he causes earthquakes. - From www.fema.gov
3Native tales and the Cascadia megathrust
earthquakes
- Stories from the Hoh and Quillette tribes of the
Olympic Peninsula of north west Washington
describe an epic battle between the supernatural
beings Thunderbird and Whale. - The great Thunderbird finally carried the
weighty animal to its nest in the lofty mountains
and there was a final and terrible contest
fought. There was shaking, jumping up and down
and trembling of the earth beneath, and the
rolling up of the great waters. - A reference to the Cascadia Megathrust
earthquake of 1705? - From The Pacific Northwest Seismograph Network
www.ess.washington.edu
4Beginning of the scientific method
- The Buddha
- (563-483 century BC)
- Believe nothing merely because you have been
told it, or because it is tradition, or because
you yourself have imagined it. - Do not believe what your teacher tells you merely
out of respect for him. - But whatever, after due examination and analysis,
you find to be conducive to the good, the
benefit, the welfare of all beings, believe and
cling to that doctrine, and take it as your
guide.
5Greek contributubtion - Nature
- Thales (6th Century BC)
- The crucial contribution of Thales to scientific
thought was the discovery of nature. By this, we
mean the idea that the natural phenomena we see
around us are explicable in terms of matter
interacting by natural laws, and are not the
results of arbitrary acts by gods. - Thales' theory of earthquakes,
- The (presumed flat) earth is actually floating on
a vast ocean, and disturbances in that ocean
occasionally cause the earth to shake or even
crack, just as they would a large boat.
6Greek contributubtion - geometry
- One of the most important contributions of the
Greeks was their development of Geometry,
culminating in Euclid's Elements, a giant
textbook containing all the known geometric
theorems at that time (about 300 BC), presented
in an elegant logical fashion. - E.g. The Pythagorean Theorem (the most famous
theorem) - The square on the hypotenuse of a right angle
triangle the sum of the squares on the other 2
sides - Led to the discovery of irrational numbers such
as SQRT(2.0)
7Greek contribution - Archimedes
- Archimedes (287-212 BC)
- One of the greatest Greek mathematicians and
Physicists - Discovered Archimedes Principle ---laws of
Buoyancy density etc - Discovered law of lever, centre of gravity
- Almost invented logarithms and calculus
8Greek contribution - Ptolemy
- Ptolemy (87-150AD)
- Astronomer, mathematician and geographer.
- He believed the planets and sun orbit the Earth
in the order Mercury, Venus, Sun, Mars, Jupiter,
Saturn . This system became known as the
Ptolemaic system. - The Ptolemaic view of the universe was the
considered by western scientists and religious
leaders to be the true picture of the universe
for 1400 years
9The first seismic instrument
- The Chinese Seismoscope Invented 132 AD
- The instrument is reported to have detected a
four-hundred-mile distant earthquake which was
not felt at the location of the seismoscope.
10Arabic contribution
- Al-Hazen, as Europeans referred to Ibn Al-Haytham
(d. 1040) was universally acknowledged to have
gone beyond the Greeks in optics. - European mathematics continued to build on Arab
advances. - Hindu-Arabic Science
- The modern system of numerals, which was
replacing the old, cumbersome system of "Roman
numerals" in the fifteenth and sixteenth
centuries, was brought to Europe from India by
Arabic traders. - By streamlining calculations, "Hindu-Arabic
numerals immeasurably expanded the ease of doing
mathematics.
11The European Scientific Revolution
- The Scientific Revolution (1543- )
- 1543 - the year that Capernicus published his
famous work on The Revolution of the Heavenly
Bodies - Put sun at centre of universe with planets
circling the sun. - Tycho Brahe (1546-1601) --- Invented telescope
- Frances Bacon (1561-1626) --- Pioneered the
scientific method using inductive reasoning. - Kepler (1571-1630) ---- showed orbits of
planets are ellipses - William Gilbert (1540-1603) --- argued that the
Earth was a magnet
12Sir Isaac Newton (1642-1727)
- Newton is ranked as the most influential figure
in the history of Western science (Simmons,1996) - Best known for his 3 laws of motion.
- (i) The law of inertia
- A body in motion moves with constant velocity
unless acted upon by some force. - A body at rest remains at rest unless acted upon
by some force. - (ii) An object's acceleration is directly
proportional to the object's mass (Fma) - (iii) To every action there is an equal and
opposite reaction - Law of Gravity
- The gravitational force between 2 bodies is
- proportional to the product of their masses
and - inversely proportional to the square of the
distance - between them
- Invented Calculus
13Robert Hooke (1635 - 1703)
- Natural philosopher, inventor
- Robert Hooke is one of the most neglected natural
philosophers of all time. The inventor of - the iris diaphragm in cameras,
- the universal joint used in motor vehicles,
- the balance wheel in a watch
- the originator of the word 'cell' in biology
- Best known for Hooke's Law
- stress is proportional to strain
14Christian Huygens (1629-1695)
- Improved telescope and resolved numerous
astronomical questions - Invented pendulum clock and balance clocks to
improve the measurement of time - worked on wave theory of light
- discovered polarized light
- deduced laws of reflection and refraction
- Huygen's Principal Every point on a wave
front can be regarded as a new source of waves
15The first scientifically studied earthquake
- The Lisbon Earthquake (Nov 1, 1755)
- Probably magnitude 9 with a 3 large tsunamis,
thousands killed - epicentre 200 km off SW corner of Portugal
- destroyed the city of Lisbon, Portugal
- tsunami's struck England and were detected across
the Atlantic Ocean in North America - Its widespread physical effects aroused a wave
of scientific interest and research into
earthquakes.
(From geology.about.com/library/
bl/bllisbon1755eq.htm)
16The Lisbon Earthquake
- J. Mitchel (1761) and J. Drijhout (1765)
- Noted the separation of the earthquake source
from the effects that it produced - proposed that the distant motion was caused by a
wave propagating from a specific location. - Mitchel suggested that the vibrations close to
the source were related to wave propagating
through the elasticity of the rocks - Suggested the cause of the earthquake itself was
caused by water vaporized by sudden contact with
underground fires.
17Earthquake Studies before 1880
- first systematic catalogue of shocks - Van Hoff
and A Perry - First intensity scale - P. Eagen (1828)
- followed by M De Rossi, F. Forel and G. Mercalli
intensity scales - first isoseismal map - J. Noggerath (1847)
- C. Lyell - showed earthquakes could cause
vertical motions over large areas - Studied the 1819 Rann and Cutch earthquake in
India - 1822 and 1835 Chulian earthquakes
- 1855 Wairrarapa earthquake in New Zealand
- R. Mallet (1810-1881 ) Irish geologist and
engineer - Constructed one of the most complete earthquake
catalogues to date - Made an attempt to measure seismic velocities
using explosive sources - believed earthquakes were caused by the sudden
expansion of steam as water met hot rock
18Earthquake Locations - Mallet, 1868.
19Earthquake Studies before 1880
- Early seismic instruments
- 1856 L. Palmiero built a seismoscope that also
recorded time - 1873 Verbeck first pendulum observations
- 1875 Cecchi, Italy built first seismometer
- 1880 Wegner constructed a common-pendulum
seismometer which did not write records. - Wegner detected 27 earthquakes.
- None of above instruments worked very well
- J. Milne, J. Ewing and T. Gray developed first
successful working seismographs in 1880-1885
period
20Earthquake studies after 1880
- Ewing used a horizontal pendulum seismometer to
detect earthquakes - Circular smoked paper record obtained by Ewing's
seismograph of a local earthquake in Japan on
March 8, 1881.
21- Milne and Gray (1881) conducted experiments on
the propagation of elastic waves - artificial sources such as dynamite blasts.
- obtained an apparent velocity of 500 feet /sec.
- The farthest station was 400 feet from the
source.
22First recording of a distant earthquake
- April 18, 1889
- In Potsdam, Germany, E. von-Rebeur-Pashwitz had
built a sensitive horizontal pendulum seismograph
for measuring tidal tilts, his interest was
primarily astronomical. - The figure below is an engraving of the recording
he made of the 1989 earthquake in Japan
23Seismology milestones (1880-)
- Waves
- Lord Rayleigh (1842-1919) - Predicted Rayleigh
waves (1885) - Richard Oldham (1900) - identified P waves, S
waves and Rayleigh waves from records of the
1897 Assam earthquake - A E. H. Love (1863-1940) - predicted existence
of Love waves (1911) - Earth structure
- Oldham (1906) - confirmed the existence of the
Earth's core - A. Mohorovicic (1909) - Discovered the Moho from
analysis of data at relatively short distance
from earthquake (the Kulpa Valley earthquake in
Croatia) - I. Lehman (1936) showed that the core has a solid
inner core.
24Earth structure
- H. Jeffereys (1891-1989) and K. Bullen
(1906-1976) - Used large volumes of data and improved analysis
of epicentre locations and derived new standard
earth model - The Jeffreys-Bullen Seismological Tables (1940)
- Showed earth nearly spherical symmetrical with
only a few discontinuities. - Showed core-mantle boundary separated a solid
mantle from a liquid core.
25Jeffreys-Bullen Earth Model
26Earthquake mechanism (1911-1950)
- 1911 Reid's strain rebound theory -
earthquakes related to faults - 1917 T. Shida first to show that the first
motions could be divided into quadrants separated
by nodal lines - 1923 Nekano provided the first theoretical
treatment of the fault source mechanism - 1935 Richter developed the Richter magnitude
scale - Other pioneers in this area
- Byerly, S. Nakamura, S. Kunitomi, H.Honda, M.
Ishimoto and Keilis Borok - Arguments both for single couple and
double-couple sources were presented. - J. Hodgson attempted to use S waves to
distinguish between the double-and single couple
sources.
27Seismic Vault in 1950s
Data is stored on photographic paper and sent to
others using microfilm
28The computer and seismology
- The practical computer (1960 onwards)
- The tape recorder--- analogue, then digital---
reel to reel, cassettes, Exabyte etc - Punch cards and paper tape replaced with
interactive terminal - 1980 - Personal computers 1985 -
- GPS and satellite communication -
- The internet 1995-
- Memory-- diskettes, CD , DVD, flash sticks, 300
gigabyte drives - The memory of 1 DVD approximately that of 4000
diskettes - The slide-rule was replaced with the pocket
calculator in 1972
Price 395 US in 1972
29New tools for seismologists
- Finite difference analysis
- Synthetic Seismograms
- Ray tracing
- Numerous Inversion techniques
- Digital filtering numerous filters --- band-pass,
wave shaping, stacking , velocity etc - Fast Fourier Transform (FFT) --- Cooley Tukey
1967 --- - reduce the number of computations from N N to
NlogN - Example-- get the spectrum of a seismic trace 60
seconds long sampled at 100 samples/sec - N 6000 - NN 36,000,000
- - NlogN 22,669
- The FFT is 1,588 times faster in this example
30The Nuclear Test Ban Treaty
- 1963 The limited test-ban treaty signed
- Funding resulted in improved instrumentation
around the world - This was particularly for the World Wide
Standardized Seismic Network (WWSSN) - 120 standardized recording stations located
world-wide - Numerous seismic arrays were also set up around
the world - e.g. WRA Australia, YKA Canada, GBA India,
ESK Scotland, NORSAR Norway - ESSN seismic network of 100 stations in Soviet
Union and eastern block - Late 1970s --- Analogue to digital conversion
begun
31WRA, GBA, YKA Seismic Arrays Constructed in
1960s
Upper mantle (400 and 650 km) discontinuities
detected in the 1960s from analysis of array data
32Further milestones in seismology
- 1966 Keiiti Aki defines seismic moment
- A physical measure of the magnitude of an
earthquake. - Mo Area slip rigidity
- 1969-72 Apollo astronauts place a seismometer
on he Moon, and the first "moonquakes" are
registered. - 1977 Hiroo Kanamori establishes the moment
magnitude scale - A measure of earthquake magnitude based on
seismic moment.
33Plate tectonic theory
341984 The US National Science Foundation and US
Geological Survey provide funding for a new,
digital seismic network, the GSN. to replace the
aging WWSSN. 1996 The International Data Center
is established in Vienna and seismic monitoring
is done through the International Monitoring
System (IMS). The IMS makes use of many stations
of the GSN.
35New developments Passive experiments
36Passive experiments
- EarthScope
- 400 portable 3 component broadband instruments on
a regular grid - 400 portable 3 component short-period and
broadband seismographs and 2000 single channel
high-frequency recorders - Permanent array of broadband 3 component stations
across the country as part of the USGS Advanced
National Seismic System
37- Message From the SSA - April 14, 2006
- The complete archive of BSSA from 1911-2006 is
now available online - In conjunction with our 100th anniversary, SSA
is pleased to announce that all issues of the
Bulletin of the Seismological Society of America
(BSSA) back from Volume 1 Number 1 (March 1911)
are now available (and searchable) on the World
Wide Web through Geoscience World.