Time-independent hazard-random process in time: used for building design, planning, insurance, probability - PowerPoint PPT Presentation

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Time-independent hazard-random process in time: used for building design, planning, insurance, probability

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Recurrence Interval Paleoseismology and recurrence interval Pallet Creek offset 1857 1745: 112 years 1470: 275 years 1245: 225 years 1190: 55 years 965: ... – PowerPoint PPT presentation

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Title: Time-independent hazard-random process in time: used for building design, planning, insurance, probability


1
The Idea of Earthquake Prediction
  • Time-independent hazard-random process in time
    used for building design, planning, insurance,
    probability
  • Time-dependent hazard-a degree of predictability,
    enable authorities to prepare for an event-false
    alarms- loss of public confidence, China- shut
    down of public services during false alarms

2
Earthquake Predictions
  • The 1960s- descriptions of physical changes
  • 1970s- 1975, successful prediction 1976,
    250,000- people died in Tangshen, China
  • 1980s- Jim Berkland, fluctuations of missing dogs
    in local newspapers, increase number of calls to
    satellite TV companies
  • Greek scientists, electrical signals

3
Haichen, China, 1975
  • An evacuation warning was issued the day before
  • The local rural population was educated and aided
    in the monitoring
  • changes in land elevation and ground water
  • reports of peculiar animal behavior- snakes
    coming out of the ground in January, livestock
    not going into their barns
  • an increase in small earthquakes

4
The Idea of Earthquake Prediction or Forecasting
  • 1977- National Earthquake Hazards Reduction
    Program (NEHRP)
  • 1. Precursor detection instruments at the site
  • 2. Detect and recognize precursors
  • 3. Get colleagues to agree, accept and put out a
    warning

5
Earthquake Forecasts
  • Earthquake forecasting- some connection between
    the level of chance between observation and
    event probabilities and errors involved
  • Scientists cannot predict earthquakes
  • Evacuation before an event since 1975 has not
    occurred

6
Long-term Forecasts
  • Retrofitting
  • Building codes
  • Legislation
  • Insurance
  • Emergency plans
  • Education to the public
  • Preparedness

7
Long-term Forecasting Methods
8
Paleoseismicity
  • Identify fault trace
  • Trench
  • Analyze sedimentary layers and offsets
  • Date organic material

9
Historical Seismicity Patterns
  • Large Bay Area earthquakes are more frequent at
    some times more than others
  • 1836-1911 1911-1979 (68 years of no events)

10
Recurrence Interval
  • Statistical Method of historic earthquakes
  • Shortest interval
  • Longest interval
  • Average 25.5 years
  • Problems with this method?
  • Parkfield Seismic Area
  • 1988-90 probability for a M6 earthquake
  • 1901
  • 1922 21 years
  • 1934 12 years
  • 1966 32 years
  • 2004 38 years

11
Paleoseismology and recurrence interval
  • Shortest interval?
  • Longest interval?
  • Average?
  • 187 years
  • Strengths of this method
  • Shortcomings?
  • Pallet Creek offset
  • 1857
  • 1745 112 years
  • 1470 275 years
  • 1245 225 years
  • 1190 55 years
  • 965 225 years
  • 865 100 years
  • 545 320 years

12
Seismic Gaps -areas on a larger fault system that
lack seismicity
13
Variation of average movement on known faults
  • Bay Area faults belong to the San Andreas fault
    system
  • Movement varies
  • Right-lateral strike-slip faults
  • 1868- Hayward fault
  • 1906-San Andreas fault
  • 1989-San Andreas fault

14
Variation of average movement on known faults
  • Bay Area faults move at different rates to
    accommodate the total amount of slip of the San
    Andreas fault system
  • Total 34 mm/year
  • SAF 19 mm/yr
  • Hayward fault 9 mm/yr

15
Earthquake Prediction and Probability
Variation of average movement on known faults
  • Each vector represents the amount of movement on
    each fault
  • Variations may indicate an imminent earthquake

16
Pattern of Seismicity
17
Earthquake Forecasting and Probability
  • Working Group on California Earthquake
    Probabilities
  • Group of 100 geologists, engineers, government
    officials evaluated all information
  • Came up with a probability of a magnitude 7 or
    greater in the next 30 years
  • 1988. 1999, 2003, 2008

18
Earthquake Forecasting and Probability
  • Assumes a random distribution of earthquakes
  • In the Bay Area, 5 earthquakes greater or equal
    to M 6.75 occur approximately every 30 years
  • 50 probability-just as likely to happen as not
    to happen

19
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20
The Idea of Earthquake Forecasting
  • Loma Prieta- 30 probability in 1988- eq, 1989
  • Parkfield -90 probability in 1988-eq, 2004
  • Landers, Northridge, Kobe- earthquake on a little
    known fault

21
Short-term Prediction based on precursors
22
All the described precursors sometimes occur but
as of yet do not occur in a manner that
successfully predict earthquakes
23
What should be expected?
  • A reasonable time period
  • The location- fault or fault segment
  • Magnitude or amount of energy released

24
Ground Deformations
  • Ground deformation
  • Preceding the 1906 earthquake in Marin
    County-elastic rebound theory
  • The Palmdale bulge- monitoring began in the
    1960s , associated with the SAF

25
Radon Gas Emissions
  • Radon emission- a radioactive gas that sometimes
    shows an increase preceding an earthquake-
  • There was a ten-fold increase 30 kilometers away
    from the epicenter 9 days preceding the
    earthquake.
  • Problem with this method?

26
Parkfield Experiment
  • Examining precursors or those events that
    sometimes occur before a main event
  • Changes in physical properties in close proximity
    to the fault

27
Parkfield experiment
  • Magnitude 6 earthquake occurred on average every
    22 years from 1857-2004
  • Similar location
  • Similar seismic wave pattern recorded

Hopes of documenting an earthquake before,
during, and after the main shock in order to
produce a short-term prediction technique.
28
Precursors expected to observe
  • Foreshocks
  • Ground deformation

Surface cracks associated with the 2004 earthquake
29
San Andreas Fault Observatory at Depth 2004
Examining physical changes to the rocks at depth
30
Animal Prediction
  • Unusual animal behavior prior to a disaster
  • Greece, 373 BC, rats, snakes and weasels deserted
    days before an earthquake
  • Advanced vibrations?
  • Change in electrical charges?
  • Change in magnetic field?
  • So far, unable to use unusual animal behavior to
    predict earthquakes

31
Chi Chi Earthquke,Taiwan, 1999
  • Initial smaller earthquake during the first 4
    seconds have higher frequency waves than larger
    earthquake
  • The warning could be sent
  • Seismic waves travel at about 2 miles per second

32
Early Warning System
  • Detect P-wave arrival
  • Warning system
  • Emergency centers, hospitals, railways
  • Depends on distance to how helpful
  • Japan-March , 2011, M9, Tokyo-stopped trains
    cell phone notification 8-10 minutes tsunami
  • Kobe-fault under city
  • Mexico-11 warnings, M6 or greater

33
Early Warning System U.S.
  • 80 dollars over 5 years
  • Arrival of P-waves
  • 3-4 minutes Cascadia Subduction Zone
  • 1 minute warning for SAF
  • 30 seconds
  • doctors stop surgery
  • Duck and cover
  • Trains stop
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