Title: Time-independent hazard-random process in time: used for building design, planning, insurance, probability
1The 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
2Earthquake 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
3Haichen, 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
4The 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
6Long-term Forecasts
- Retrofitting
- Building codes
- Legislation
- Insurance
- Emergency plans
- Education to the public
- Preparedness
7Long-term Forecasting Methods
8Paleoseismicity
- Identify fault trace
- Trench
- Analyze sedimentary layers and offsets
- Date organic material
9Historical Seismicity Patterns
- Large Bay Area earthquakes are more frequent at
some times more than others - 1836-1911 1911-1979 (68 years of no events)
10Recurrence 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
11Paleoseismology 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
12Seismic Gaps -areas on a larger fault system that
lack seismicity
13Variation 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
14Variation 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
15Earthquake 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
16Pattern of Seismicity
17Earthquake 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
18Earthquake 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
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20The 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
21Short-term Prediction based on precursors
22All the described precursors sometimes occur but
as of yet do not occur in a manner that
successfully predict earthquakes
23What should be expected?
- A reasonable time period
- The location- fault or fault segment
- Magnitude or amount of energy released
24Ground 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
25Radon 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?
26Parkfield Experiment
- Examining precursors or those events that
sometimes occur before a main event - Changes in physical properties in close proximity
to the fault
27Parkfield 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.
28Precursors expected to observe
- Foreshocks
- Ground deformation
Surface cracks associated with the 2004 earthquake
29San Andreas Fault Observatory at Depth 2004
Examining physical changes to the rocks at depth
30Animal 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
31Chi 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
32Early 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
33Early 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