Can we forecast an Earthquake??? In the next minute there will be an earthquake somewhere in the world! This sentence is correct (we have seen that there.

Slides:



Advertisements
Similar presentations
Earthquake Prediction Methods. Earthquake predictions  Because earthquakes do not happen on regular intervals it is difficult to predict when the next.
Advertisements

Active Folding within the L.A. Basin with a focus on: Argus et al. (2005), Interseismic strain accumulation and anthropogenic motion in metropolitan Los.
16/9/2011UCERF3 / EQ Simulators Workshop RSQSim Jim Dieterich Keith Richards-Dinger UC Riverside Funding: USGS NEHRP SCEC.
Recurrence Intervals Frequency – Average time between past seismic events – aka “recurrence interval” Recurrence Interval = Average slip per major rupture.
Size of earthquakes. MODIFIED MERCALLI SCALE Defines the INTENSITY of an earthquake by the amount of damage caused.
Test 2 mean: 75, median: 79 multiple choice: 42 questions, 2 points each short answer: 4 questions, 4 points each 100 total: circled number inside front.
Ch 3: Characterization of the SFBR Earthquake Sources Working Group on California Earthquake Probabilities, 2002.
Larry Braile AS-1 Workshop, September, 2008 San Francisco Bay Area Earthquake Ground Motion Simulations
Earthquake Predictibility, Forcasting and Early Warning Bill Menke October 18, 2005.
Using Geodetic Rates in Seismic Hazard Mapping March 30, Geodetic and Geologic slip rate estimates for earthquake hazard assessment in Southern California.
SCEC Annual Meeting - ITR 09/17/021 Numerical Modeling Using Finite Difference Techniques.
Earthquakes-Pt.2 Earthquake Processes (mechanisms/causes) Effects of earthquakes (damage) Earthquake risk and prediction Responses to earthquake hazards.
TOPIC 2: How does the challenge of predicting hazards differ between earthquakes - at plate boundaries -In plate boundary zones -within plates?
Small Scale Precursors to Earthquakes Predicting EQs by magnetic field variations.
Earthquake Prediction Methods By Jason Long. Outline Background Statistical Methods Physical and Geophysical measurements and observations Conclusion.
Kenneth W. Hudnut U. S. Geological Survey Pasadena, California Southern California Earthquake Center --- Workshop on Tectonophysics of Southern California.
The Empirical Model Karen Felzer USGS Pasadena. A low modern/historical seismicity rate has long been recognized in the San Francisco Bay Area Stein 1999.
Earthquake potential of the San Andreas and North Anatolian Fault Zones: A comparative look M. B. Sørensen Department of Earth Science, University of Bergen,
2007 NSTA: St. Louis, Missouri Earthquake Prediction and Forecasting: A Case Study of the San Andreas and New Madrid Faults Sponsored by: IRIS (Incorporated.
Forecasting Earthquakes ・ Difference between Predictions and Forecasts ・ Earlier Efforts in Earthquake Prediction ・ Long-term Probability Estimates.
Earthquake Predictions & Tectonic Environments
Paleoseismic and Geologic Data for Earthquake Simulations Lisa B. Grant and Miryha M. Gould.
Section 10.3 pg. 222 Earthquake Hazards.
Time-independent hazard-random process in time: used for building design, planning, insurance, probability Time-dependent hazard-a degree of predictability,
Chapter 5 EARTHQUAKES and ENVIRONMENT. Earthquakes Violent ground-shaking phenomenon by the sudden release of strain energy stored in rocks One of the.
Earthquakes A Whole Lot of shakin’ going on!. What are Earthquakes and where do they occur? Seismology is the study of earthquakes. Seismology is the.
Earthquakes Source: NPS Source: USGS.
Thailand Training Program in Seismology and Tsunami Warnings, May 2006 Forecasting Earthquakes.
The specification notes that you must be able to describe methods of earthquake prediction. You must also understand the social consequences of earthquake.
Earthquakes Most destructive forces on Earth. But it is buildings and other human structures that cause injury and death, not the earthquake itself 1988.
Class lectures available
The next big earthquake at SFO (coming soon) Tom Brocher USGS, Coordinator, NC Earthquake Hazard Investigations M Hayward.
Lisa Wald USGS Pasadena U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program Earthquakes 101 (EQ101)
Before you jump into this slide show, you should view the Presentation on EarthquakeSeismology See notes for link.
Kenneth W. Hudnut USGS, Pasadena, CA West Newport Beach Association Public Forum, Newport Beach City Hall March 5, 2003 Coping with ‘quakes.
Earthquake Science (Seismology). Seismometers and seismic networks Seismometers and seismic networks Earthquake aftershocks Earthquake aftershocks Earthquake.
National Seismic Hazard Maps and Uniform California Earthquake Rupture Forecast 1.0 National Seismic Hazard Mapping Project (Golden, CO) California Geological.
In the past ~15 years we’ve learned a lot and have new questions: Paleoseismology shows that continental intraplate seismicity often migrates, is episodic,
A functional form for the spatial distribution of aftershocks Karen Felzer USGS Pasadena.
U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program Earthquakes 101.
Earthquake forecasting using earthquake catalogs.
Scientific Drilling Into the San Andreas Fault zone San Andreas Fault Observatory at Depth (SAFOD)
Earthquake Predictability Test of the Load/Unload Response Ratio Method Yuehua Zeng, USGS Golden Office Zheng-Kang Shen, Dept of Earth & Space Sciences,
Faults and Earthquakes. Some faults become “locked” –Pressure pushes together the irregular walls of the fault; surfaces resist sliding Slip can’t occur.
PREDICTION Paleoseismology: Documenting and evaluating past events. 1.) Usually done with looking at offset layers in sediments in trenches 2.) Calculate.
U.S. Department of the Interior U.S. Geological Survey The Earthquake is Inevitable: The Disaster is Not.
Correlating aftershock sequences properties to earthquake physics J. Woessner S.Wiemer, S.Toda.
06/22/041 Data-Gathering Systems IRIS Stanford/ USGS UNAVCO JPL/UCSD Data Management Organizations PI’s, Groups, Centers, etc. Publications, Presentations,
Forecasting Earthquakes
112/16/2010AGU Annual Fall Meeting - NG44a-08 Terry Tullis Michael Barall Steve Ward John Rundle Don Turcotte Louise Kellogg Burak Yikilmaz Eric Heien.
Forecasting Earthquakes ・ Difference between Predictions and Forecasts ・ Earlier Efforts in Earthquake Prediction ・ Long-term Probability Estimates.
Earthquakes 101 (EQ101) Lisa Wald USGS Earthquake Hazards Program
Earthquakes and crustal Deformation - Objectives of class- Introduce a variety of techniques to describe ‘quantitatively’ deformation of the lithosphere.
Objectives Relate earthquake activity to plate tectonics Define earthquake, and identify the focus and epicenter of an earthquake. Describe the types.
J. Havskov Recent large earthquakes, including Haiti 2010, could they have been predicted ?
Earthquakes.
BREVIA Time-Variable Deformation in the New Madrid Seismic Zone Eric Calais 1 and Seth Stein 2 velocities relative to the rigid interior ofNorth Amer-
Geologic Hazards Geologic Hazards are those Earth processes that are harmful to humans and/or their property. Includes: Earthquakes Volcanic eruptions.
Earthquakes USGS Earthquake Hazards Program Earthquake Basics
Earthquakes.
Velocities in ITRF – not appropriate for interpretation
Kinematic Modeling of the Denali Earthquake
SAN ANDREAS FAULT San Francisco Bay Area North American plate
EARTHQUAKE EFFECTS, PATTERNS, AND RISK
San Andreas Fault Zone Mr. Kleinschrodt.
VII. Earthquake Mitigation
Dealing With Earthquakes
Frequency, regularity and predictability of earthquake hazard events
Presentation transcript:

Can we forecast an Earthquake??? In the next minute there will be an earthquake somewhere in the world! This sentence is correct (we have seen that there is at least 150 earthquake of magnitude every hour!) but quite useless.

Long vs Short Term forecast Long term: Geological observation: Paleoseismology Mapping Faults Seismic Gaps Geodesy Geophysics: Earthquake processing Stress propagation Earthquake Simulations SEISMIC HAZARDS MAPS Short term Foreshocks Animal Behavior Rock Conductivity Rock Seismic Velocity Water Level Gas Emission (Radon) EVACUATION

Problems with Short Term Every earthquake seems to behave in a different way and in general we make the observations only after the event. The only real forecast with evacuations happen in February 1975 in China (Haicheng) but none of the observed sign of the 1975 event were visible next year in TangShan (China) when an earthquake killed people. The recurrence time is too long to test our models

Haicheng earthquake

Seismic Gap (1) USGS, 1989

Seismic Gaps (2) From Brumbagugh, 1999

The SCEC 3.0 velocity field

Velocity and velocity gradient of all segments

Maximum horizontal shear

Relation between seismicity and interseismic deformation

Historical Major Earthquakes 1857Fort Tejon San Francisco Imperial Valley Loma Prieta Landers Northridge Hector Mine7.2 The BIG Ones

Timeline years Recurrence Intervals 150 years40 years24 years 210 years 400 years Average time between major earthquake events on a fault segment Short recurrence intervals are identified along faults of high stress accumulation rate 400 Imperial Parkfield Mojave Santa Cruz Peninsula Calaveras Concord more repeating earthquakes

Paleoseismic

Current motion in the Aegean-Caucuses (with respect to Eurasia) McClusky et al. (2000)

Stain et al, 1997 Anatolian Fault

Hazards Maps

City Planning Schools From Brumbagugh, 1999

Education