1. Research opportunities using IRIS and other seismic data resources John Taber, Incorporated Research Institutions for Seismology Michael Wysession, Washington University

2. Overview Hands on – Estimating seismic hazard using IRIS Earthquake Browser Discovering a predictive mathematical model Demo – Exploring regional tectonics using focal mechanisms – Recording and analyzing data from an educational or research-grade seismometer – Viewing a set of seismograms from an earthquake – USArray ground motion visualizations – Understanding earthquakes via a simple physical model

3. Estimating seismic hazard Research problem You and your partner have been asked to compare the seismic hazard in two regions to determine which is safer for building a new manufacturing plant. 1.What type of data would you need to collect to make the comparison? 2. How could you express your findings in a quantitative way?

4. Earthquake hazard from a single fault Would like to know How often do the biggest earthquakes occur? When will the next big one occur? Extend earthquake history with geologic record

5. Earthquake recurrence along a single fault Sieh et al., 1989 With a partner: Determine when the next Pallett Creek earthquake is going to occur. Can you estimate the uncertainty in your answer?

6. Earthquake recurrence along a single fault can be highly variable: probabilities hard to assess M >7: mean = 132 yr Standard deviation = 105 yr Estimated probability of next earthquake in 30 yrs is 7-51% -> Nearly Random! Sieh et al., 1989

7. How can we deal with unpredictable nature of individual faults? Try regional approach Use the rate of earthquake occurrence in one time period to forecast earthquake activity in another time period Combine results from multiple faults Consider more than just the biggest earthquakes

8. IRIS Earthquake Browser - www.iris.edu/ieb

9. Can use for introduction to plate tectonics – Explore plate boundaries – Turn plate boundary lines on and off – Interactive 3D viewer General exploration of spatial distribution of local and regional seismicity

10. Estimating seismic hazard Steps: Select a region of the world that is of interest to you Interrogate the earthquake catalog to determine the number of events that occur in a 25 year period – Set the Time Range – Set the Magnitude Range In an Excel spreadsheet, record the total number of events for each magnitude range Determine the number of earthquakes/year for each magnitude range Plot the magnitude range vs the number of earthquakes/year

11. IRIS Earthquake Browser - www.iris.edu/ieb

12. Questions to discuss with a partner Given the range of the data, what sort of plot gives the clearest representation of the data? Do you see any patterns or trends in your data? How does your plot compare to your partner’s plot of a different region? What is the likelihood of earthquakes of magnitude 6.0 or greater and 7.0 or greater occurring in the next year in the 2 regions? What is the likelihood of these events occurring in the next 100 years in each region?

13. Earthquakes, Magnitude >3.5, 1973-2007

16. Earthquakes/year Magnitude California (blue) and Eastern US Earthquakes (red)

18. How often does a M6 earthquake occur?

19. How often does a M7 earthquake occur?

20. Real, imperfect data set

21. Interpretation questions How can you use the seismicity information to estimate which of your two regions would be a safer choice for the manufacturing plant mentioned at the beginning of the exercise? What are some assumptions, limitations, and potential sources of error in drawing conclusions about long-term seismic hazard using the above technique?

22. http://pasadena.wr.usgs.gov/office/hough/east-vs-west.jpg Ground shaking from a magnitude 5 earthquake in the east is approximately equivalent to that of a magnitude 6 earthquake in the west. Virginia M 5.8 California 6.5 Going from seismicity rate to ground shaking

23. USGS National Seismic Hazard Map Submitted draft exercise explores hazard map

24. Exploring regional tectonics using f o c a l m e c h a n i s m s Visual sorting of normal, reverse, and strike-slip mechanisms Can explore distribution in a subduction zone IRIS main menu: Data and Software > Products – Select Moment Tensors, then Quick links – http://www.iris.edu/spud/momenttensor Focal mechanism animation available

25. Recording and analyzing seismic data u s i n g j A m a s e i s Real time data streaming and simple analysis – Simple filtering, arrival picking, locations, magnitudes

26. Recording and analyzing seismic data u s i n g j A m a s e i s Real time data streaming and simple analysis – Simple filtering, arrival picking, locations, magnitudes Up to 3 data streams can be viewed and stored locally – Local or remote educational seismographs – Any global research station received and stored in the IRIS Data Management Center

27. Recordings from the Global Seismic Network Real time data streaming and simple analysis

28. Potential seismograph-related research t o p i c s Local seismograph calibration and sensitivity – Distance/magnitude relationship Alan Kafka – Analyzing seismic data to find what earthquakes were recorded and then learning about the tectonics of each region Dave Voorhees’ student – Finding the best recording location

29. Rapid E a r t h q u a k e V i e w e r Developed and maintained by Univ S. Carolina

30. Understanding earthquakes via a simple p h y s i c a l m o d e l Earthquake machine Simple data collection and analysis leads to very similar result to real earthquake catalog

31. USArray Ground Motion Visualizations Visualizations exist for all parts of lower 48 1D and 3D versions

32. EPO web p a g e f r o m w w w. i r i s. e d u Feedback? Comments? Questions?

33. EXTRAS

34. USArray Ground Motion Visualizations Visualizations exist for all parts of lower 48

35. Investigating Earth structure using t o m o g r a p h i c m o d e l s Select a region and a submitted velocity model and generate a cross section Fate of slabs Crustal and upper mantle thickness under mountain ranges

36. Selection from focal mechanism animation