1. IRIS Data Tools and Animations John Taber, Tammy Bravo, Michael Hubenthal, Jenda Johnson

2. Outline Seismicity Teachable Moments Animations Seismogram viewer Prepackaged record sections (SPUD) Seismogram retrieval (Web services)

4. IRIS Earthquake Browser www.iris.edu/ieb Explore global, regional, and local seismicity Both recent and historic events Easy to use and based on Google maps

5. Regional Seismicity

6. Explore Plate Boundaries

7. Exploring Forecasting & Prediction

8. Export Data

9. Teachable Moment slide sets Newsworthy earthquakes motivate students to learn more about seismology Wide range of online resources available but college faculty and teachers have little time to prepare Slide sets produced within 1 day –Most content from other groups, particularly USGS –Try to tell a story –In English and Spanish

10. This earthquake occurred at the boundary between the Nazca and South American tectonic plates. The two plates are converging at a rate of 80 mm per year. The earthquake occurred as thrust-faulting on the interface between the two plates, with the Nazca plate moving down and landward below the South American plate. The tension axis (T) reflects the minimum compressive stress direction. The pressure axis (P) reflects the maximum compressive stress direction. USGS Centroid Moment Tensor Solution Simplified diagram of thrust faulting during a subduction zone earthquake. The sudden motion along the fault displaces massive volumes of seawater creating a tsunami. (© 1999 Zeke Smith) Magnitude 8.8 OFFSHORE MAULE, CHILE Saturday, February 27, 2010 at 06:34:17 UTC Images courtesy of the U.S. Geological Survey

11. Although magnitude is still an important measure of the size of an earthquake, particularly for public consumption, seismic moment is a more physically meaningful measure of earthquake size. Seismic moment is proportional to the product of the slip on the fault and the area of the fault that slips. These “maps” of the slip on the fault surfaces of the January 12th M7.0 Haitian earthquake and the M8.8 Chilean earthquake show that, although the slip in Chile was only about 50% greater, the fault area was vastly larger. This accounts for the release of approximately 500 times more energy in the Chilean earthquake than in the Haiti earthquake. Chile Haiti Magnitude 8.8 OFFSHORE MAULE, CHILE Saturday, February 27, 2010 at 06:34:17 UTC Images courtesy of the U.S. Geological Survey

12. NZ eq animation

13. Animations Over 40 animations available online –Created by Jenda Johnson Illustrating concepts related to plate tectonics, earth structure, earthquakes, and volcanoes Includes background information and teaching sequences using multiple animations Linked to activities and Teachable Moments http://www.iris.edu/hq/programs/education_and_outreach/anim ations

15. Based on Tom Boyd wave front movie

18. Student sequence www.iris.edu/explore

20. Prepackaged Record Sections from the Data Management Center

21. Data at www.iris.edu/spud Description at www.iris.edu/ dms/products/eventplot

24. Web services www.iris.edu/ws/timeseries/builder

25. Viewing and Analysis Tools Existing –SAC –Matlab –New jAmaseis –Under development by Moravian College Seismic Canvas –Glenn Kroeger

26. jAmaseis