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LIVE INTERACTIVE YOUR DESKTOP Tuesday, January 29, 2008 NSDL/NSTA Web Seminar: Earth in Reverse: Magnetic Wiggles on the Ocean Floor.

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Presentation on theme: "LIVE INTERACTIVE YOUR DESKTOP Tuesday, January 29, 2008 NSDL/NSTA Web Seminar: Earth in Reverse: Magnetic Wiggles on the Ocean Floor."— Presentation transcript:

1 LIVE INTERACTIVE LEARNING @ YOUR DESKTOP Tuesday, January 29, 2008 NSDL/NSTA Web Seminar: Earth in Reverse: Magnetic Wiggles on the Ocean Floor

2 Dr. Anthony Koppers, Associate Professor of Marine Geology and Geophysics at Oregon State University Today’s NSDL Experts http://nsdl.org Dr. Chris Massell Symons, Researcher at the Scripps Institution of Oceanography http://earthref.org/ERESE

3 How did we get from “blue” oceans to such great detail? Magnetic Wiggles!!! http://nsdl.org

4 Earth’s Magnetic Field http://nsdl.org

5 BUT…..Magnetic North is NOT at the North Pole http://nsdl.org

6 AND…the Magnetic Field Reverses Field reverses ~1 time every 200,000 years on average. 400 times in last 330 million years. Last reversal was 780,000 years ago. NORMALREVERSE

7 Poll Question! On average, how long does each magnetic reversal take to complete? A. 10,000 years B. 5,000 years C. 1,000 years D. 100 years http://nsdl.org

8 Let’s pause for two questions from the audience…. http://nsdl.org

9 Recording the Magnetic signature MID-OCEAN RIDGE REVERSE NORMAL http://nsdl.org

10 Sampling the Seafloor http://nsdl.org

11 Early Maps of Seafloor Anomalies ICELAND Mid-Atlantic Ridge Heirtzler et al., 1966 Raff and Mason, 1961 http://nsdl.org

12 Sample Profiles across Mid-Ocean Ridges http://nsdl.org

13 Changing Spreading Rate = Modified Wiggle Pattern http://nsdl.org

14 Shipboard Magnetic Data Across the EPR MEXICO PROFILE 2 PROFILE 1 http://nsdl.org

15 MODEL PROFILE 2 Using the marker, identify the location of the spreading ridge on PROFILE 2. http://nsdl.org East Pacific Rise

16 MODEL PROFILE 2 Solution - Matching Peaks 11 2 33 2 http://nsdl.org

17 50 km/my100 km/my125 km/my How fast is the East Pacific rise spreading? http://nsdl.org

18 Mid-Atlantic Spreading Ridge ICELAND GREENLAND http://nsdl.org

19 Data across Reykjanes Ridge http://nsdl.org

20 What is the average spreading rate at the Reykjanes Ridge over the last 10 million years? North American PlateEurasian Plate 1 km/my5 km/my10 km/my Stamp One:

21 Let’s pause for two questions from the audience…. http://nsdl.org

22 How old are the wiggles? http://nsdl.org

23 Time Scale http://nsdl.org

24 Age of the Earth~ 4.6 Billion Years Oldest Rock ~ 3.5 Billion Years Oldest Mineral ~ 3.0 Billions Years Oldest Seafloor ~ xxx ??? http://nsdl.org

25 Seafloor Age Map http://nsdl.org

26 Dating OLDEST Seafloor http://nsdl.org

27 Ocean Drilling Program 1983-2003 http://www.odplegacy.org/ http://nsdl.org

28 From seafloor to analysis to storage….. http://nsdl.org

29 Argon-40/Argon-39 Dating http://nsdl.org

30 Blue = North Orange = South Why does the Earth’s magnetic field reverse? WHEN will be the next reversal? Unsolved Mysteries http://nsdl.org

31 THANK YOU! Dr. Chris Massell Symons csymons@ucsd.edu Dr. Anthony Koppers akoppers@coas.oregonstate.edu http://nsdl.org http://earthref.org/ERESE

32 Download our Seminar Resource List Utilize our blog featuring our presenters for the Fall Series sharing their insights on careers in science and science education: http://expertvoices.nsdl.org/2007fall-nsta-sems/ Go to http://nsdl.org and click on the K-12 audience page to:http://nsdl.org

33 http://learningcenter.nsta.org NLC screenshot

34 National Science Teachers Association Gerry Wheeler, Executive Director Frank Owens, Associate Executive Director Conferences and Programs Al Byers, Assistant Executive Director e-Learning LIVE INTERACTIVE LEARNING @ YOUR DESKTOP NSTA Web Seminars Flavio Mendez, Director Danielle Troiano, Project Coordinator Jeff Layman, Technical Coordinator


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