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2012 Seafloor Geodesy in Cascadia - William Wilcock - University of ...

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Appendix B: Meet<strong>in</strong>g Agenda <br />

Ocean Sciences Build<strong>in</strong>g Room 425 <br />

Monday, June 11 <br />

Introduction and Motivation <br />

8:30 Meet<strong>in</strong>g Goals <strong>William</strong> <strong>Wilcock</strong> <br />

8:40 The <strong>Cascadia</strong> Subduction Zone – An Introduction * (p. 27) Ray Wells <br />

9:00 Offshore Structure Anne Tréhu <br />

9:20 Known and Unknown Deformation* (p. 28-­‐30) David Schmidt <br />

9:40 Lessons from Tohoku* (p. 31) Ryota H<strong>in</strong>o <br />

10:10 Break <br />

Exist<strong>in</strong>g Infrastructure <br />

10:30 Pacific Northwest Seismic Network Paul Bod<strong>in</strong> <br />

10:40 Pacific Northwest Geodetic Array Tim Melbourne <br />

10:50 Canadian Land Networks Herb Dragert <br />

11:00 <strong>Cascadia</strong> Initiative* (p. 32) Doug Toomey <br />

11:10 Ocean Observatory Initiative Deborah Kelley <br />

11:20 Neptune Canada* (p. 33) Mart<strong>in</strong> Scherwath <br />

11:30 DARTs for tsunami source def<strong>in</strong>ition Vasily Titov <br />

What is Miss<strong>in</strong>g? <br />

11:40 What is miss<strong>in</strong>g from the big picture? Kel<strong>in</strong> Wang <br />

11:50 Discussion <br />

12:30 Lunch <br />

Geodetic techniques <br />

1:30 Acoustic GPS and Rang<strong>in</strong>g* (p. 34-­‐36) David Chadwell <br />

1.45 Geodetic Acoustic Benchmark Beacon Inverted <br />

Echosounder (GABBIES) <br />

Yang Shen <br />

1:55 <strong>Seafloor</strong> Pressure Spahr Webb <br />

2:10 Deformation at Axial Seamount* (p. 37-­‐38) Bill Chadwick <br />

2:25 Pressure, Gravity and Optical Stra<strong>in</strong>* (p. 39-­‐40) Mark Zumberge <br />

2:40 Tilt Measurements* (p. 41) Andrew Newman <br />

2:55 Borehole Hydrological Methods* (p. 42-­‐43) Earl Davis <br />

3:10 <strong>Seafloor</strong> Hydrological Methods Evan Solomon <br />

3:25 Break <br />

3:40 Discussion <strong>of</strong> Geodetic Techniques <br />

25

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