October 8, 2009
at Lamont Doherty Earth Observatory


Columbia Climate School
Senior Advisor to the Co-Deans
Lamont-Doherty Earth Observatory
Higgins Professor Emeritus
Other Speakers
Dr. Maya Tolstoy, Doherty Research Scientist, Lamont -Doherty Earth Observatory

"Subduction zones are where oceanic crust or continental crust dives back down into the mantle. And it was discovered in the ‘60s again at Lamont principally by Lynn Sykes that deep earthquakes were associated with the slab as we call it going down into the mantle. "
-Art Lerner Lam