The Columbia Earth Institute

  Earth Institute News
posted 07/05/01 11:OO AM EST

Marie Tharp
honored with first
Lamont-Doherty Earth Observatory
Heritage Award

PROGRAM and CITATION

 
 

PROGRAM

 Lamont-Doherty Earth Observatory has a distinguished history of scientific discovery. Numerous organizations have honored the achievements of its graduates and scientific staff, but unfortunately the institution which trained and sustained them has not. To correct this omission, the Observatory will bestow the Lamont-Doherty Heritage Award on its graduates or current and past members of the staff whose contributions to their field, and to the Observatory, are deemed exceptional. The first recipient is Marie Tharp.

Welcome
G.M. Purdy
  Director, Lamont-Doherty Earth Observatory

Speakers
Paul J. Fox
  Professor of Geology/Geophysics and Oceanography
  Texas A&M University
William Ryan
  Doherty Senior Research Scientist
  Lamont-Doherty Earth Observatory
G. Leonard Johnson
  Research Scientist
  University of Alaska, Fairbanks
Walter Pitman
  Special Research Scientist
  Lamont-Doherty Earth Observatory

Presentation of Award
G.M. Purdy & Marie Tharp

Heritage Award

CITATION

 Determined, ingenious and visionary, Marie Tharp is a quintessential scientific pioneer. She has trod where none else had before, simultaneously blazing two trails into unexplored territories. As a scientist, she revealed for the first time the previously hidden and unknown seafloor and provided the first maps to guide earth scientists in this new realm. As a woman, she also charted the course, opening up the field of earth science to women and providing a role model for women scientists.

In the early 1950s,Tharp found the first evidence for mid-ocean ridge rift valleys and stood by her finding in the face of long-held, deeply entrenched beliefs that continental drift was scientific heresy. Soon after, with Bruce Heezen and Maurice Ewing, Tharp helped establish the existence of the Earth's most dramatic and fundamental geological feature - the globe-encircling, 40,000-mile-long mid-ocean ridge system.

Over the course of 30 years, in the great tradition of what is now the Lamont-Doherty Earth Observatory, Tharp and Heezen relentlessly and resourcefully gathered the data they needed and dared to tackle a global problem. They systematically and meticulously unshrouded and pieced together the seafloor-sounding by sounding, seamount by seamount, and ocean basin by ocean basin - until they gave us our first visual image of the spectacular seascape that, until then, had remained beyond human purview.

Their maps played a critical role in helping to bring the controversial theory of continental drift into the realm of rational speculation. The borders of the earth's plates beneath the seafloor became apparent and took shape. The mid-ocean ridge system was discovered to be the site of seafloor spreading. And in short order, evidence coalesced around the fundamentally new framework of plate tectonics.

For scientists and lay people alike, Heezen and Tharp's maps revolutionized our understanding of our planet almost as dramatically as Copernicus did centuries before. Their World Ocean Floor Panorama hangs on the walls of offices and hallways throughout all oceanographic institutions - a ubiquitous source of reference and inspiration, and arguably the closest thing earth science has to iconography.

With profound admiration, the Lamont-Doherty Earth Observatory of Columbia University confers upon Marie Tharp its Heritage Award.
 

 

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