Harry Hess was an American geologist who was born in New
York and studied at Yale University as an electrical engineer
but later changed to study geology. He spent two years in
Zimbabwe (then Rhodesia) studying as an exploration geologist
before he continued his studies at Princeton University.
As a graduate student, Hess worked with a number of students
in a submarine gravity study of the West Indies under F.
A. Vening Meinesz. Later he extended these studies into the
Lesser Antilles using naval submarines. In December 1941, as
a U.S. Navy reserve officer, Hess was called to active duty in
New York City and was assigned responsibility for detecting
enemy submarine operation patterns in the North Atlantic,
resulting in the virtual elimination of the submarine threat
within two years. Hess arranged a transfer to the decoy vessel
U.S.S. Big Horn to test the effectiveness of the submarine
detection program; he then remained on sea duty for the rest
of the war. As commanding officer of the transport vessel
U.S.S. Cape Johnson, Hess carefully chose his travel routes to
Pacific Ocean landings on the Marianas, Philippines, and Iwo
Jima, continuously using his ship’s echo sounder. This
unplanned wartime scientific surveying enabled Hess to collect
ocean floor profiles across the North Pacific Ocean,
resulting in the discovery of flat-topped submarine volcanoes,
which he termed “guyots” after the Princeton Geology Building.
Hess contributed greatly to the fields of science, including
geophysics, geodesy, tectonophysics, and mineralogy.
Because of his outstanding achievements, the American Geophysical
Union set up the “Harry H. Hess Medal for outstanding
achievements in research in the constitution and
evolution of Earth and sister planets.”
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