description Harry Hess Overview
Harry Hammond Hess (1906-1969) was an American geologist and Princeton University professor whose work helped explain the movement of the ocean floor. While serving as a United States Navy officer during World War II, he used echo-sounding equipment to investigate submarine features. These observations contributed to his developing account of ocean basins, linking naval surveying with a major question in Earth science. Hess circulated his seafloor-spreading hypothesis before publishing History of Ocean Basins in 1962.
He proposed that new oceanic crust forms along mid-ocean ridges and moves outward, with older crust eventually descending at ocean trenches. This supplied a mechanism essential to the later theory of plate tectonics. Independent paleomagnetic research, including the explanation of ocean-floor magnetic stripes, helped confirm the model. His work marks a connection between field observations and a testable account of continental movement.
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What major geological theory did Harry Hess formulate?
Hess formulated the theory of seafloor spreading in 1960. This theory proposed that new oceanic crust is formed at mid-ocean ridges and spreads outwards, providing the crucial mechanism for continental drift.
Was Harry Hess also involved in World War II?
Yes, he served as an officer in the United States Navy during World War II. He commanded the assault transport USS Cape Johnson and used the ship's sonar to secretly map the ocean floor.
Did Harry Hess win any awards for his geological work?
He was awarded the prestigious Penrose Medal by the Geological Society of America in 1966. His research fundamentally laid the groundwork for the modern theory of plate tectonics.
How did Harry Hess discover guyots (flat-topped mountains)?
While commanding his naval ship in the Pacific, Hess mapped numerous flat-topped underwater mountains, which he named "guyots." He deduced that these were ancient volcanic islands that had their peaks eroded by waves before sinking.
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