The theory that the Earth's surface is made up of a number of plates that move and interact with each other
Pioneers of Plate Tectonics
Alfred Lothar Wegener
Harry Hammond Hess
Frederick Vine and Drummond Matthews
John Tuzo-Wilson
Dan McKenzie
Plate
A large, rigid section of the Earth's surface
Plate tectonics of the UK
Harry Hammond Hess
Professor of geology at Princeton University (USA)
Interested in the geology of the oceans while serving in the US Navy in World War II
Used sonar (also called echo sounding) to map the ocean floor across the North Pacific
Published 'The History of Ocean Basins' in 1962, outlining a theory that could explain how the continents could actually drift, later known as 'Sea Floor Spreading'
Discovered that the oceans were shallower in the middle and identified the presence of Mid Ocean Ridges
Envisaged that oceans grew from their centres, with molten material (basalt) oozing up from the Earth's mantle along the mid ocean ridges, creating new seafloor which then spread away from the ridge in both directions
Believed that ocean trenches were the locations where ocean floor was destroyed and recycled
Although his theory made sense, Hess knew, like Wegener, that he still needed convincing geophysical evidence to support it