In 1960, Hess made his single most important contribution, which is regarded as part of the major advance in geologic science of the 20th century. In a widely circulated report to the
Office of Naval Research, he advanced the theory, now generally accepted, that the Earth's crust moved laterally away from long, volcanically active
oceanic ridges. He only understood his ocean floor profiles across the North Pacific Ocean after
Marie Tharp and
Bruce Heezen (1953,
Lamont Group) discovered the
Great Global Rift, running along the
Mid-Atlantic Ridge.
Seafloor spreading, as the process was later named, helped establish
Alfred Wegener's earlier (but generally dismissed at the time) concept of
continental drift as scientifically respectable. This triggered a revolution in the earth sciences. Hess's report was formally published in his
History of Ocean Basins (1962), which for a time was the single most referenced work in solid-earth
geophysics. Hess was also involved in many other scientific endeavours, including the
Mohole project (1957–1966), an investigation onto the feasibility and techniques of
deep sea drilling. ==Accolades and affiliations==