John Tuzo Wilson
John Tuzo Wilson CC OBE FRS FRSE FRSC (October 24, 1908 – April 15, 1993) was a Canadian geophysicist and geologist who achieved worldwide acclaim for his contributions to the theory of plate tectonics.
John 'Jock' Tuzo Wilson
October 24, 1908
April 15, 1993 (aged 84)
Theory of Plate tectonics
- Officer, Order of Canada
- Companion, Order of Canada
- Fellow, Royal Society of Canada
- Fellow, Royal Society of London[1]
- Fellow, Royal Society of Edinburgh
- Legion of Merit
- Order of the British Empire
- Maurice Ewing Medal, AGU
- Maurice Ewing Medal, SEG
- Bucher Medal, SEG
- Penrose Medal, GSA
- Wegener Medal, EUG
- Wollaston Medal, Geological Society
- Vetlesen Prize, Columbia University
- Canada Centennial Medal
- 125th Anniversary Medal (Canada)
John J. Carty Award (1975)
William Taylor Thom, Jr
Plate tectonics is the scientific theory that the rigid outer layers of the Earth (crust and part of the upper mantle), the lithosphere, is broken up into around 13 pieces or "plates" that move independently over the weaker asthenosphere. Wilson maintained that the Hawaiian Islands were formed as a tectonic plate (extending across much of the Pacific Ocean) shifted to the northwest over a fixed hotspot, spawning a long series of volcanoes. He also conceived of the transform fault, a major plate boundary where two plates move past each other horizontally (e.g., the San Andreas Fault).
His name was given to two young Canadian submarine volcanoes called the Tuzo Wilson Seamounts.[3] The Wilson cycle of seabed expansion and contraction (associated with the Supercontinent cycle) bears his name. One of the two large low-shear-velocity provinces was given the name Tuzo after him, the other being named Jason after W. Jason Morgan, who furthered Wilson's work into plume theory.
Early life and education[edit]
Wilson was born in Ottawa on October 24, 1908, the son of John Armistead Wilson CBE, and his wife, Henrietta Tuzo.[4] Wilson's father was of Scottish descent and his mother was a third-generation Canadian of French descent.
He became one of the first people in Canada to receive a degree in geophysics, graduating from Trinity College at the University of Toronto in 1930.[5] He obtained a second (BA) degree from St. John's College, Cambridge in 1932 and then a doctorate (ScD). He then pursued further graduate studies as Princeton University, where he received a Ph.D. in geology in 1936 after completing a doctoral dissertation titled "The Geology of the Mill creek - Stillwater Area, Montana."[6]
Career[edit]
In 1936, Wilson joined the Geological Survey of Canada as a government geologist. This was interrupted by the Second World War during which he served with the Royal Canadian Engineers, serving in Europe and reaching the rank of Colonel. He was involved in Operation Musk Ox.[7] For his wartime service, he was appointed an OBE.
In 1946 he was appointed the first Professor of Geophysics at the University of Toronto.
He made significant contributions to the theory of Plate tectonics, adding a concept of hot spots. Plate tectonics is the scientific theory that the rigid outer layers of the Earth (crust and part of the upper mantle), the lithosphere, is broken up into around 13 pieces or "plates" that move independently over the weaker asthenosphere. Wilson maintained that the Hawaiian Islands were created as a tectonic plate (extending across much of the Pacific Ocean) shifted to the northwest over a fixed hotspot, spawning a long series of volcanoes. He also conceived of the transform fault, a major plate boundary where two plates move past each other horizontally (e.g., the San Andreas Fault).
The Wilson cycle of seabed expansion and contraction (associated with the Supercontinent cycle) bears his name, in recognition of his iconic observation that the present-day Atlantic Ocean appears along a former suture zone[8] and his development in a classic 1968 paper[9] of what was later named the "Wilson cycle" in 1975 by Kevin C. A. Burke, a colleague and friend of Wilson.[10]
His name was given to two young Canadian submarine volcanoes called the Tuzo Wilson Seamounts.[11]
Wilson was president (1957–1960) of the International Union of Geodesy and Geophysics (IUGG).
In 1967 he became principal of Erindale College, now known as University of Toronto Mississauga. In 1974 he left to become the Director General of the Ontario Science Centre. In 1983 he became Chancellor of York University, Toronto.
He was the host of the television series The Planet of Man.
Honours and awards[edit]
For his service during the Second World War, Wilson was appointed an Officer of the Order of the British Empire in 1946. In 1969, he was made an Officer of the Order of Canada and was promoted to the rank of Companion of that order in 1974.[12] He was elected to the American Academy of Arts and Sciences in 1971 and the American Philosophical Society in 1971.[13][14] Wilson was awarded the John J. Carty Award from the National Academy of Sciences, of which he was already a member, in 1975.[15][16] In 1978, he was awarded the Wollaston Medal of the Geological Society of London and a Gold Medal by the Royal Canadian Geographical Society. He also served as honorary vice president of the RCGS.[17] He was a Fellow of the Royal Society, the Royal Society of Canada, and of the Royal Society of Edinburgh.[18]
He was elected president-elect (1978–1980) and president (1980–1982) of the American Geophysical Union.
He also served as the director general of the Ontario Science Centre from 1974 to 1985.
Wilson and his plate tectonic theory are commemorated on the grounds of the Centre by a giant "immovable" spike that records the amount of plate movement since Wilson's birth.
The J. Tuzo Wilson Medal of the Canadian Geophysical Union recognizes achievements in geophysics. He is also commemorated by a named memorial professorship and an eponymous annual public lecture delivered at the University of Toronto.
He is one of the 2016 inductees into Legends Row: Mississauga Walk of Fame.[19]
Personal life[edit]
Photography[edit]
Wilson was an avid traveller and took a large number of photographs during his travels to many destinations, including European countries, parts of the then USSR, China, the southern Pacific, Africa, and to both polar regions. Although many of his photos are geological—details of rocks and their structures or panoramas of large formations—the bulk of his photos are of the places, activities and people that he saw on his travels: landscapes, city views, monuments, sites, instruments, vehicles, flora and fauna, occupations and people.