Alfred Edward Ted Ringwood was an Australian experimental geophysicist and geochemist born April 19, 1930, in Kew, Melbourne, Australia, who died November 12, 1993, and who worked at the Australian National University. He discovered that germanates functioned as a low pressure analogue to high pressure silicates, allowing predictions about mantle mineral phase changes, demonstrated in 1959 that iron olivine transforms to a denser spinel structure, synthesized the spinel form of magnesium iron silicate in 1966, and in 1978 his team invented synroc, a synthetic rock technology for radioactive waste disposal; the mineral ringwoodite, discovered in the Tenham meteorite in 1969, is named for his predicted high pressure polymorph of olivine. He was elected a Fellow of the Royal Society in 1972, received the William Bowie Medal in 1974, the Mueller Medal in 1975, the Wollaston Medal in 1988, the V. M. Goldschmidt Award in 1991, and the Clarke Medal in 1992.
Facts
FieldGeochemistry, petrology, planetology 1 Notable WorkPredicted high pressure olivine polymorph, the mineral ringwoodite is named after him 1 BirthplaceKew, Melbourne, Australia 1 In the Other Atlases
- Also in Geography Atlas: Australia, nationality there.
Sources
1. Ted Ringwood, Wikipedia
Infobox, Born date
19 April 1930
Infobox, Born place
Kew, Melbourne, Australia
Later life
Ringwood died of lymphoma on 12 November 1993
Opening paragraph, description
Australian experimental geophysicist and geochemist
Infobox, Fields
Geochemistry, petrology, planetology
Opening paragraph, mineral
The mineral ringwoodite is named after him.
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