Edward C. T. Chao
| Edward C.T. Chao | |
|---|---|
| Born |
30 November 1919 Suzhou, China |
| Died |
February 3, 2008 (aged 88) Fairfax, Virginia |
| Fields | Geology |
| Institutions | U.S. Geological Survey |
| Alma mater | University of Chicago |
| Known for | impact metamorphism |
| Notable awards | Barringer Medal (1992) |
Edward C. T. Chao (Edward Ching-Te Chao) (November 30, 1919 – February 3, 2008) was one of the founders of the field of impact metamorphism, the study of the effects of meteorite impacts on the Earth's crust.
Born in Suzhou, China, he was best known for discovering two high-pressure forms of silica in nature, coesite and stishovite.
Chao came to the United States in 1945 to teach Chinese to American troops. He then attended the University of Chicago and was granted a PhD in geology in 1948. In 1949, he was employed by the United States Geological Survey (USGS), where he spent his entire professional career until retiring in 1994.
Chao worked on a variety of topics over the course of his USGS career, including engineering geology, economic geology, and coal petrology. However, he was best known for his work on impact geology and tektites. Shortly after he began work on tektites in 1960, Chao was given a sample of sandstone from the vicinity of Meteor Crater, Arizona. From this material, he was able to isolate an unusual mineral with high refractive index, which he showed to be a high-pressure polymorph of silicon dioxide. He named the new mineral coesite in honor of the scientist who had synthesized the same phase in the laboratory seven years earlier. Several years later, Chao found a second high-pressure polymorph of silica in these rocks. It too had been previously synthesized in laboratory studies, but was not known to occur in nature. He named this mineral stishovite in honor of the person who had first made it, Russian physicist, Sergei Stishov. Coesite and stishovite became known as hallmarks of impact crater events, which were essentially the only natural processes that produced high enough pressures to transform ordinary quartz into both of these dense minerals. Chao went on to find coesite and stishovite in rocks from the Ries Crater in Bavaria, Germany, establishing that this structure was also produced by impact cratering.
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