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  1. Sir George Biddell Airy KCB FRS (/ ˈ ɛər i /; 27 July 1801 – 2 January 1892) was an English mathematician and astronomer, as well as the Lucasian Professor of Mathematics from 1826 to 1828 and the seventh Astronomer Royal from 1835 to 1881.

    • 27 July 1801, Alnwick, Northumberland, England
  2. Sir George Biddell Airy was an English scientist who was astronomer royal from 1835 to 1881. Airy graduated from Trinity College, Cambridge, in 1823. He became Lucasian professor of mathematics at Cambridge in 1826 and Plumian professor of astronomy and director of the Cambridge observatory in.

    • The Editors of Encyclopaedia Britannica
  3. Jul 27, 2022 · The Density of the Earth. Another of Airys research objects was the determination of the mean density of planet Earth. He tackled the problem with the help of pendulums that he made swing on the surface and in the depths. In 1826, he began experiments at the Dolcoath Mine in Cornwall, but the pendulum, which was set up underground, was buried.

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  5. Learn about the life and achievements of Sir George Biddell Airy, the Astronomer Royal who expanded the Royal Observatory and designed the Airy Transit Circle telescope. Find out how he contributed to science, navigation, astronomy and eclipse expeditions.

  6. Learn about the life and work of George Biddell Airy, a British astronomer and mathematician who was a fellow of the Royal Society. Explore his publications, correspondence, and related items on topics such as astronomy, meteorology, tides, and the state of the interior of the earth.

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  7. Sir George Biddell Airy KCB FRS ( / ˈɛəri /; 27 July 1801 – 2 January 1892) was an English mathematician and astronomer, as well as the Lucasian Professor of Mathematics from 1826 to 1828 and the seventh Astronomer Royal from 1835 to 1881.

  8. May 8, 2018 · Airy, George Biddell (1801–92) A Cambridge astronomer and mathematician, Airy became Astronomer Royal in 1835. He investigated planetary motion and tides, and studied the Earth and its density, using gravity measurements. His name is used to describe one version of the theory of isostasy.

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