James David Forbes

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James David Forbes
Natural Philosophy, University of Edinburgh (1833–60)
Principal of the United College, St Andrews
(1860–8)
Notes
Member of the Highland Society (1836)
Resting place: Dean Cemetery, Edinburgh
The grave of James David Forbes, Dean Cemetery
The inscription on James David Forbes's grave

James David Forbes

conduction of heat and seismology. Forbes was a resident of Edinburgh for most of his life, educated at its University and a professor there from 1833 until he became principal of the United College of St Andrews
in 1859.

Life and work

Forbes was born on 20 April 1809 at 86

William Forbes, 7th Baronet, of Monymusk and Pitsligo (1773–1828) and Williamina Belches of Invermay. His brothers were the advocate and agriculturalist Sir John Stuart Hepburn Forbes
of Fettercairn and Pitsligo and the banker Charles Forbes.

He entered the

Royal Society of London. At this time he maintained correspondence with Sir David Brewster, who encouraged him to pursue an original research in science. A year later he was appointed professor of natural philosophy at the University of Edinburgh in succession to Sir John Leslie, and during his tenure of that office, which he did not give up until 1860, he not only proved himself an active and efficient teacher, but also did much to improve the internal conditions of the university. In 1859 he was appointed successor to Brewster in the principalship of the United College of St Andrews, a position which he held until his death at Clifton in 1868.[3]

As a scientific investigator he is best known for his researches on heat and on glaciers.

rock salt. His work won him the Rumford Medal of the Royal Society in 1838, and in 1843 he received its Royal Medal for a paper on the "Transparency of the Atmosphere and the Laws of Extinction of the Sun's Rays passing through it."[5] He invented an inverted pendulum seismometer in 1842.[6][7]

In response to a series of earthquakes near Comrie in Scotland in 1839, a committee was formed in the United Kingdom in order to produce better detection methods for earthquakes. The outcome of this was the production of one of the first modern seismometers by Forbes, first presented in a report by David Milne-Home in 1842.[7] This seismometer was an inverted pendulum, which recorded the measurements of seismic activity through the use of a pencil placed on paper above the pendulum. The designs provided did not prove effective, according to Milne's reports.[7]

In 1846 he began experiments on the temperature of the earth at different depths and in different soils near Edinburgh, which yielded determinations of the thermal conductivity of trap-tufa, sandstone and pure loose sand. Towards the end of his life he was occupied with experimental inquiries into the laws of the conduction of heat in iron bars, and his last piece of work was to show that the thermal conductivity of iron diminishes with increase of temperature.[8]

His attention was directed to the question of the flow of glaciers in 1840 when he met Louis Agassiz at the Glasgow meeting of the British Association, and in subsequent years he made several visits to Switzerland, where he was particularly impressed by Bernhard Studer's theories,[9] and also to Norway for the purpose of obtaining accurate data. His observations led him to the view that a glacier is an imperfect fluid or a viscous body which is urged down slopes of a certain inclination by the mutual pressure of its parts, and involved him in some controversy with Tyndall and others both as to priority and to scientific principle.[10] A notable defender of Forbes in this controversy was John Ruskin, the two having first met by coincidence in 1844 during a study tour of the Alps.[11]

During these expeditions, he made many measurements of the boiling point of water at various altitudes.[12] This data set, published in 1857, is often known in statistics as Forbes's data, its utility being that:

  • It illustrates how a
    physical phenomenon
    observed.
  • It emphasises the importance of residuals analysis in linear regression as the residuals manifest an outlier that is not apparent in a visual inspection of the raw data.

Forbes was also interested in geology, and published memoirs on the thermal springs of the Pyrenees, on the extinct volcanoes of the Vivarais (Ardèche), on the geology of the Cuchullin and Eildon hills, etc. In addition to about 150 scientific papers, he wrote Travels through the Alps of Savoy and Other Parts of the Pennine Chain, with Observations on the Phenomena of Glaciers (1843); Norway and its Glaciers (1853); Occasional Papers on the Theory of Glaciers (1859); A Tour of Mont Blanc and Monte Rosa (1855). He was also the author (1852) of the "Dissertation on the Progress of Mathematical and Physical Science," published in the eighth edition of the Encyclopædia Britannica.[10]

The

Glacier de Saleina and the Glacier du Tour[13] in the Mont Blanc massif.[14]

James David Forbes was a devout Christian, as can be seen in the work "Life and Letters of James David Forbes" (1873), a compilation of personal letters written by Forbes, co-authored by John Campbell Shairp and Forbes's student Peter Guthrie Tait.

He died on 31 December 1868 and is buried in Dean Cemetery in Edinburgh. The grave is marked by a simple but large grey granite Celtic cross and lies on the south side of the main path just west of the roundel. His wife, Alicia Wauchope (1824–1885), is buried with him. His cousins were Scottish Episcopal Church leaders Alexander Penrose Forbes and George Hay Forbes. His son was the scientist George Forbes.

Selected publications

  • Travels through the Alps of Savoy and Other Parts of the Pennine Chain, with Observations on the Phenomena of Glaciers. Profr. Forbes's travels through the Alps. A. and C. Black ; Longman, Brown, Green, and Longmans. 1843.[15]
  • Norway and its Glaciers. A. and C. Black. 1853.
  • A Tour of Mont Blanc and Monte Rosa. Travels in the Alps of Savoy. A. and C. Black. 1855.
  • Occasional Papers on the Theory of Glaciers. A. and C. Black. 1859.

References

  1. ISBN 978-0-684-10114-9
    .
  2. Proceedings of the Royal Society of London
    , vol. XIX, p ii
  3. ^ Chisholm 1911, p. 638.
  4. ^ "Forbes, James David" . Dictionary of National Biography. London: Smith, Elder & Co. 1885–1900.
  5. ^ Chisholm 1911, pp. 638–639.
  6. ISBN 978-0-902198-84-5. Archived from the original
    (PDF) on 4 October 2006. Retrieved 24 January 2011.
  7. ^ a b c Oldroyd, David (2007). "The Study of Earthquakes in the Hundred Years Following Lisbon Earthquake of 1755". Researchgate. Earth sciences history: journal of the History of the Earth Sciences Society. Retrieved 4 October 2022.
  8. ^ Chisholm 1911.
  9. ^ Letters from Forbes in the Whewell papers, to William Whewell. Forbes wrote that '[Studer's] merit has not been sufficiently recognized elsewhere partly owing to the jealousy of the French'.
  10. ^ a b Chisholm 1911, p. 639.
  11. ^ E.T. Cook (1911). The Life of John Ruskin, Volume I (1st ed.). pp. 164–165.
  12. ^ Forbes's data Archived 5 September 2015 at the Wayback Machine Column 1 is a serial number; 2, boiling point in Fahrenheit and 3, pressure in inches of mercury
  13. ^ Aiguille Forbes (1:25,000) (Map). Swisstopo. Retrieved 29 January 2015.
  14. ^ Discover New Zealand:A Wises Guide (9th ed.). 1994. p. 377.
  15. ^ "Review of Travels through the Alps of Savoy, and other Parts of the Pennine Chain; with Observations on the Phenomena of Glaciers by James D. Forbes". The Quarterly Review. 74: 39–70. June 1844.

Further reading

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