Principal Triangulation of Great Britain

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Three foot Theodolite used in the triangulation

The Principal Triangulation of Britain was a triangulation project carried out between 1784 and about 1853 at the instigation of senior surveyor General William Roy (1726–1790).

History[edit]

In 1783 the French Academy of Sciences suggested it would be useful to astronomy to connect the royal observatories of London and Paris through the scientific method of triangulation. After the Royal Society agreed, General Roy commissioned a new theodolite from leading instrument maker Jesse Ramsden. The baseline for the triangulation was established in 1784 between Hampton Poor House and King's Arbour on Hounslow Heath, a distance of just over 27,400 feet.[1][2]

This Ramsden theodolite, delivered in 1787, for the first time divided angular scales accurately to within a second of arc.[3] General Roy and his team used it to accurately triangulate the distance between the observatories. Calculations were completed in 1787.

The baseline derived during that work, together with the new theodolite, served as the basis for the planning and execution of the subsequent work on the Principal Triangulation. Around 1791, shortly after his death, Roy's team began the field work, using the specially built Ramsden theodolite. In 1794 a seven mile long baseline of verification was measured on Salisbury Plain.[4]

Eventually the triangulation extended to cover the whole of the British Isles, after it was decided in 1824 that a 6-inch-to-the-mile (1:10,560) map of Ireland was necessary for accurate land taxing.

The Principal Triangulation was subsequently superseded by the Retriangulation of Great Britain some 150 years later.

Baseline measurement[edit]

The original base-line across Hounslow Heath was measured with deal rods and iron bars to be 27,404 ft. It was re-measured with 1,370 placements of glass tubes as 27,406 ft. This was corrected for temperature and mean sea-level, and the value achieved an accuracy of 1 inch in 27,404 ft, which is 3 parts per million.

Corrections[edit]

During subsequent triangulation errors due to atmospheric diffraction, deflection of plumb-bobs, temperature, and the spherical nature of the earth (meaning there were more than 180 degrees in a triangle) were all allowed for.

See also[edit]

References[edit]

  1. ^ Major General William Roy biography, Royal Engineers Museum
  2. ^ Michael Knowles, THE FRENCH CONNEXION – BETWEEN ENGLISH AND FRENCH MAP SURVEYS, Proceedings of the BRLSI Volume 7 2003
  3. ^ Insley, J. (2008) The Tale of the Great Theodolites, retrieved 8 january 2014.
  4. ^ Lieut.-Colonel T. Pilkington White, The Ordnance Survey Of The United Kingdom, Scottish Mountaineering Club Journal Volume 2 Number 5

Further reading[edit]

External links[edit]