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Retriangulation of Great Britain

Retriangulation of Great Britain is a science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Retriangulation of Great Britain rather than just read about it. In short: The Retriangulation of Great Britain was a triangulation project carried out between 1935 and 1962 that sought to improve the accuracy of maps of Great Britain. Data gathered from the retriangulation replaced data gathered during the Principal Triangulation of Great Britain, which had been performed between 1783 and 1851.

Retriangulation of Great Britain — main illustration
Retriangulation of Great Britain — illustration

Key takeaways

  • Retriangulation of Great Britain belongs to science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Retriangulation of Great Britain to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Retriangulation of Great Britain from memory before moving on to harder problems.

Reference excerpt

The Retriangulation of Great Britain was a triangulation project carried out between 1935 and 1962 that sought to improve the accuracy of maps of Great Britain. Data gathered from the retriangulation replaced data gathered during the Principal Triangulation of Great Britain, which had been performed between 1783 and 1851. The work was designed to form a complete new survey control network for the whole country, and to unify the mapping of the United Kingdom from local county projections into a single national datum projection and reference system. Its completion led to the establishment of the OSGB36 datum and Ordnance Survey National Grid in use today.

History and overview

The retriangulation was begun in 1935 by the Director General of the Ordnance Survey, Major-General Malcolm MacLeod. It was directed by the cartographer and mathematician Martin Hotine, head of the Trigonometrical and Levelling Division (TLD). The work was halted by the outbreak of World War II in 1939, by which time the primary triangulation network covered all of England and Wales, but only as far as the Moray Firth in Scotland. Secondary triangulation had commenced in 1945, and after the end of the war, the retriangulation work was focused on secondary and lower-order survey work, to expedite the completion of new large-scale surveys. The wartime priorities of the TLD were focused on survey work in connection with the war effort, such as airfield and military construction, survey and computations for anti-aircraft and coastal battery positions, and survey of radiolocation sites. One-third of the Ordnance Survey staff were called up during the war, and the headquarters in Southampton was bombed and badly damaged. Staff were relocated to the Home Counties, where they produced 1:25,000 scale maps of France, Italy, Germany and most of the rest of Europe in preparation for invasion. Primary triangulation observations were not resumed until 1949, and completed in 1952. A problem during the Principal Triangulation was that the exact locations of surveying stations were not always rediscoverable, relying on buried markers and unreliable local knowledge. To overcome this, a network of permanent surveying stations was built, most familiarly the concrete triangulation pillars (about 6,500 of them) found on many British Isles hill and mountain tops, but there were many other kinds of surveying stations used. To minimise differences between the 1783–1851 survey and the retriangulation, eleven Principal Triangulation stations, ranging from Dunnose on the Isle of Wight to Great Whernside in Yorkshire, were chosen and pillars erected on them to act as the core framework from which all other measurements were made. The main work of the Retriangulation was finished in 1962, creating the Ordnance Survey National Grid. This system continued to be used, and measurements refined by ground-based surveying, into the 1980s, after which satellite use took over. Electronic measuring devices were introduced towards the end of the Retriangulation, but at that time were not proven reliable enough to replace traditional surveying.

The Primary Retriangulation and survey field work

One of the first steps in the retriangulation was the adoption of a new projection for the mapping, with the existing Cassini projection replaced by the Transverse Mercator. This was preferred by the Ordnance Survey because the use of the Cassini projection would have resulted in angular distortion of almost four minutes of arc in the survey.

Planning and work on the new projection Neither the solid form of the Earth, nor the geoid (an equipotential surface of Earth's gravity field, comparable to the imaginary surface that mean sea level would follow in the absence of winds, tides and currents), can be fully defined by simple formulae. The spheroid is the nearest mathematical model, but as no one spheroid fits worldwide, a number have to be used. The Airy spheroid provides a good fit in the region of the British Isles, and the Transverse Mercator Projection of this spheroid was therefore adopted by the Ordnance Survey as the basis of the national co-ordinate system. No projection can be true to scale across its entirety. In the Transverse Mercator, the scale at any given point increases in correlation with its east or west distance from the central meridian. The scale along the north-south line that contains the point remains consistent. The true origin of the projection lies at latitude 49° N, longitude 2° W. A false origin positioned roughly 170 kilometres west of The Lizard was established to ensure all national grid coordinates remained positive, as the whole country is further east and further north than that point. In this system, the central meridian is 400 km east. The scale on the central meridian should be correct, or 1. However, to ensure that scale error is imperceptible on the national mapping at the eastern and western boundaries, a scale reduction of 1:2500 was applied. This provides a local scale factor of 0.9996 at the central meridian. The scale continually increases with distance from the central meridian, east and west, reaching 1 at 580 km east and 220 km west. It continues to rise, reaching 1.0005 at the eastern and western extremes. The corresponding local scale factor must be employed to convert a site measured plane length to a projection distance, and vice versa. As the spheroid is set at mean sea level, any surveyed length must be reduced to mean sea level before applying the local scale factor.

Commencement of retriangulation fieldwork The primary triangulation work commenced with the division of survey work into blocks. The size of these blocks was governed by the largest number of survey observations which could be computed in a simultaneous least-squares adjustment. Reconnaissance of survey stations was commenced in 1935, using Tavistock theodolites to confirm the inter-visibility of stations. Survey of the triangulation commenced in April 1936, with observations made during the hours of darkness to electric beacon lamps manufactured by Cooke, Troughton & Simms. In flat areas of the country, such as East Anglia, Bilby towers designed by the United States Coast and Geodetic Survey were used.

… excerpt ends here. Continue reading the full article.

Illustrations

Retriangulation of Great Britain: The Crow Knowl triangulation station at Crompton Moor in the South Pennines. It is one of the concrete pillars erected by the Ordnance Survey during the retriangulation of Great Britain. It was possible (in clear weather) to see at least two other trig points from any one trig point.
The Crow Knowl triangulation station at Crompton Moor in the South Pennines. It is one of the concrete pillars erected by the Ordnance Survey during the retriangulation of Great Britain. It was possible (in clear weather) to see at least two other trig points from any one trig point.
Retriangulation of Great Britain: Martin Hotine (17 June 1898 – 12 November 1968), head of the Trigonometrical and Levelling Division of the Ordnance Survey responsible for the retriangulation
Martin Hotine (17 June 1898 – 12 November 1968), head of the Trigonometrical and Levelling Division of the Ordnance Survey responsible for the retriangulation
Retriangulation of Great Britain: A Tavistock theodolite
A Tavistock theodolite

Worked examples

Example 1 — a first encounter with Retriangulation of Great Britain

Start with the simplest possible case. Write down what Retriangulation of Great Britain claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Retriangulation of Great Britain before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Retriangulation of Great Britain ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Retriangulation of Great Britain

In research
Retriangulation of Great Britain appears in science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Retriangulation of Great Britain in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Retriangulation of Great Britain is common in secondary-school and first-year university syllabi. It links to neighbouring topics Angle, Geodetic surveys, Geography of Great Britain, so understanding it makes those chapters shorter.
In everyday life
Look for Retriangulation of Great Britain outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Retriangulation of Great Britain in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Retriangulation of Great Britain means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Retriangulation of Great Britain out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Retriangulation of Great Britain in simple terms?

The Retriangulation of Great Britain was a triangulation project carried out between 1935 and 1962 that sought to improve the accuracy of maps of Great Britain. Data gathered from the retriangulation replaced data gathered during the Principal Triangulation of Great Britain, which had been performe…

Why does Retriangulation of Great Britain matter?

Because it connects several science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Retriangulation of Great Britain?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Retriangulation of Great Britain.

Tags

  • Angle
  • Geodetic surveys
  • Geography of Great Britain
  • Surveying of the United Kingdom

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