Ordnance Survey Maps - Six-inch England and Wales, 1842-1952

Triangulation, projection, meridians and sheet lines

Diagram showing chain surveying by triangles
Chain surveying by triangles.
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Triangulation had been employed by European map-makers intermittently from the sixteenth century as a means of working out a network of distances from measuring a single base line and the related angles of set of triangles. Ordnance Survey's achievements in triangulation were to use the latest instruments and greater manpower to measure more accurate angles and base line distances than before in order to position a network of triangulation stations over the whole country between 1791 and 1822. This is often termed the Primary Triangulation. In the following decades, work on geodesy progressed on several fronts, and much of the earlier work was checked and revised in an ongoing quest for greater accuracy. For example, the Greenwich-Paris connection by trigonometry was re-measured in 1821-1823, new chronometers for better determination of longitude were used under the direction of the Astronomer Royal George Airy in the 1840s, latitudes were more accurately determined with improved zenith sectors, and the shape of the earth or spheroid was extensively researched. In the early 1860s, the triangulations of England, France and Belgium were connected, and further international collaboration with Russia and Prussia allowed the 52 degree North parallel, from the West of Ireland to the Urals, to be accurately measured. Much of the credit for these mid-century improvements in Ordnance Survey rests with Alexander Ross Clarke (1828-1914), who headed the Trigonometrical and Levelling Branch until the early 1880s. Clarke was responsible for completing the Principal Triangulation in the 1850s, adjusting as he did the positions of 289 base stations based on revised measurements which were not improved upon until the 1935 Retriangulation.


Ordnance Survey County Series maps were based on the Cassini Projection, a transverse cylindrical projection, where a central meridian of longitude forms the point of origin and the line of zero distortion (where all distances are true to scale). Distances along great circles of latitude that meet this central meridian at right angles are also plotted true to scale, but all (North-South) distances parallel to the central meridian are increasingly too great on the map, the farther they are away from the central meridian. It follows that the Cassini Projection is best suited for areas with a relatively narrow extent in longitude, perhaps no more than three or four counties width in the case of the large-scale maps.

Following the recommendations of the Ordnance Survey Davidson Committee in 1938, all large-scale maps were recast on a new national Transverse Mercator projection with metric sheet lines, subsequently known as the National Grid. From 1945 the new National Grid kilometre square lines were usually overprinted onto the County Series maps.


On the County Series maps, although some counties had their own separate county point of origin (usually the nearest triangulation station to the North-South centre line of the county), most counties shared a meridian. Due to the nature of the Cassini projection, counties with separate origins do not fit precisely with their neighbouring county sheets, especially at their East-West extents. Those counties sharing a common origin - for example, 14 counties in central England with the Dunnose origin, or 11 counties in or bordering on Wales sharing the Llangeinor origin - have regular adjoining sheetlines and common sheets at county borders. These sheets usually carry references under both counties, although on our website, we have tended to record the sheet reference under the first named county only. Please note that our recording of dates for sheets at county boundaries is also usually for the first named county only: the marginal information in the lower left of the sheet contains fuller information on dates of survey/revision of neighbouring counties for the whole sheet.

Unlike in Scotland, where 11 counties changed meridians and sheet lines over the course of the County Series, only two counties in England and Wales changed meridians over time: Essex and Northumberland after 1912-13. These two counties had new sheet lines for the County Series maps, with their sheet numbers often prefixed by the letter 'N' after 1912-13.

Within each county, sheets were laid out from North-West to South-East in separate county sequences.

Full-sheet and quarter-sheet extents

Illustration of an Ordnance Survey copper plate printing machine
OS copper plate printing machine.
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From the 1840s to the early 1880s, all the six-inch maps were engraved and printed from special hammered copper, 1/10th inch thick and measuring 26.5 by 38.5 inches in extent. ( Read more about OS engraved six-inch map printing ). From 1882 onwards, the usual practice was to print the maps as quarter-sheets by photo- or helio-zincography. Zincography was significantly cheaper than copper plate engraving, and corrections were easier to make, but it was criticised for producing less clear maps. Photo- or helio-zincography also allowed the automatic reduction of 25 inch maps to the six-inch scale through photographic methods, allowing further economies in map production. The six-inch full sheets were resumed briefly between 1920-24, but were quickly discontinued, following protests from users.

The Ordnance Survey six-inch maps were generally uncoloured, but blue wash was used for water features in the 1890s, and red used for contours from ca. 1912.

All Ordnance Survey six-inch map sheets carried their relevant county name followed by the specific sheet number. Quarter-sheets, dividing the full-sheet area into North-West, North-East, South-West, and South-East quarters, were the more usual practice.


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