Part 1 – The Language of Maps: A map for every occasion

Cite this article

Overview

The QDL boasts roughly 800 maps of the Arabian Peninsula and the Gulf. This is the first article in a series of five by the author, explaining cartographic terminology.

Other articles in this series: Part 2; parts 3-5 are forthcoming. 

Note: further cartographic terminology from the records can be found in the Glossary.

The QDL has a generous range of maps, and our journey here begins by attempting to classify them. To understand a map fully, we need to appreciate the map-making process, including the methods of the surveyor. From the surprising complexities of position fixing, to the mysteries of unravelling marginalia, maps abound with challenging terminology.

A sumptuous map showing the peninsula of Aden. Captain Trevenen James Holland, 1863. IOR/X/3257, f. 1r
A sumptuous map showing the peninsula of Aden. Captain Trevenen James Holland, 1863. IOR/X/3257, f. 1r

Maps are drawn for many purposes, including navigation, planning, administration, tourism, and military campaigns. The QDL hosts everything from world to city maps, accurate to sketch maps, themed to general maps. Categorising them can be fraught, because some maps display so many characteristics that they fit comfortably into numerous categories. What follows is an inventory of the map categories found on the QDL.

Maps, Charts, and Plans

Like many specialisms, cartography – the art and science of drawing maps – has its own lexis. The term map embraces almost any kind of diagrammatic portrayal of an area as viewed from above. However, some maps can be described more precisely. Plans, for example, are large-scale maps of relatively small areas, the generous scale allowing depiction of such details as residential roads, pavements, individual buildings, and house numbers.

Charts, on the other hand, are specifically for mariners and aviators. Hydrographic charts focus on water bodies and their land margins, typically portraying soundings Measurements of the depth of a body of water. , rocks, sands, navigational aids (for example, lighthouses and buoys), and anchorages. Meanwhile air charts might include runway information, air space boundaries, and minimum flying heights (as calculated from terrain elevations and obstructions such as tall buildings and power lines).

Examples on the QDL of a plan, hydrographic chart, and air chart
Examples on the QDL of a plan, hydrographic chart, and air chart

Top: Extract from a sketch plan of Naresi and Ahwaz. General Staff, India, 1938. IOR/L/MIL/17/15/24, f. 65r
Middle: Extract from a hydrographic chart of the Gulf. The numbers are soundings in fathoms. The letters show seabed characteristics (M = mud, G = gravel, Sh = shingle). The dots reveal the extent of sand and mud at low tide. Note the anchor symbol at Doha. Admiralty, 1912. IOR/X/3828/2837b, f. 1r
Bottom: Extract from an air chart of the Gulf. Following international conventions, air information is shown in purple. War Office, 1933. IOR/R/15/2/263, f. 194r

Topographic versus The Rest

A fundamental distinction exists between topographic maps and all others. Serious cartophiles (map enthusiasts) regard topographic maps as “proper” maps, in that they show features in their true position. Most official government mapping falls into this category. The rest comprise mainly sketch maps drawn when an approximate representation will suffice or where time and/or resources are limited.

A topographical map (above) and sketch map of the same area around Tehran
A topographical map (above) and sketch map of the same area around Tehran

Top: Extract from a topographical map of Tehran and north-west Persia. Survey of India, 1922. IOR/L/MIL/17/15/23, f. 302r
Bottom: Extract from a sketch map of the Trans-Persian Railway. Cartographer unknown, 1928. IOR/L/PS/10/794, f. 156r

One particular type of non-topographic map is the topological map. This preserves the relationships between features while sacrificing other properties to improve clarity. Metro maps are good examples, where stations appear in the correct order and lines interchange in the correct places, yet distortion is applied to scale (stations are depicted as equidistant irrespective of the true distance) and direction (lines are always drawn horizontally, vertically or on forty-five-degree diagonals).

Extract from a topological map, depicting the Mirjawa Station Yard. The map is not to scale, but the sequences of, and connections between the tracks are still correct. Cartographer unknown, 1930. IOR/L/MIL/17/15/7, f. 71r
Extract from a topological map, depicting the Mirjawa Station Yard. The map is not to scale, but the sequences of, and connections between the tracks are still correct. Cartographer unknown, 1930. IOR/L/MIL/17/15/7, f. 71r

Thematic maps

Thematic maps emphasise information on a particular topic, perhaps geology, population, or climate. Usually, the map comprises two distinct information layers: an unobtrusive background or base map A map portraying background detail. (often topographic in nature) and a more prominent thematic layer. For example, geology maps typically combine a faint base layer of hills, rivers, roads, railways, and towns, with another superimposed layer showing the underlying rock types. Other categories of thematic map on the QDL include cadastral (property ownership) maps, population maps, and maps portraying meteorology and ocean conditions.

Extract from a geological map of the Turko-Persian frontier. An unobtrusive monochrome base map is overlaid with coloured geology. W. K. Loftus, c. 1863. ST 393, vol 17, p 166a, f. 1r
Extract from a geological map of the Turko-Persian frontier. An unobtrusive monochrome base map is overlaid with coloured geology. W. K. Loftus, c. 1863. ST 393, vol 17, p 166a, f. 1r

Overprints and Overlays

Sometimes extra information is added to a map later. The existing map becomes a base map A map portraying background detail. , and the additional information (for example troop positions) may be added either by printing over it (an overprint Additional information printed on to an existing map. ), or by plotting it on to a transparent or translucent sheet and aligning (or keying) it to the existing map (an overlay A transparent or translucent sheet designed to be placed over a map to show additional information. ). Overprints Additional information printed on to an existing map. and overlays A transparent or translucent sheet designed to be placed over a map to show additional information. are also popular methods for updating information, such as adding new roads.

Extract from an overprint, showing the positions of British and Turkish troops in red and green respectively. In a quickly changing battle, new overprints could be added several times daily. War Office, 1916. Mss Eur F112/555, f. 5r
Extract from an overprint, showing the positions of British and Turkish troops in red and green respectively. In a quickly changing battle, new overprints could be added several times daily. War Office, 1916. Mss Eur F112/555, f. 5r
Base map (left) and keyed overlay depicting a possible redistribution of Ottoman and Arabian Territory after the First World War. Edward Stanford and the Foreign Office, 1918
Base map (left) and keyed overlay depicting a possible redistribution of Ottoman and Arabian Territory after the First World War. Edward Stanford and the Foreign Office, 1918

Left: Mss Eur F112/570, f. 28r | Right: Mss Eur F112/570, f. 27r

Isopleths and Choropleths

Maps are also useful tools for showing geographical trends in statistical data (e.g. climate or population). Two types are particularly suited. The first is the isopleth, a map comprising lines joining points of equal value. For example, lines joining points of equal height are contours and lines joining points of equal air pressure are isobars. Structure contours, specifically, show the height above an underground structure (e.g. the upper surface of a naturally occurring body of underground water), and often bear no relation to land surface contours.

Extract from a structure contour map showing the distribution of artesian water in Bahrain. Bahrain Petroleum Company, 1948. IOR/R/15/2/850, f. 18r
Extract from a structure contour map showing the distribution of artesian water in Bahrain. Bahrain Petroleum Company, 1948. IOR/R/15/2/850, f. 18r

The second type is the choropleth, a map that uses a graded colour scale to portray the average value of a particular attribute within defined geographical boundaries. Where isopleths and choropleths show information on specific topics, they are also thematic maps.

Extract from a map of Izmir that would be a choropleth if each administrative area were shaded on a graded scale to show the percentage of Greeks/Armenians present. Royal Geographical Society and War Office, 1916-20. Mss Eur F112/570, f. 5r
Extract from a map of Izmir that would be a choropleth if each administrative area were shaded on a graded scale to show the percentage of Greeks/Armenians present. Royal Geographical Society and War Office, 1916-20. Mss Eur F112/570, f. 5r

Route Maps

During journeys of discovery, speedy travel requires light loads, and there is neither the time nor equipment for a full survey. A route map A map depicting a specific journey. must suffice. These plot just the route, the features along it, and significant features visible from it. Many route maps A map depicting a specific journey. are long and thin and often aligned to the shape of the paper rather than adopting the more conventional ‘north at the top’.

Extract from a route map across Arabia. Captain George Forster Sadleir, 47th Regiment of Foot, c. 1821. IOR/X/3215, f. 1r
Extract from a route map across Arabia. Captain George Forster Sadleir, 47th Regiment of Foot, c. 1821. IOR/X/3215, f. 1r

Related Items

The QDL also houses items related to maps. Cross sections The shape revealed by cutting vertically through a land surface at right angles to the feature of interest. show the shape revealed by cutting vertically through the land surface at right angles to the feature of interest. The most common types are geological cross sections The shape revealed by cutting vertically through a land surface at right angles to the feature of interest. (exposing the sub-surface rock structure) and river cross sections The shape revealed by cutting vertically through a land surface at right angles to the feature of interest. (portraying the shape of a river valley at right angles to the direction of flow).

Extract from a geological cross section of the River Khabur. The enlarged vertical scale makes the hills clearer. Ralph du Boulay Evans, Survey Party, Middle East Forces, 1920. IOR/L/PS/10/815, f. 44r
Extract from a geological cross section of the River Khabur. The enlarged vertical scale makes the hills clearer. Ralph du Boulay Evans, Survey Party, Middle East Forces, 1920. IOR/L/PS/10/815, f. 44r

Perpendicular to a cross section The shape revealed by cutting vertically through a land surface at right angles to the feature of interest. is the profile (or long profile), the shape revealed by cutting vertically through the land surface along the feature’s length. For example, the long profile of a river valley shows the river’s changing gradient from source to mouth. Similar profiles can show the gradients of roads and railways.

Extract from a profile section of the Lynch Road in south western Persia. Intelligence Branch Topographical, India, 1909. IOR/L/MIL/17/15/10/3, f. 66r
Extract from a profile section of the Lynch Road in south western Persia. Intelligence Branch Topographical, India, 1909. IOR/L/MIL/17/15/10/3, f. 66r

The QDL is a rich resource, and its maps are no exception. Whether it is a topographic map for geographical context, a thematic map for more specific needs, or an explorer’s sketch map to unlock the undiscovered, the QDL has a map for everyone. 

Part 2 examines how these maps were made.