Map

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A map is a graphic representation of geographic phenomena—a symbolic depiction of the spatial relationships that phenomena such as objects, regions, or themes have with each other. It is a tool used for performing geographic tasks. Many maps are static two-dimensional, geometrically accurate (or approximately accurate) representations of three-dimensional space, while others are dynamic or interactive, even three-dimensional. While most maps are commonly used to depict geography, maps may represent any space, real or imagines, independent of context or scale in other fields of study (i.e. brain mapping, DNA mapping, extraterrestrial mapping).

Geographic maps

Cartography, or map-making is the study, and often the practice, of crafting representations of the Earth upon a flat surface (see History of cartography), and one who makes maps is called a cartographer.

Road maps are perhaps the most widely used maps today, and form a subset of navigational maps, which also include aeronautical and nautical charts, railroad network maps, and hiking and bicycling maps. In terms of quantity, the largest number of drawn map sheets is probably made up by local surveys, carried out by municipalities, utilities, tax assessors, emergency services providers, and other local agencies. Many national surveying projects have been carried out by the military, such as the British Ordnance Survey (now a civilian government agency internationally renowned for its comprehensively detailed work).

In addition to location information maps may also be used to portray contour lines (isolines) indicating constant values of elevation, topography, temperature, rainfall, etc.

Orientation of maps

The Hereford Mappa Mundi, about 1300, Hereford Cathedral, England. A classic "T-O" map with Jerusalem at centre, east toward the top, Europe the bottom left and Africa on the right.

The term Orientation (physical) refers to the relationship between directions on a map and compass directions. The word orient is derived from orients, meaning east. In the Middle Ages many maps, including the T and O maps, were drawn with east at the top. Today the most common, but far from universal, cartographic convention is that North is at the top of a map. Examples of maps not oriented to north are:

  • Buckminster Fuller's Dymaxion maps are based on a projection of the Earth's sphere onto an icosahedron. The resulting triangular pieces may be arranged in any order or orientation.
  • Many maps used in the Society for Creative Anachronism show the west at the top, in honor of the Society starting in California.[citation needed]
  • Maps from non-Western traditions are oriented a variety of ways. Old maps of Edo show the Japanese imperial palace as the "top", but also at the centre, of the map. Labels on the map are oriented in such a way that you cannot read them properly unless you put the imperial palace above your head.[citation needed]
  • Medieval European T and O maps such as the Hereford Mappa Mundi were centred on Jerusalem with east at the top. Indeed, prior to the reintroduction of Ptolemy's Geography to Europe around 1400, there was no single convention in the West. Portolan charts, for example, are oriented to the shores they describe.
  • Polar maps of the Arctic or Antarctic regions are conventionally centred on the pole, in which case the direction north would be towards or away from the centre of the map, respectively.
  • Reversed maps, also known as Upside-Down maps or South-Up maps, which generally show Australia and New Zealand at the top of the map instead of the bottom.
  • Route and channel maps have traditionally been oriented to the road or waterway they describe.

Scale and accuracy

Many, but not all, maps are drawn to a scale, expressed as a ratio such as 1:10,000, meaning that 1 of any unit of measurement on the map corresponds exactly, or approximately, to 10,000 of that same unit on the ground. The scale statement may be taken as exact when the region mapped is small enough for the curvature of the Earth to be neglected, for example in a town planner's city map. Over larger regions where the curvature cannot be ignored we must use map projections from the curved surface of the Earth (sphere or ellipsoid) to the plane. The impossibility of flattening the sphere to the plane implies that no map projection can have constant scale: on most projections the best we can achieve is accurate scale on one or two lines (not necessarily straight) on the projection. Thus for map projections we must introduce the concept of point scale, which is a function of position, and strive to keep its variation within narrow bounds. Although the scale statement is nominal it is usually accurate enough for all but the most precise of measurements.

Large scale maps, say 1:10,000, cover relatively small regions in great detail and small scale maps, say 1:10,000,000, cover large regions such as nations, continents, and the whole globe. The large/small terminology arose from the practice of writing scales as numerical fractions: 1/10000 is larger than 1/10000000. There is no exact dividing line between large and small but 1/100000 might well be considered as a medium scale. Examples of large scale maps are the 1:25000 maps produced for hikers; on the other hand maps intended for motorists at 1:250,000 or 1:1,000,000 are small scale. A few popular map scales include 1:24,000, used by the USGS, where one inch is equal to 2000 feet and 1:63,360 where one inch is equal to one mile.

It is important to recognize that even the most accurate maps sacrifice a certain amount of accuracy in scale to deliver a greater visual usefulness to its user. For example, the width of roads and small streams are exaggerated when they are too narrow to be shown on the map at true scale; which on a printed map they would be narrower than could be perceived by the naked eye. The same applies to computer maps where the smallest unit is the pixel. A narrow stream say must be shown to have the width of a pixel even if at the map scale it would be a small fraction of the pixel width.

Cartogram: The EU distorted to show population distributions.
Sometimes the scale of a map is distorted deliberately. For example, the map of Europe shown here has been distorted to show population distributions. Clearly the basic scale is approximately uniform for the rough shape of the continent is still visible. This is an example of a cartogram.

Another example of distorted scale is the famous London Underground map. The basic geographical structure is respected but the tube lines (and the River Thames) are smoothed to clarify the relationships between stations. Near the centre of the map stations are spaced out more than near the edges of map.

Further inaccuracies may be deliberate. For example, cartographers may simply omit military installations or remove features solely in order to enhance the clarity of the map. For example, a road map may or may not show railroads, smaller waterways or other prominent non-road objects, and even if it does, it may show them less clearly (e.g. dashed or dotted lines/outlines) than the highways. Known as decluttering, the practice makes the subject matter that the user is interested in easier to read, usually without sacrificing overall accuracy. Software-based maps often allow the user to toggle decluttering between ON, OFF and AUTO as needed. In AUTO, the degree of decluttering is adjusted as the user changes the scale being displayed.

Projections

Map of large underwater features. (1995, NOAA)

Maps that depict the surface of the Earth also a projection, a way of translating the three-dimensional real surface of the geoid to a two-dimensional picture. There are nearly a dozen different projections, each capable of depicting different regions of the world more accurately than others. Carefully consider which projection will be best suited for the region you are mapping.

Electronic maps

From the last quarter of the 20th century, the indispensable tool of the cartographer has been the computer. Much of cartography, especially at the data-gathering survey level, has been subsumed by Geographic Information Systems (GIS). The functionality of maps has been greatly advanced by technology simplifying the superimposition of spatially located variables onto existing geographical maps. Having local information such as rainfall level, distribution of wildlife, or demographic data integrated within the map allows more efficient analysis and better decision making. In the pre-electronic age, such superimposition of data led Dr. John Snow to discover the cause of cholera. Today, it is used by agencies as diverse as wildlife conservationists and militaries around the world.

Even when GIS is not involved, most cartographers now use a variety of computer graphics programs to generate new maps.

Interactive, computerised maps are commercially available, allowing users to zoom in or zoom out (respectively meaning to increase or decrease the scale), sometimes by replacing one map with another of different scale, centred where possible on the same point. In-car global navigation satellite systems are computerised maps with route-planning and advice facilities which monitor the user's position with the help of satellites. From the computer scientist's point of view, zooming in entails one or a combination of:

  1. replacing the map by a more detailed one
  2. enlarging the same map without enlarging the pixels, hence showing more detail by removing less information compared to the less detailed version
  3. enlarging the same map with the pixels enlarged (replaced by rectangles of pixels); no additional detail is shown, but, depending on the quality of one's vision, possibly more detail can be seen; if a computer display does not show adjacent pixels really separate, but overlapping instead (this does not apply for an LCD, but may apply for a cathode ray tube), then replacing a pixel by a rectangle of pixels does show more detail. A variation of this method is interpolation.

For example:

  • Typically (2) applies to a Portable Document Format (PDF) file or other format based on vector graphics. The increase in detail is, of course, limited to the information contained in the file: enlargement of a curve may eventually result in a series of standard geometric figures such as straight lines, arcs of circles or splines.
  • (2) may apply to text and (3) to the outline of a map feature such as a forest or building.
  • (1) may apply to the text (displaying labels for more features), while (2) applies to the rest of the image. Text is not necessarily enlarged when zooming in. Similarly, a road represented by a double line may or may not become wider when one zooms in.
  • The map may also have layers which are partly raster graphics and partly vector graphics. For a single raster graphics image (2) applies until the pixels in the image file correspond to the pixels of the display, thereafter (3) applies.

See also: Webpage (Graphics), PDF (Layers), MapQuest, Google Maps, Google Earth, OpenStreetMap or Yahoo! Maps.

Index maps

Index maps are a type of finding aid that allow users find a set of maps covering their regions of interest along with the name or number of the relevant map sheet. An index maps provides geospatial representation on either a sheet of paper or a computer screen. In this way, a map acts as a kind of gazetteer, with the location (such as a call number) represented within a grid overlaying the maps surface.[1]

One important need for geospatial data such as this: political borders often change. Information is being searched by coordinates, rather than the metadata for a particular country and region that can be entered into a catalog. Additionally, in various institutions, maps are sometimes cataloged individually or as sets, resulting in various levels of specificity.

Street maps

A street map is a map showing roads and streets in a district or entire city. Street maps are great tools for navigating cities, towns or communities. They are available in printed forms, online on the internet or on mobile phones with GPRS connection.

Non-geographical spatial maps

Maps exist of the solar system, and other cosmological features such as star maps. In addition maps of other bodies such as the Moon and other planets are technically not geological maps.

Non-spatial maps

Many diagrams such as Gantt charts display logical relationships between items, and do not display spatial relationships at all.

Many maps are topological in nature, and the distances are completely unimportant, and only the connectivity is significant.

Limitations of Maps

Part of the problem with maps is that people often think that a map shows everything, like a photograph. A map is not a photograph. Maps do not show every bit of information; they are generalized. This generalization limits the usability of the map because of selection, scale, spatial, and distortion when transferring information from the earth (a sphere) to a map (flat).

Selection involves the generalization of maps and the inevitable bias that a map has that a photograph does not. A well-made map shows what the map's creator wants to emphasize, and is inevitably biased.

Scale limitations come from the fact that all maps are scaled down. They show large areas on an area that is small enough to view on that map. This process of scaling down causes generalization that increases (loss of detail) as you decrease from the real-life size of the area being viewed on the map. (Note: Smaller the scale of the map gives less detail.)

Spatial limitations are also inevitable in mapmaking. Maps can only accurately show relationships and characteristics that have some sort of spatial component..[2]

What makes maps popular

According to Map Use: Reading, Analysis, and Interpretation, there are four main factors that contribute to the popularity and widespread use of maps.

"1. Maps are convenient to use. They are usually small and flat for ease of storage and handling. Thus, they bring reality into less unwieldy proportion for study.

2. Maps simplify our surroundings. Without them, our world often seems a chaos of unrelated phenomena that we need to organize in order to understand our environment. The section of information found on a map, on the other hand, is clear at a glance. The world becomes intelligible.

3. Maps are credible. They claim to chow how things really are. The coordination between symbol and reality seems so straightforward that we're comfortable letting maps 'stand for' the environment. When we manipulate maps, we expect the results to apply in our surroundings. Maps, even more than the printed word, impress people as authentic. We tend to accept the information on maps without question.

4. Maps have strong visual impact. Maps create a direct, dramatic, and lasting impression of the environment. Their graphic form appeals to our visual sense. It's axiomatic that 'seeing is believing' and 'a picture is worth a thousand words.'"[3]


See also

General
Map design and types
Modern maps
Map history
Related Topics

Footnotes

  1. Jensen, et al., K.L. (June 2004), "Index maps for the digital age", Information Technology and Libraries 23 (2): 81–7 
  2. Tyner, J. A. Principles of Map Design. The Guilford Press. 2010. 10-11.
  3. Kimerling, A. Jon., et al. Map Use: Reading, Analysis, and Interpretation. JP Publications, 2005.

References

  • David Buisseret, ed., Monarchs, Ministers and Maps: The Emergence of Cartography as a Tool of Government in Early Modern Europe. Chicago: University of Chicago Press, 1992, ISBN 0-226-07987-2
  • Denis E. Cosgrove (ed.) Mappings. Reaktion Books, 1999 ISBN 1-86189-021-4
  • Freeman, Herbert, Automated Cartographic Text Placement. White paper.
  • Ahn, J. and Freeman, H., “A program for automatic name placement,” Proc. AUTO-CARTO 6, Ottawa, 1983. 444-455.
  • Freeman, H., “Computer Name Placement,” ch. 29, in Geographical Information Systems, 1, D.J. Maguire, M.F. Goodchild, and D.W. Rhind, John Wiley, New York, 1991, 449-460.
  • Mark Monmonier, How to Lie with Maps, ISBN 0-226-53421-9
  • O'Connor, J.J. and E.F. Robertson, The History of Cartography. Scotland : St. Andrews University, 2002.

External links