PTE · Reading & Writing: Fill in the Blanks

Principles of Map Projections

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1

The Mercator Projection and Navigation

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Developed during the sixteenth century primarily for nautical navigation, the Mercator projection represents lines of constant compass bearing, known as rhumb lines, as straight line segments. This specific mathematical characteristic allows mariners to plot a straightforward course across vast oceans without having to recalculate bearings continuously. However, because the spacing between parallels of latitude increases exponentially towards the polar regions, the projection exaggerates the surface area of landmasses situated in high latitudes. Greenland, for instance, appears roughly comparable in size to the African continent, the latter landmass is in reality more than twelve times larger. While such geometric distortion has attracted enduring criticism regarding geographic bias, the projection remains uniquely for marine charting and contemporary digital tile mapping. Cartographers therefore must carefully distinguish between conformal models that preserve local angular relationships and those designed to true relative proportions across the global surface.

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2

Compromise Projections in Atlases

Because no flat map can depict the spherical Earth without introducing some mathematical error, cartographers frequently turn to compromise projections for general reference atlases. Unlike conformal or equal-area formulations, these hybrid designs do not 1 preserve any single geometric property perfectly. Instead, they seek a balanced visual compromise, 2 distributing errors among shape, area, scale, and direction so that none of these elements becomes excessively deformed. The Robinson projection, introduced in the mid-twentieth century, achieved widespread popularity by curving the meridians inward to create an aesthetically pleasing oval boundary, thereby 3 the extreme polar inflation typical of rectangular grids. Later, geographic societies favoured the Winkel Tripel projection, which minimises the combined sum of three distinct types of distortion. Although compromise projections are unsuitable for precise navigational calculations or scientific measurement, their visually balanced presentation makes them ideal for 4 broad spatial patterns. They demonstrate that cartographic design often entails managing unavoidable trade-offs 5 than striving for unattainable geometric perfection.

  • Gap 1:barely · vaguely · rigidly · narrowly
  • Gap 2:hastily · fiercely · reluctantly · evenly
  • Gap 3:curbing · neglecting · prolonging · amplifying
  • Gap 4:illustrating · concealing · disrupting · forging
  • Gap 5:further · better · rather · other
3

Azimuthal Projections and Great Circles

Azimuthal projections are generated by mathematically projecting the surface of the terrestrial sphere onto a flat, tangent or secant plane. In this family of maps, all points preserve accurate directions, or azimuths, relative to the central point of 1. When centred directly over one of the poles, the projection arranges parallels of latitude as concentric circles and meridians as straight lines radiating outward like wheel spokes. A primary advantage of the gnomonic azimuthal variant is that all great circle paths—the shortest distance between any two locations on Earth—are depicted as straight lines. This unique attribute makes planar charts 2 for long-distance aviation planning and polar navigation, where standard nautical charts prove impractical. Nevertheless, distortion increases 3 with distance from the central contact point, causing peripheral continents to appear heavily sheared or magnified. Users of azimuthal maps must therefore remain conscious of these perimeter distortions, 4 that accurate distance and bearing measurements apply only along lines extending directly through the projection's central 5.

  • Gap 1:velocity · gravity · tangency · fluctuation
  • Gap 2:hazardous · redundant · indispensable · superfluous
  • Gap 3:scarcely · rapidly · tardily · evenly
  • Gap 4:denying · demanding · refuting · recognising
  • Gap 5:origin · orbit · outpost · barrier
4

Conic Projections for Regional Mapping

Conic projections are constructed by conceptually placing a cone over the globe, typically touching the surface along one or two standard parallels of latitude. Because distortion is minimal along these standard lines, conic projections are exceptionally well suited for mapping mid-latitude landmasses that extend predominantly from east to west. In a secant conic model, the cone intersects the sphere at two distinct latitudes, thereby 1 distortion across the intermediate zone between them. For instance, national geological surveys and topographic agencies often rely on the Lambert conformal conic projection to produce regional aeronautical charts, as it retains correct local shapes and bearings with high 2. Alternatively, the Albers equal-area conic projection is widely employed when accurate area calculations are 3 for demographic or environmental inventories across broad continental expanses. However, because distortion escalates rapidly away from the standard parallels, conic projections are rarely used for complete world maps. Instead, cartographers 4 their use to regional frameworks where mid-latitude precision can be maintained without introducing 5 peripheral deformities.

  • Gap 1:accelerating · constraining · originating · complicating
  • Gap 2:ambiguity · precision · reluctance · leniency
  • Gap 3:essential · detrimental · nominal · incidental
  • Gap 4:restrict · expand · abandon · dismiss
  • Gap 5:negligible · unacceptable · favourable · impeccable

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