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The Robinson projection is a map projection of a world map that shows the entire world at once. It was specifically created in an attempt to find a good compromise to the problem of readily showing the whole globe as a flat image.
This map projection, also known as a compromise, presents an entire view of the globe’s surface at once. Unlike most map projections, the Robinson projection is neither constructed using any mathematical formula nor drawn to scale and was constructed to show a pleasing image of the entire globe.
The Robinson projection is basically secant, with lines of tangency running along the 38° 0′ 0″N and 38° 0′ 0″S lines of latitude. Robinson projections have normal aspects. Robinson projections differ from one another in the locations of their central meridians. Distortions.
The primary purpose of the Robinson projection is to create a visually appealing map of the entire world. Because it is a compromise visualization, it does not eliminate every type of distortion. The goal is to keep the levels of all distortions relatively low over the majority of the map.
The Robinson Projection is a map projection designed to create a visually appealing representation of the entire world while minimizing distortion in size, shape, distance, and direction.
In 1961, Arthur H. Robinson created the Robinson Projection, which was designed more to make global maps “look correct” than to exactly measure anything. Many popular maps, including those from the National Geographic Society and the Rand McNally series, have utilized this now-common projection.
The Robinson projection is known for its ability to create visually appealing maps of the entire world. Unlike some other map projections, the Robinson projection aims to minimize distortion rather than eliminate it entirely.
Robinson Projection. This attempt at creating a faithful world map took a similar tack to the Sinusoidal by pulling out the edges of the map to mimic a sphere. The Robinson isn’t as extreme, however, taking the form of a much more gentle oval.
The Robinson projection, developed by cartographer Arthur H. Robinson in 1963, represents a major advancement in map-making. This projection is widely recognized for its aesthetic appeal. It is effective in balancing the various distortions inherent in mapping the globe onto a flat surface.
The Robinson Projection is a compromise between accuracy and the readability of the map on a flat surface. It shows the poles as lines, which accurately shows the high altitude lands and water to land ratio.