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In a small area, Earth is essentially flat, so a flat map is accurate. But to represent a larger portion of Earth, map makers must use some type of projection to collapse the third dimension onto a flat surface. A projection is a way to represent the Earth’s curved surface on flat paper.
A globe is the only representation of the earth that does not distort its geometry — except, of course, its size. A systematic transformation of the earth’s surface to a flat map is called a map projection.
On a flat map many of the spatial properties such as size, shape, angular relationships, and distance are compromised in the projection process. A cartographer may be able to preserve one of these attributes but not the others. This means that all flat maps contain some type of distortion.
Size Matters Flattening a three-dimensional globe onto a flat surface isn’t possible without some distortion. Mercator maps distort the shape and relative size of continents, particularly near the poles.
The biggest downfall of the AuthaGraph map is that longitude and latitude lines are no longer a tidy grid. As well, continents on the map are repositioned in a way that will be unfamiliar to a population that is already geographically challenged.
Maps may show visible features, such as rivers and lakes, forests, buildings, and roads. They may also show things that cannot be seen, such as boundaries and temperatures. Most maps are drawn on a flat surface. A map displayed on a round surface is called a globe. The most familiar kinds of maps are topographic and political maps.
One in particular, known as the Mercator projection, distorts the actual sizes of landmasses like Alaska and Greenland and makes them appear larger in comparison to Africa or North America than they are. But why does this happen? As it turns out, depicting the surface of a round planet on a flat sheet of paper is no easy task.
A globe of the Earth would have an error score of 0.0. We found that the best previously known flat map projection for the globe is the Winkel tripel used by the National Geographic Society, with an error score of 4.563.
Inspired by methods used by scientists (like Tissot’s indicatrix method), you will draw same-size circles all over the globe (balloon), create a projection (flat map) and study its distortions. Start by drawing one circle centered on an intersection of the equator and a line of longitude.