The other popular map projections include the so-called "compromise" projections, including:
Robinson
Winkel Tripel
Dymaxion (Buckminster Fuller)
Butterfly Map (Cahill)
Kavrayskiy
Wagner pseudocylindrical
Chamberlin trimetric
Fine's cordiform
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Map Nation claims to have the best directions. There are many other companies out there as well, including google maps, mapquest, and a variety of others.
A map that preserves both shape and size is known as an equidistant map projection. This type of projection maintains distances accurately, allowing for both shape and scale to be represented correctly. However, it's important to note that while some projections can preserve shape (like conformal projections) or size (like equal-area projections), few can do both simultaneously across the entire map. As a result, equidistant projections often compromise on one of these properties to maintain the other.
Well the Peter's Projection IS a "real map," as you say; or rather, another projection. There are hundreds out there and none are better than any others. It just depends on what you're using it for. The Peter's Projection is just an image of the world that, when it was brought out in 1974, was different than anyone had previously seen, since the Mercator projection in 1596. The Peter's Projection basically is a more accurate version of what you are referring to as a "real map." A Mercator projection shows the shapes of land masses as they appear on a globe, but flattened out, which gives an extremely inaccurate picture of the size of the masses. (For instance, it shows Greenland as being roughly the same size as Africa, when in fact it 14 times smaller!!) The Peter's was created in order to show the true size of land masses, in a more fair representation. It does, however, sacrifice true shape.The best thing you can do is look at images of several projections next to each other so that you can see what I mean.Check out website with URL in related links for Explanation & Guide of the Peters World Map.
Mercator Projection : longitude and latitude as straight, parallel lines Conic Projection : a circular map made from a flattened cone, centered on a pole or other point Gall-Peters Projection : relocates standard parallels, narrows longitudinal spacing Robinson Projection : approximates a true spherical view of the Earth, except the poles Winkel Tripel Projection : an azimuth approximation of the world view, similar to Robinson The most widely used is the Mercator projection, the major disadvantage being its area expansions (areas closer to the poles appear larger and lack their true shapes). The Gall-Peters Projection provides a closer approximation of the relative areas. All flat representations of a spherical surface will create variances in "true" size or shape. (see image links)
Lines of longitude on the Mercator projection are straight and evenly spaced, while on the other two projections (such as the Robinson or Winkel Tripel), they are curved and vary in spacing. This distortion in longitude is a trade-off for maintaining accurate shapes and angles on the Mercator projection.
Compare: Both Mercator and Gnomonic projections are commonly used for nautical purposes, such as routes for ships to take.Contrast: Gnomonic projections usually display a small area of the Earth, whereas a Mercator projection displays the entire Earth, but with distortions at the poles.
Mercator projection distorts the size of land masses, resulting in high distortion near the poles. Equal area projections maintain accurate land area proportions, making them useful for representing data like population density.
The Mercator projection has straight meridians and parallels that intersect at right angles. Scale is true at the equator or at two standard parallels equidistant from the equator. The projection is often used for marine navigation because all straight lines on the map are lines of constant azimuth.
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Mercator Projection : longitude and latitude as straight, parallel lines Conic Projection : a circular map made from a flattened cone, centered on a pole or other point Gall-Peters Projection : relocates standard parallels, narrows longitudinal spacing Robinson Projection : approximates a true spherical view of the Earth, except the poles Winkel Tripel Projection : an azimuth approximation of the world view, similar to Robinson The most widely used is the Mercator projection, the major disadvantage being its area expansions (areas closer to the poles appear larger and lack their true shapes). The Gall-Peters Projection provides a closer approximation of the relative areas. All flat representations of a spherical surface will create variances in "true" size or shape. (see image links)
Equal-area map projections, such as the Mollweide or Gall-Peters projections, are best for comparing the sizes of countries as they accurately represent the relative sizes of land masses. This helps to avoid distortions that can occur in other types of map projections, such as the Mercator projection.
The Mercator projection is commonly used for navigation and general-purpose world maps due to its ability to accurately represent directions. The Gnomonic projection, on the other hand, is often used for navigational purposes like plotting great circle routes or representing shortest paths between two points on a globe.
All map projections put the earth's surface on to a flat sheet, in different ways. For navigation the Mercator projection is very common because a line on a constant compass bearing is shown as a straight line in this projection. Mercator is an example of a conformal projection because the shape of a small feature - like an island - is preserved on the map. Other projections preserve area or direction, but no projection can achieve everything, it's always a compromise.
World map projections vary in their characteristics, primarily in how they represent the Earth's curved surface on a flat plane. Common types include the Mercator projection, which preserves angles but distorts sizes, particularly near the poles; and the Robinson projection, which aims for a more balanced representation of area, shape, and distance, reducing distortion overall. Other projections, like the Peters projection, prioritize area accuracy, leading to significant shape distortion. Each projection serves different purposes, making them useful for various applications in navigation, education, and thematic mapping.
because 2nd and 4th angle projection overlap each other