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.
The map projection that Cuba uses is equirectangular projection. It shows the equidistant or constant spacing map representation of the country.
A map projection simply is a representation of the round, 3D surface of the earth onto a flat, 2D map. There are different map projections such as Mercator and Robinson each of which have advantages and disadvantages.The appropriate projection for a map depends on the scale of the map and the purposes for which it will be used. For example, a Mercator projection has straight rhumb lines and is therefore excellent for navigation, because compass courses are easy to determine, but there is distortion near the poles.
The Robinson projection shows the entire world map at once.
Polar Area
A map projection that is used for sea travel includes the gnomonic projection. This was most often used to find the shortest routes between points on a sphere.
The Peters map projection was created by German historian Arno Peters in 1973 as an alternative to the traditional Mercator map projection. The Peters map aims to provide a more accurate representation of the relative sizes of land masses by distorting shapes.
Gall-Peters Projection is an item. This item is a table top map projector. Several schools have begun incorporating Gall-Peters Projection into their classrooms.The projector is named after James Gall and Arno Peters.
a map projection is a map that has lots of different angles.
a map projection is a map that has lots of different angles.
a map projection is a map that has lots of different angles.
this map does not have excellent location. please correct me if i am wrong.
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)
Positives of a polar projection map: It accurately represents the area around the poles, making it useful for navigating polar regions. Negatives: Distortion occurs towards the edges of the map, impacting accuracy for equatorial regions. Positives of a Peters projection map: It accurately represents the relative size of landmasses, offering a more equitable view of the world. Negatives: Shapes are distorted, particularly towards the poles, making it less accurate for navigation or land shape representation.
The "Peter Projection" (also called the Gall-Peters projection) has accurate relative areas but distorted shapes. It is is one specialization of a configurable equal-area map projection known as the equal-area cylindric.These projections preserve area:Gall orthographic (also known as Gall-Peters, or Peters, projection)Albers conicLambert azimuthal equal-areaLambert cylindrical equal-areaMollweideHammerBriesemeisterSinusoidalWernerBonneBottomleyGoode's homolosineHobo-DyerCollignonTobler hyperelliptical
The most common method is using a map projection, which mathematically transforms the curved surface of the Earth onto a flat map. Different map projections exist, each with its own way of distorting certain features such as distances, areas, or shapes. Mercator, Peters, and Robinson are examples of popular map projections used to depict the Earth.
A Winkle Tribal map projection is a modified azimuthal map projection. This is one of three projection.
A map projection is a method used to represent the curved surface of the Earth on a flat surface, like a map. Different projections have different properties, which can affect the accuracy of size, shape, distance, or direction of features on the map. Each projection has its own strengths and weaknesses depending on the purpose of the map.