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Robinson Projection because it has minor distortions, the sizes and shapes near the eastern and western edges of the map are accurate, and outlines of the continents appear much as they do on the globe.
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)
cylindrical projectionhave fun :)
Gerardus Mercator (1512-1594) developed a method (Mercator cylindrical projection) of displaying the Earth's surface (which is curved) as a flat nautical map. On his map of 1569, sailing courses along a fixed bearing appeared as straight lines with the proper angle to the meridians. (But areas nearer the equator appear smaller than similar areas nearer the poles.) This map could not be fully applied to its intended use (sailing) until nearly 200 years later.
prime meridian
The Mercator projection preserves the shape of countries accurately, but distorts their size, especially near the poles. This means that countries near the equator will appear smaller than they actually are on a Mercator map, while those near the poles will appear larger.
Mercator projection represents rhumb lines, which are useful for navigation. It makes the areas near the poles appear very large.
Mercator projection represents rhumb lines, which are useful for navigation. It makes the areas near the poles appear very large.
The Mercator projection is a cylindrical projection, where the meridians are equally spaced vertical lines and the parallels are horizontal lines parallel to the equator. It distorts the size of land masses as they get farther from the equator, making areas like Greenland appear much larger than they actually are.
A cylindrical map projection in which the meridians and parallels of latitude appear as lines crossing at right angles and in which areas appear greater farther from the equator.conic
On a Mercator projection, meridians appear as straight, parallel lines running from top to bottom of the map, spaced evenly apart. This is because the Mercator projection is a cylindrical map projection that preserves straight lines of constant bearing, resulting in meridians being stretched vertically towards the poles.
Robinson Projection because it has minor distortions, the sizes and shapes near the eastern and western edges of the map are accurate, and outlines of the continents appear much as they do on the globe.
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)
The Mercator map was created in 1569 by Gerardus Mercator. The projection's creator wanted to create a map that would be helpful in navigating the world's seas. The map is set up on a useful grid. However, the map is clearly distorted! At the north and south ends of the map, Antarctica and Greenland are just two examples of landforms that appear far bigger than they should. Areas and distances are not portrayed accurately on this 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)
cylindrical projectionhave fun :)
The Robinson projection map shows the shapes of the continents more accurately than the Mercator projection map, but both distort the sizes of landmasses, making areas near the poles appear larger than they are. Waterways and continents are more accurately depicted in size and shape on specialized maps like the Winkel Tripel projection, which aims to balance size and shape distortions.