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A map made by cylindrical projection appears rectangular in shape. This is because the Earth's surface is projected onto a cylinder positioned over the globe, resulting in distortion towards the poles.
The three main types of map projections are cylindrical, conic, and azimuthal. Cylindrical projections show the Earth's surface on a cylinder, conic projections project the Earth's surface onto a cone, and azimuthal projections project the Earth's surface onto a plane. Each type has variations that can result in different map distortions.
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.
A map with parallel meridians is called a conic projection map. This type of projection is often used for mapping smaller regions or countries, as it maintains accurate shapes and angles near the standard lines of latitude.
Map projection is a technique used to represent the three-dimensional surface of the Earth onto a two-dimensional map. This helps to minimize distortion of the Earth's features such as shape, area, distance, and direction when mapping different regions.
Geographers can use a projection method that minimizes distortion, such as the Lambert cylindrical equal-area projection. They can also represent Greenland in a non-standard orientation to better convey its true size and shape. Additionally, including a note or disclaimer explaining the limitations of the map's representation of Greenland can help mitigate misunderstandings.
The Mercator system is a cylindrical map projection. It is essentially the shape of globe on a flat surface. It was first designed by mapmaker Gerardus Mercator in 1569.
cylindrical projection
Mercator is not a map, but a map projection, i.e. a way of representing the continents on a map. The Mercator projection is only accurate between 30 degrees north and south latitude. The further away you go from that point, the greater the exaggeration.
A Mercator projection map is a cylindrical map presented on a flat surface. It was first presented to the world by Gerardus Mercator in 1569.
Three projection methods used by geographers and map makers are: cylindrical conic planar.
actually, we don't have any idea about this because our teacher, florentino morales jr didn't taught us what is this stuff!
Two other projection methods used by geographers and mapmakers are the azimuthal projection, which displays the Earth's surface with a single point from a specific location as the central point, and the conic projection, which projects the Earth's surface onto a cone wrapped around it. Each of these methods has strengths and weaknesses depending on the purpose of the map being created.
Cylindrical
A map with parallel meridians is called a conic projection map. This type of projection is often used for mapping smaller regions or countries, as it maintains accurate shapes and angles near the standard lines of latitude.
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)
Because of distortion
It is the Mercator.