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Equidistant conic projection is a type of conic projection that projects the Earth onto a conical surface and displays it as a map. It is characterized by keeping the intervals between meridians and parallels constant. In particular, it is designed to minimize distortion of distance along one or two parallels called standard parallels.
In this projection, meridians are drawn as straight lines radiating from the apex of the cone, and parallels are drawn as concentric circular arcs. It is often used for creating maps on a national or continental scale, as it can display large areas on Earth (mainly in the east-west direction) relatively accurately.
Although the equidistant conic projection cannot perfectly maintain area, shape, and direction, it is suitable for situations where the accuracy of distances in a specific latitude band is important. It is particularly suitable for maps of mid-latitude regions that extend east to west (e.g., North America, Japan, China, etc.), and is often used for educational atlases, geographical materials, administrative planning maps, etc.
The equidistant conic projection is particularly suitable for mapping wide areas located in the mid-latitudes. For example, it is often used for maps that cover a wide area in the east-west direction, such as the entirety of Japan, the United States, and China, and is used in fields where distance is important, such as weather maps, administrative district maps, temperature distribution maps, and road planning maps. It is also suitable for measuring distances on maps and planning routes, and is widely adopted as a projection that combines readability and practicality.
1. Equidistant conic projection.

2. Shows an equidistant or simple conic projection with standard parallels located in the Northern (left) and Southern (right) Hemispheres.

Transverse Mercator Projection
Longitude / Latitude Projection