The equidistant conic projection is a conic map projection commonly used for maps of small countries as well as for larger regions such as the continental United States that are elongated east-to-west.

Also known as the simple conic projection, a rudimentary version was described during the 2nd century CE by the Greek astronomer and geographer Ptolemy in his work Geography.

The projection has the useful property that distances along the meridians are proportionately correct, and distances are also correct along two standard parallels that the mapmaker has chosen. The two standard parallels are also free of distortion.

For maps of regions elongated east-to-west (such as the continental United States) the standard parallels are chosen to be about a sixth of the way inside the northern and southern limits of interest. This way distortion is minimized throughout the region of interest.

Coordinates from a spherical datum can be transformed to an equidistant conic projection with rectangular coordinates by using the following formulas, where λ is the longitude, λ₀ the reference longitude, φ the latitude, φ₀ the reference latitude, and φ₁ and φ₂ the standard parallels:

where

Constants n, G, and ρ₀ need only be determined once for the entire map. If one standard parallel is used (i.e. φ₁ = φ₂), the formula for n above is indeterminate, but then

The reference point (λ₀, φ₀) with longitude λ₀ and latitude φ₀, transforms to the x,y origin at (0,0) in the rectangular coordinate system.