Parameters: Latitude of origin, Standard parallel 1, Standard parallel 2
Geocart menu class: Conic
Neither conformal nor equal area
Meridians: Equally spaced straight lines converging at a common point, which is one of the poles. The angles between them are less than the true angles.
Parallels: Unequally spaced concentric circular arcs centered on the pole of convergence of the meridians. The meridians are therefore radii of the circular arcs. Spacing of parallels increases away from the central latitudes.
Poles: One pole is a point; the other pole cannot generally be shown, but, under some conditions, it is a circular arc
Symmetry: About any meridian
True along one or two chosen standard parallels, which may be on the same side of or both sides of the Equator
Scale is constant along any given parallel.
Free of distortion only along the one or two standard parallels. Distortion is constant along any given parallel but changes more rapidly in a north-south direction than it does on conformal or equal-area conics, and the Perspective Conic has no compensating advantage. Other projections should be used instead.
Projection is produced geometrically by projecting the Earth perspectively from the center (or from some other point) onto a cone tangent or secant along the standard parallels.
Polar Gnomonic projection, if the pole is the single standard parallel. The cone of projection thereby becomes a plane. Central Cylindrical projection, if the Equator is the single standard parallel. The cone of projection thereby becomes a cylinder. Standard conic formulas must be rewritten.
A stereographic perspective conic was presented by Carl Braun in 1867. The map is projected from the South Pole onto a cone tangent at latitude 30° N.
Description adapted from J.P. Snyder and P.M. Voxland, An Album of Map Projections, U.S. Geological Survey Professional Paper 1453. United States Government Printing Office: 1989.