Classifications
cylindric
perspective
Graticule
Meridians: Equally spaced straight parallel lines.
Parallels: Unequally spaced straight parallel lines, closest near the equator, but spacing increases poleward at a much greater rate than it does on the Mercator. Perpendicular to meridians.
Poles: Cannot be shown.
Symmetry: About any meridian or the equator.
Aspects
Normal is described above. Transverse aspect is called the Wetch projection, since it was discussed by J. Wetch in the early 19th century.
Scale
True along the equator.
Increases with distance from the equator to infinity at the poles.
Changes with direction at any given point, except at the equator, but scale in a given direction is constant at any given latitude or at the latitude of opposite sign.
Distortion
Shape, area, and scale distortion increase rapidly away from the equator, where there is no distortion.
Other features
Projection is produced geometrically by projecting the Earth's surface perspectively from its center onto a cylinder tangent at the equator.
Should not be confused with the Mercator, which is not perspective.
Usage
Distortion is too great for any usage except showing the appearance of the Earth when so projected and contrasting with the Mercator.
Similar projections
Mercator projection, which is not perspective, also cannot show the poles, but the poleward increase in the spacing of the parallels does not occur as rapidly as it does on the Central cylindric projection.
Call and other perspective cylindric projections can be produced by moving the point of perspective away from the center of the Earth. The poles can then be shown.
Gnomonic projection is projected perspectively from the center of the Earth onto a tangent plane rather than a cylinder and is very different in appearance.
Origin
Uncertain
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.