Geocart menu class: Pseudocylindric
Equally spaced parallels
Meridians: Central meridian is a straight line half as long as the Equator. Other meridians are equally spaced sinusoidal curves intersecting at the poles and concave toward the central meridian.
Parallels: Equally spaced straight parallel lines perpendicular to the central meridian
Symmetry: About the central meridian or the Equator
True along every parallel and along the central meridian
Severe near outer meridians at high latitudes but can be substantially reduced by interruption with several central meridians. Free of distortion along the Equator and along the central meridian.
Atlas maps of South America and Africa. Occasionally used for world maps. Formerly used for other continental maps and star maps. Combined with Mollweide projection to develop other projections such as the Homolosine and the Boggs.
Developed in the 16th century. Used by J. Cossin in 1570 and by J. Hondius in Mercator atlases of the early 17th century. Often called Sanson-Flamsteed projection after later users. Oldest current pseudocylindrical projection.
For educational purposes, it has been shown in various aspects as examples of normal, transverse, and oblique aspects of almost any pseudocylindrical projection.
Several other pseudocylindrical projections, such as Craster Parabolic and Boggs Eumorphic, are very similar, but parallels are not equally spaced, and meridians are curved differently. Eckert V and VI have sinusoidal meridians but have lines for poles.
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.