Classification
Geocart menu class: Miscellaneous
Conformal
Graticule
Meridians: Central meridian is straight. Other meridians are curved and concave toward the central meridian.
Parallels: Equator is straight. Other parallels are curved and concave toward the nearest pole.
Poles: Points
Symmetry: About the central meridian or the Equator
Scale
Increases rapidly with distance from the center
Distortion
Great distortion of area toward the 180th meridians in comparison with the center
Other features
Boundary of the world map is a two-cusped epicycloid. Like the Eisenlohr projection, this projection has no “singular” point at which conformality fails. Unlike the Eisenlohr, the map boundary has a varying scale.
Usage
Novelty whole-world maps
Origin
Presented by F. August and G. Bellermann in Germany in 1874
Aspects
Transverse oblique aspect used by Athelstan F. Spilhaus in 1942 to show a map of world oceans
Other names
August
Similar projections
Eisenlohr has a boundary of constant scale.
Van der Grinten IV is not conformal and has circular arcs for meridians and parallels.
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.