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The Dymaxion map projection, also called the Fuller projection, is a kind of polyhedral map projection of the Earth's surface onto the unfolded net of an icosahedron.The resulting map is heavily interrupted in order to reduce shape and size distortion compared to other world maps, but the interruptions are chosen to lie in the ocean.
Dymaxion is a term coined by architect and inventor Buckminster Fuller and associated with much of his work—prominently his Dymaxion house and Dymaxion car. Dymaxion, a portmanteau of the words dy namic , max imum , and tens ion ; [ 1 ] sums up the goal of his study, "maximum gain of advantage from minimal energy input."
Buckminster Fuller's Dymaxion map. A polyhedral map projection is a map projection based on a spherical polyhedron. Typically, the polyhedron is overlaid on the globe, and each face of the polyhedron is transformed to a polygon or other shape in the plane. The best-known polyhedral map projection is Buckminster Fuller's Dymaxion map.
Fuller, along with co-cartographer Shoji Sadao, also designed an alternative projection map, called the Dymaxion map. This was designed to show Earth's continents with minimum distortion when projected or printed on a flat surface.
Dymaxion map: Polyhedral Compromise Buckminster Fuller: Also known as a Fuller Projection. 1999 AuthaGraph projection: Polyhedral Compromise Hajime Narukawa: Approximately equal-area. Tessellates. 2008 Myriahedral projections: Polyhedral Equal-area Jarke J. van Wijk: Projects the globe onto a myriahedron: a polyhedron with a very large number ...
The Dymaxion car, c. 1933, artist Diego Rivera shown entering the car, carrying coat. The Dymaxion car was designed by American inventor Buckminster Fuller during the Great Depression and featured prominently at Chicago's 1933/1934 World's Fair. [1]
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More generally, any mapping onto polyhedral faces becomes an interrupted map when laid flat. Buckminster Fuller proposed his "dymaxion" map in 1943, using a modified icosahedral interruption scheme to divide the oceans up in a way that shows the continents in a nearly continuous mass as "one island". [4]