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Nicolosi Globular Projection is a pseudocylindrical compromise world map projection introduced by the Italian cartographer Giambattista Nicolosi in 1660. It is one of the best-known early globular projections and was widely used before modern mathematical projections became standard. The projection represents the world in a rounded form and was valued for its visually balanced appearance. It is neither equal-area nor conformal, and today it is mainly of historical interest.
The Nicolosi Globular Projection has the following main characteristics:
The Nicolosi Globular Projection is mainly used in historical cartography, educational materials on map history, and decorative map design. It is useful when the goal is to present a traditional rounded world image or to illustrate pre-modern approaches to global mapping. However, for modern practical mapping, atlas production, or spatial analysis, it is rarely chosen because more accurate and functional projections are available.
1. Hemispheres on the Nicolosi globular projection. 15° graticule, 115°W and 65°E central meridians. Imagery is a derivative of NASA's Blue Marble summer month composite with oceans lightened to enhance legibility and contrast. Image created with the Geocart map projection software.

2. Nicolosi globular projection distortion. Deeper tint means more distortion. Neutral color means distortion is balanced between angular deformation and areal inflation. Tissot indicatrix at 15° intervals.
Vertical Near-side Perspective Projection
Two-point Equidistant Projection