Map projections

Map projections: types and distortion

One world. Different ways to show it.

Compare 18 projections. See which preserve area, shapes and angles, then explore their maps.

Compare projection properties
Equal EarthThe same world, a different perspective
01 / Projection atlas

The same world in 18 projections

Choose a map to understand its distortion or try the projection in the interactive lab.

11
Neither equal-area nor conformal

Orthographic projection

It looks like a photograph of the globe from space: only one hemisphere is visible, and areas near the edge of the disk are squeezed hard.

2nd century BCAncient Greeks (used by Hipparchus, among others)

15
Conformal

Spilhaus projection

A square map on which all the oceans form one continuous body of water, while the edges of the square cut through Asia and both Americas.

1979Athelstan Spilhaus (based on Adams' 1925 World in a Square II projection)

16
Neither equal-area nor conformal

Gnomonic projection

Less than a hemisphere is visible, every great circle is a straight line, and scale grows rapidly toward the edge of the view.

6th century BCUnknown; traditionally, though speculatively, attributed to Thales of Miletus

02 / Comparison

Projection property matrix

What does each map preserve, and what does it sacrifice? Every projection and five properties in one table.

  • Preserved

    The property holds. Shapes and angles: locally.

  • Partially

    Only from the centre or along a family of lines. Continuity: at most a hemisphere.

  • Compromise

    Several properties have deliberately moderate distortion.

  • Distorted

    The property does not hold. Continuity: the map is cut into parts.

Scroll sideways to compare every property. Projection names stay in place.

Summary of Map Projection Properties. A comprehensive side-by-side comparison of all projections across their main geometric characteristics.
ProjectionOpen the full guideArearelative sizesShapelocal shapesDistancesroute lengthsAngles and directionslocal anglesContinuitywithout cuts
01Mercator projectionConformalDistortedPreservedDistortedPreservedPreserved
02Robinson projectionCompromiseCompromiseCompromiseCompromiseCompromisePreserved
03Gall-Peters projectionEqual-areaPreservedDistortedDistortedDistortedPreserved
04Mollweide projectionEqual-areaPreservedDistortedDistortedDistortedPreserved
05Winkel Tripel projectionCompromiseCompromiseCompromiseCompromiseCompromisePreserved
06Equal Earth projectionEqual-areaPreservedDistortedDistortedDistortedPreserved
07Peirce quincuncial projectionConformalDistortedPreservedDistortedPreservedPreserved
08Berghaus star projectionEquidistantDistortedDistortedPartiallyPartiallyInterrupted
09August epicycloidal projectionConformalDistortedPreservedDistortedPreservedPreserved
10Plate Carrée (equirectangular) projectionEquidistantDistortedDistortedPartiallyDistortedPreserved
11Orthographic projectionNeither equal-area nor conformalDistortedDistortedDistortedDistortedPartially
12Waterman butterfly projectionCompromiseCompromiseCompromiseCompromiseCompromiseInterrupted
13Dymaxion (Airocean) projectionCompromiseCompromiseCompromiseCompromiseCompromiseInterrupted
14Werner cordiform projectionEqual-areaPreservedDistortedPartiallyDistortedPreserved
15Spilhaus projectionConformalDistortedPreservedDistortedPreservedInterrupted
16Gnomonic projectionNeither equal-area nor conformalDistortedDistortedDistortedDistortedPartially
17Azimuthal equidistant projectionEquidistantDistortedDistortedPartiallyPartiallyPreserved
18Interrupted Goode homolosine projectionEqual-areaPreservedDistortedPartiallyDistortedInterrupted

No flat map preserves every distance. Preserved shapes and angles refer to small areas. Classification is based mainly on the Esri ArcGIS Pro projection documentation.

Take a closer look at two projections side by side
03 / Reading maps

What is a map projection?

A map projection is a mathematical method used to represent the three-dimensional curved surface of the Earth on a flat map plane. Because a sphere cannot be flattened without tearing, stretching, or compressing it, every flat map must contain distortions.

The Cartographer's Trilemma

In 1827, mathematician Carl Friedrich Gauss proved (in his Theorema Egregium) that a sphere cannot be projected onto a flat plane without deformation. Cartographers must choose which of the three main properties to preserve at the expense of others:

Conformal projections

Preserve local angles and shapes. They are vital for navigation (Mercator keeps compass bearings straight), but they strongly distort area, usually most of all far from the map center.

Examples in the catalog: Mercator, Peirce Quincuncial, August Epicycloidal, Spilhaus Projection

Equal-area projections

Preserve the relative sizes of landmasses. Countries have the correct relative surface areas, but their local shapes become heavily stretched or distorted.

Examples in the catalog: Gall-Peters, Mollweide, Equal Earth, Werner Projection, Interrupted Goode Homolosine

Compromise projections

Do not perfectly preserve area or shapes, but instead balance both distortions to produce a natural, visually pleasing map of the world.

Examples in the catalog: Robinson, Winkel Tripel, Waterman Butterfly, Airocean (Dymaxion)

Explore it on a map