Gall-Peters projection

Equal-areaCylindricalCreator: James Gall / Arno PetersYear: 1855 / 1973

Gall-Peters answers the question Mercator ignores: how much area do countries and continents truly occupy? It preserves area more faithfully, but pays for that fairness with strongly stretched shapes.

Projection guide

A map of fair area and uncomfortable shapes

The main value of Gall-Peters is that Africa, South America, and South Asia regain visual weight. Global South countries stop looking like side notes to the northern hemisphere. That is why the projection became a symbol in the debate over whether maps can reinforce political views of the world.

At the same time, it is not visually comfortable. Equatorial countries look vertically stretched, while areas closer to the poles are flattened. In return, you get a fairer answer about area, but a worse answer about natural shape.

Global Cartographic Grid

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Distortion Properties

PropertyCharacteristic
Area
PreservedPreserved (equal-area projection)
Shape
DistortedSeverely distorted: stretched north to south between the 45° parallels and east to west beyond them, toward the poles
Distances
DistortedDistorted; scale is true only along the 45° N and S standard parallels
Angles and directions
DistortedDistorted (not conformal)
Continuity
PreservedPreserved

History & Origin

First described by James Gall in 1855, and independently popularized in 1973 by German historian Arno Peters. Peters promoted it as a politically fair alternative to Mercator, correctly portraying the size of Global South countries.

Applications

Education, humanitarian agencies (like UNESCO), and publications advocating for geographic equality of developing nations. Esri's documentation advises against cylindrical equal-area projections for whole-world maps, because they badly distort shapes near the poles.

How to read this map

This map is like a scale: it is not meant to look elegant, but to weigh continents more fairly. If something looks thin or flattened, check the area, not the silhouette.

  • Areas are much more fairly comparable than in Mercator.
  • Equatorial countries can look unnaturally tall.
  • Shapes near the poles become horizontally compressed.
  • It works well for global data measured per square kilometer.

What you gain and lose

Gall-Peters preserves area but gives up natural appearance. It is a strong example of a map that can be mathematically fairer while feeling less intuitive.

Best for

Thematic area maps, education about the Global South, and discussions of geopolitical perception.

Avoid for

Navigation, visually polished wall atlases, and country-shape analysis.

Not sure this projection fits your map? Answer three questions in the finder →

Want to see it next to another projection? Compare: Gall-Peters vs Mercator →

Facts worth remembering

  • The projection was promoted as a political alternative to Mercator in the twentieth century.
  • It is equal-area, so countries with the same area should occupy similar visual size.
  • Its controversy shows that mathematical correctness does not always mean comfortable reading.

The best internal links are the ones that help you think. These projections show different answers to the same problem: how to flatten a sphere.

Keep reading about maps that reshape intuition

Frequently Asked Questions

It is used for equal-area presentations showing the true relative sizes of countries (e.g., highlighting that Africa is dramatically larger than Europe).

It must not be used for navigation, local maps, or surveying. Due to extreme angular distortion, country outlines are severely warped.

Equatorial countries (like DRC, Indonesia, and Brazil) which look vertically stretched, and polar nations (like Canada and Russia) which are heavily compressed horizontally.

Countries near the 45° N and S parallels, along which the projection has no distortion (such as France, Italy, Romania, and the northern United States, and in the south New Zealand and Patagonia).

To maintain equal areas on a rectangular grid, this cylindrical projection must stretch shapes vertically near the equator and compress them horizontally near the poles.