How to use it
- Choose a country and press Add.
- Drag the shape across the map. It shrinks towards the equator and grows towards the poles.
- Add more countries to compare them. Read the real areas in the table.
5 practical uses
- Show a class the distortion of the Mercator map.
- Compare the real size of countries for an article or a slide.
- Settle how big Greenland, Australia or Alaska really is.
- Judge the scale of a country you are about to travel across.
- Illustrate a post about map projections.
The maths behind it
The Mercator projection scales the map by the secant of the latitude, sec φ = 1/cos φ, so at 60° everything is drawn twice as large and at 80° nearly six times. To move a country, each vertex is stored as its bearing and great-circle distance from the country's centroid, and re-placed from the new centroid with the direct geodesic formula, which keeps the true size and shape to within the change in convergence of the meridians.
Why maps lie about size
The Mercator projection, which every web map uses, keeps angles right (so north is always up and a compass course is a straight line) at the cost of size: scale grows with the secant of the latitude, so at 60° everything is twice as wide and twice as tall as at the equator, four times the area. Greenland at 72°N looks the size of Africa; in truth Africa is 14 times larger. This tool moves each vertex of the shape by its bearing and distance from the shape's centre, which keeps the true size and near enough the true shape.