Tukuk-OSYou Cannot Flatten a Sphere
Peel an orange in one piece and press the skin flat: it tears or crumples. That is not a manufacturing defect, it is Gauss's theorema egregium — a sphere has curvature that no flat surface shares, so any map of the world drawn on paper must stretch, squeeze or tear somewhere. A map projection is simply a chosen set of rules for where to lie. Pick your favourite property and something else pays for it.
The usual things on offer: shape (conformal — compass angles and small features look right), area (equal-area — countries compare honestly), distance (equidistant — only from one or two chosen points), direction (true bearings from a centre), and straight rhumb lines (constant compass course — navigation gold). You can have two-ish of these at a time; never all of them.
The Mercator Myth, Precisely
Gerardus Mercator's 1569 cylinder projection was built for sailors: any straight line on it is a constant compass bearing, so you rule the line and read the heading off the map. The price is the well-known inflation factor — everything grows like sec(latitude), so near the poles the stretch becomes infinite. Greenland renders at roughly the area of Africa, which is actually about fourteen times larger; the UK appears comparable to Congo. The classic "the world looks like this" classroom map is therefore a map that is excellent at bearings and hopeless at sizes — and it is still the right choice for the phone app navigating you, because tiles are conformal by design: local shapes must look like the ground you are standing on.
Every Projection Is a Political Choice Too
Where you cut the sphere, which pole is up, whether the map is centred on Greenwich, the Pacific or your own capital — none of it is mathematics, all of it is convention. Australia has appeared "upside down" on purpose; South America's size only becomes honest on equal-area maps like Gall–Peters, which then wobbles shapes badly in the mid-latitudes. The honest reaction to any world map is to ask what was preserved here, and what paid for it — the same instinct that makes you check what a statistic was cut to favour.
What Web Maps Actually Do
Slippy online maps (including the one on our route planner) use Web Mercator: the Mercator formula applied as if the Earth were a perfect sphere rather than the slightly squashed WGS84 ellipsoid, introducing up to a few hundred metres of positional error mid-latitude — irrelevant at street zoom, technically a sin to a surveyor. Countries like Finland and Indonesia have real reasons to prefer their own national projections where local distances stay honest; a national grid map of a long thin country is never going to be a global projection.
Try It Yourself
Compare the same two countries — say Norway and Uganda — on a Mercator world map and on an equal-area one, then check their real areas against our World Statistics pages. Or open the maps page, route between two cities on the equator and two near a pole with the same coordinate difference, and watch the driving distance betray the grid you grew up trusting. Once you can see the lie in a projection, you start seeing the chosen lie in every chart, headline and dashboard too.