Why every world map is wrong - Kayla Wolf

834,060 views ・ 2021-03-29

TED-Ed


Please double-click on the English subtitles below to play the video.

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Fourteen Greenlands could fit in Africa,
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but you wouldn’t guess it from most maps of the world.
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The fact is, every world map humans have ever made is wrong.
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Actually, it’s impossible to make a map of the world 100% right.
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No, not you, globe— we know you’re accurate.
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Not you, Google Earth, you’re just a digital globe.
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We're talking about flat maps, which, let's face it,
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are way more convenient for a lot of things.
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Anyway, as we were saying,
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it’s impossible to make a 100% accurate flat map of a spherical planet.
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For a long time, people didn't even try.
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They just plonked places down in arbitrary locations without any consistent scale.
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Then in 150 AD, the Greek mathematician and astronomer Ptolemy
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systematically mapped the Earth on a grid
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and placed locations on the grid according to coordinates,
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so maps could be checked against others and replicated.
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Ptolemy built his grid out of lines we still use today:
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180 lines of latitude and 360 lines of longitude.
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01:14
In spite of these advances, people kept getting lost.
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Part of the problem was a— shall we say—
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incomplete understanding of the world’s geography.
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But it was also just really difficult to navigate using a map.
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Because the Earth is round,
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the shortest route from one place to another is a path along a circle.
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If we draw this route on a flat map,
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it passes through every line of longitude at a different angle.
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To follow the route, you’d have to constantly shift
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the direction you're traveling.
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Any slight error would land you in the wrong place.
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In 1569, Gerardus Mercator fixed this problem.
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He created a world map proportioned
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so these curved navigational routes would be straight,
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passing through every line of longitude at the same angle
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and therefore allowing navigators to set a constant bearing—
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in other words, travel in one direction— for a whole journey.
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There was just one tiny hitch:
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to do this, he had to distort land masses and bodies of water
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so those furthest from the equator got larger
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and those closest to the equator shrank.
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In spite of its inaccuracies, Mercator’s map was very useful.
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In fact, it’s still widely used today, including in online maps.
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But it’s still wrong!
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In 1925, the Goode Homolosine Projection was created as— get this—
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an interrupted pseudo-cylindrical equal area projection.
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What does that mean? Not important.
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The point was to minimize distortion for the entire world.
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The map can be land-oriented... or ocean-oriented.
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Either way, the so-called orange peel map isn’t very easy to read.
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The Dymaxion Projection by American architect Buckminster Fuller
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in the 1940s is even better.
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Sorry, did we say better?
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It’s not better if you want to understand where things are in the world.
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It is better in the sense that there are no visibly evident distortions
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of the land masses.
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Though if you wanted to know, say, how far Brazil is from Nigeria,
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you won’t get any sense of that from this map.
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The most accurate projection to date is the AuthaGraph World Map
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designed by Japanese architect Hajime Narukawa in 1999.
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The continents and oceans are almost completely in proportion,
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and the map is rectangular, just how we like it.
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Could this be the perfect map?
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Well... no.
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Since the Mercator works for navigation and reads clearly,
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why bother with all these whacky maps?
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Arno Peters argued that by enlarging European and North American countries,
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the Mercator projection gives white nations a sense of supremacy
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over non-white nations closer to the equator.
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He adapted the Gall-Peters Projection, which counteracts that particular problem,
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but the continents are still... stretched.
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Today, we rely on maps less and less for navigation,
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but they still play a vital role in education.
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Peters was definitely on to something:
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no matter what map we’re looking at,
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it’s a story told from the perspective of the map’s creator
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that in turn shapes—perhaps unduly— our perception of our world.
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Simple changes in map design,
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even changes that have nothing to do with how we transfer
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a round Earth to a flat surface, can completely shift our point of view.
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