
Korthistorier
Udforsk arealer, projektioner og grænsedata og prøv dem på kortet.
Åbn kortet →Hvorfor ser Grønland så stort ud?
Mercatorkort strækker områder nær polerne. Derfor ser Grønland for stort ud i forhold til lande nær ækvator. Sammenlign Grønland og Australien på Equal Earth. Et kort, der er nyttigt til navigation, er ikke nødvendigvis godt til at sammenligne arealer.
Læs historien →Hvad bevarer Equal Earth?
Når en kugle gøres flad, ændres noget. Equal Earth bevarer relative arealer, men ikke alle former, afstande og retninger. På globussens kant presses former sammen. Vælg den visning, der passer til dit spørgsmål.
Læs historien →Hvorfor varierer grænser og arealer?
Forenkling af kort udelader små bugter og øer. Vi bruger Natural Earth-grænser i målestok 1:110 millioner og beregner arealer fra forenklede kugleformer. Officielle tal kan medregne vand og territorier anderledes. ≈ betyder et skøn.
Læs historien →Africa is bigger than the map in your memory
The equator crosses Africa, but familiar rectangular maps give northern regions extra space. Compare Africa with countries you know to get a sense of its size.
Læs historien →Russia and Africa: width is not area
Russia stretches across the top of many world maps. Compare that visual width with area, and learn why a country and a continent need different labels.
Læs historien →Japan and Germany: a long shape can hide a similar area
An island chain and a compact mainland country look very different. Compare area without confusing the sea between islands with land.
Læs historien →Why online maps stop before the poles
Square tiles make a world map easy to zoom, but Mercator cannot place the poles at a finite height. Learn what the missing polar strip means.
Læs historien →Why a country looks smaller at the globe’s edge
A globe avoids the familiar rectangular world, but its screen image still compresses the edge. Separate spherical area from visible footprint.
Læs historien →Why the shortest flight looks curved on a map
A straight line on the screen need not be the shortest path around Earth. Compare great-circle paths with compass bearings, and see what a route illustration can tell you.
Læs historien →The map edge is not the International Date Line
Longitude wraps around, a flat map has a seam, and calendar dates have a boundary. These three ideas are related but not identical.
Læs historien →Antarctica is a continent, not the bottom border
A stretched southern strip can hide the shape of a whole continent. Compare Antarctica on Mercator, Equal Earth and a polar globe view.
Læs historien →Pangaea was not there at the start of every timeline
At 600 million years ago, Pangaea had not yet assembled. Follow separated landmasses as they come together and later drift apart.
Læs historien →Five questions before sharing a “true world map”
Projection, zoom, viewpoint, source detail and the meaning of area all affect how you read a map. Check these before sharing a comparison screenshot.
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