OtterKnow Kids Encyclopedia

Globes and Map Projections

What Is a Globe?

A globe is a spherical model of Earth that shows the shapes, sizes, and positions of continents and oceans as accurately as possible. Because Earth is shaped like a sphere (technically a slightly squashed sphere called an oblate spheroid), a globe is the most accurate way to represent our planet. Globes show the correct relative sizes of continents, the true distances between places, and the proper shapes of landmasses. The first known globe was created in 1492 by a German mapmaker named Martin Behaim, just before Christopher Columbus sailed to the Americas. Today, globes are common tools in classrooms and libraries around the world.

The Problem with Flat Maps

Here is the big challenge mapmakers face: Earth is round, but maps are flat. Try peeling an orange and pressing the peel flat on a table, and you will see the problem. The peel tears, stretches, and distorts because a curved surface cannot be made perfectly flat. Cartographers, the people who make maps, run into the same issue when they try to show the round Earth on a flat piece of paper. Every flat map must distort something, whether it is the size of countries, their shapes, the distances between them, or the directions from one place to another. No flat map can get all of these things right at the same time.

What Are Map Projections?

A map projection is a mathematical method for transferring information from Earth’s curved surface onto a flat map. Think of it like shining a light through a clear globe onto a piece of paper. Depending on how you hold the paper and where the light is, the shadows will look different. There are hundreds of different map projections, and each one makes different trade-offs about what it keeps accurate and what it distorts. Cartographers choose a projection based on what the map will be used for, whether that is navigating the ocean, measuring land area, or showing the whole world at a glance.

The Mercator Projection

The Mercator projection is one of the most famous and widely used map projections in history. It was created in 1569 by the Flemish cartographer Gerardus Mercator to help sailors navigate the oceans. The Mercator projection keeps shapes and directions accurate, which made it perfect for plotting straight-line courses across the sea. However, it has a major drawback: it dramatically stretches areas near the North and South Poles. On a Mercator map, Greenland looks almost as big as Africa, even though Africa is actually about 14 times larger. Despite this distortion, the Mercator projection is still used in many classrooms and on websites like Google Maps for street-level navigation.

Other Important Projections

Cartographers have developed many other projections to solve different problems. The Robinson projection, created by Arthur Robinson in 1963, was designed to make the whole world look “right” to the eye by compromising on all types of distortion rather than eliminating just one. The Peters projection (also called the Gall-Peters projection) shows countries at their correct relative sizes, which means shapes look stretched but areas are accurate. The azimuthal equidistant projection shows true distances from the center point, which is why it appears on the United Nations flag. Each projection is like a different tool in a toolbox, useful for specific jobs but not perfect for everything.

Latitude and Longitude

Globes and maps both use a grid system of imaginary lines to help locate places on Earth. Lines of latitude run east to west and measure how far north or south a place is from the equator, which sits at 0 degrees latitude. Lines of longitude run north to south and measure how far east or west a place is from the Prime Meridian, which passes through Greenwich, England, at 0 degrees longitude. Together, latitude and longitude create a coordinate system that can pinpoint any location on Earth. For example, New York City is located at about 40.7 degrees north latitude and 74 degrees west longitude.

How Globes and Maps Are Used Today

Modern technology has transformed how we use globes and maps. Digital globes like Google Earth allow people to zoom in on any place on the planet using satellite imagery, seeing everything from mountain ranges to individual buildings. GPS (Global Positioning System) satellites orbiting Earth use coordinate systems based on latitude and longitude to help people navigate with pinpoint precision. Scientists use specialized map projections to study climate change, track animal migrations, and plan disaster responses. Even though we have powerful digital tools, physical globes and paper maps remain valuable because they do not need batteries or an internet connection to work.

Why Map Projections Matter

Understanding map projections helps us become smarter readers of maps and better thinkers about the world. When you know that every flat map distorts reality in some way, you can ask important questions about the maps you see. A map that makes one country look huge might make another look tiny, which can shape how people think about the importance of different parts of the world. The Mercator projection, for example, has been criticized for making countries in Europe and North America appear larger than they really are compared to countries near the equator in Africa and South America. Learning about projections reminds us to think critically about how information is presented and to look for more than one way to understand the world around us.