
By the end you can
- Explain what a map is for, and what mapmakers decide before they draw one.
- Name the common map types and the four families of projection.
- Use latitude and longitude, including the special lines, to find a place.
Unit 1 Β· Introduction to Geography Β· Lesson 1.3 The Map Case

By the end you can
This lesson uses words like projection, meridian, and hierarchy. You do not need to have made a map before. Open this if flattening a globe still feels confusing.
You already use maps. This lesson names the choices inside them. A map is a picture. It leaves most of the real world out on purpose. The Earth is round and paper is flat, so every world map stretches something. Latitude is how far north or south. Longitude is how far east or west. The rest of the lesson is vocabulary for those facts.
Look out a window. Then look at a map of the same street. The window has weather, people, and the color of a car. The map dropped those things so you could see the street. That choosing is cartography.
Peel an orange and press the peel onto a table. It rips or it bunches up. Every world map is that peel. The different ways of flattening it are called projections.
Latitude is north or south of the equator (the middle belt, 0Β°). Longitude is east or west of the prime meridian (the chosen zero line, through Greenwich). A point is where one latitude line crosses one longitude line. The course example: 30Β° N, 90Β° W is New Orleans.
The tropics sit at about 23.5Β° north and south. That is where the sun can be straight overhead. The polar circles sit at about 66.5Β° north and south. That is where you can get a 24-hour day or a 24-hour night. You do not have to love astronomy. You do have to put the northern names north of the equator, and the southern names south.
Why all world maps are wrong β Vox β About six minutes. Shows why a globe cannot become a flat map without stretching something. Your lesson calls that a projection. Skip any extra names you have not learned yet.
Someone shows you a world map where Greenland looks as big as Africa. What went wrong, the globe, or the picture of the globe?
The picture. Africa is about 14 times the area of Greenland (the course numbers: about 11.7 million square miles vs about 836,000). A cylindrical map stretched the land near the poles. The Earth did not change.
Got it now? Scroll back up and re-read the section β it should land differently.
Try this. Look out a window. Then look up the same street on a map.
The window is full of extra information: weather, people, the color of a neighbor's car. A map leaves most of that out so you can focus on what you need. A map can also show things the window never will: country borders, history, how many people live there.
That is the whole point of this study. A map is a picture of the world. Nothing more, and nothing less. Cartography is the name for making those pictures.
The slide show on page 2 is the same four questions you already met in 1.2.2. Making a map is visual communication, so the mapmaker has to know the answers.
1. What is the goal? Is this map just to show where things are, or is it trying to change how people feel? One example in the lesson is a map made to raise awareness about AIDS in Africa.
2. Who will read it? A map for experts is set up differently from a map for a textbook or a news magazine.
3. Where will it be used? A classroom wall, a pamphlet, a magazine, an atlas. The place changes both the look and what fits.
4. What data and tools are available? Mapmakers do not have unlimited time or money. The last slide is a map made in a few minutes with a website, a printer, and a highlighter.

Your study sheet asks what a mapmaker means by these two words. They are design rules. They are about how the map looks, not about politics.
The Mount Olympus animation walks through the parts in the order you should use them.
β’ Title β "Physical Geography" tells you this map is about land, not countries.
β’ Legend β colors for elevation (how high the land is). Dark brown is highest (5,000β10,000 feet), so Olympus must be a mountain.
β’ Scale β how far from Nicosia to Olympus.
β’ Compass β Nicosia is northeast of Olympus.
Then the lesson gives you a U.S. precipitation map (average rainfall and snowfall, 1961β1990) so you can practice. Same four tools: title, legend, scale, compass.
Your study sheet asks you to describe each of these. The page-8 slide show is the source.
β’ Physical maps β landforms and water.
β’ Political maps β human boundaries: countries, states, cities.
β’ Topographic maps β the shape of the land, usually with contour lines.
β’ Thematic maps β one theme (climate, population, rainfall). The precipitation map on page 7 is this kind.
β’ Cartograms β places resized by a number, not by land area. Size might mean people, money, or votes.
β’ Special purpose maps β built for one job: roads, weather, trails.
Picking the right map for the job is itself a map-reading skill. A world map will not get you from James Street to Washington Avenue. Lesson 1.3.5 will call that validity: did the map do the job it was made for?

The Earth is round. Paper is flat. The lesson uses an orange to show the problem. A photo of an orange leaves out the back. Peeling it and laying it flat makes the peel try to spring back. Tearing it into a square is even more misleading.
Mapmakers meet that problem with a map projection: a method for drawing the curved Earth on a flat page. The animation's picture is a glass globe with a light in the center. Land painted on the globe casts shadows onto a surface. Real mapmakers use math, not lightbulbs, but the idea is the same.
There is no perfect projection. The lesson's example: on a common rectangular map, Greenland looks as big as Africa. In reality Africa is about 11,668,545 square miles and Greenland is about 836,109. Africa is about fourteen times bigger. The scale grid on that map is how you correct the visual lie: one inch at the top of the map stands for fewer miles than one inch in the middle.

The study sheet asks you to describe each family and give a benefit and a drawback. The animation on page 11 gives planar and cylindrical in full. Conical and compromise are on the study sheet.
β’ Planar β shadows onto a flat wall. Benefit: good for one hemisphere, especially looking down on a pole. Drawback: leaves out the half of the globe pointing the other way.
β’ Cylindrical β paper wrapped around the globe as a tube, then unrolled. Benefit: the whole world on one sheet; useful for navigation. Drawback: stretches area near the poles (that Greenland trick).
β’ Conical β a cone over the globe. Benefit: lowest stretching in the mid-latitudes the cone was fitted to. Drawback: worse as you move away from that band; not a natural whole-world view.
β’ Compromise β stretches a little of everything so nothing is extreme. Robinson-style oval world maps live here. Benefit: looks right for a wall map. Drawback: no single property (area, shape, distance, direction) is perfectly true.
The lesson's conclusion: there is a place in the world for nearly every projection. The best one depends on the purpose of the map.

Four names. Each one is a different way to flatten the globe onto paper.
Imagine a light in the middle of a glass globe, and a flat wall next to it. The shadows make a map of one half of the Earth. Polar maps work this way. The back of the planet is missing.
Wrap the paper around the globe, then unroll it. You get the whole world. Land near the poles stretches. Greenland looks huge.
Set a cone on the globe, then unroll it into a fan. It is most accurate in the middle latitudes the cone was fitted to, like much of the United States.
Change a bit of everything so nothing looks extreme. The oval Robinson-style world maps live here. They look like the Earth you have in your head, but no one measurement is perfect.
You need a map of Arctic shipping routes, looking down on the North Pole. Which family?
Planar. One hemisphere, pole in the middle. A cylindrical world map would squash the Arctic into a stretched strip along the top.
Got it now? Scroll back up and re-read the section β it should land differently.
Britain offered a prize of 20,000 pounds, about half a million dollars today. John Harrison, a working-class carpenter, invented and perfected the first accurate seafaring chronometer. That is why the chronometer shows up on your study sheet.
A GPS reading is two numbers: latitude and longitude. Treat them like a graph. The origin, where both are zero, is the crossing of the equator and the prime meridian. Every position is north or south, and east or west, of that crossing.
The lesson's example: 30Β° N, 90Β° W is on the southern coast of Louisiana. That is New Orleans. It is still that point on a map with curved lines. The grid works on every projection.
The equator is naturally in the middle of the poles. Longitude has no natural zero, so a conference of geographers in 1884 put 0Β° through the Royal Observatory in Greenwich, England.
Four more special lines, from the sun:
β’ Tropic of Cancer ~23.5Β° N β farthest north the sun is straight overhead, June solstice.
β’ Tropic of Capricorn ~23.5Β° S β farthest south the sun is straight overhead, December solstice.
β’ Arctic Circle ~66.5Β° N and Antarctic Circle ~66.5Β° S β outer limits of 24-hour polar day and polar night.
Memory tricks from the lesson: latitude lines get shorter toward the poles. Longitude lines are all the same length. In football, a lateral pass goes to the side. Latitude lines also go side to side.


Two numbers. Same move every time: find latitude first, then longitude, then mark the crossing.
The equator (0Β° latitude) crosses the prime meridian (0Β° longitude) in the Gulf of Guinea, off west Africa. Every other place is north or south, and east or west, of that crossing.
30Β° N, 90Β° W. That is the southern coast of Louisiana: New Orleans. If you land in the Gulf of Mexico or in Canada, you swapped north/south or mixed up 30 with 90.
Equator. Prime meridian. Tropic of Cancer (north). Tropic of Capricorn (south). Arctic Circle (north). Antarctic Circle (south). Cancer and Arctic are north. Capricorn and Antarctic are south.
Tokyo is about 36Β° N, 140Β° E. Do you go north or south of the equator first?
North. Latitude first: find 36Β° N (between 30 and 45, in Japan). Then 140Β° E (between 120 and 150). The crossing is the city.
Got it now? Scroll back up and re-read the section β it should land differently.
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