Maps of the World - Free Printable
Educational worksheet: Maps of the World. Download and print for classroom or home learning activities.
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Step-by-step solution for: Maps of the World
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Show Answer Key & Explanations
Step-by-step solution for: Maps of the World
The image you've uploaded is a Robinson projection of the world map. This type of map projection was developed by Arthur H. Robinson in 1963 and is widely used for general reference world maps because it balances the distortions of size, shape, distance, and direction more evenly than many other projections.
Let’s break down the key features and characteristics of this map:
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- The Robinson projection is a pseudocylindrical map projection.
- It means that:
- The equator is represented as a straight horizontal line.
- Meridians (lines of longitude) are curved, converging toward the poles.
- The poles are points rather than lines.
- It is not conformal (does not preserve angles) or equal-area (does not preserve size), but it provides a visually pleasing compromise between distortion types.
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1. Continents and Oceans:
- All seven continents are visible: North America, South America, Europe, Africa, Asia, Australia, and Antarctica.
- The oceans are shaded in light blue; landmasses in beige.
- Country borders are outlined but not labeled.
2. Grid Lines:
- Latitude and longitude lines form a grid.
- Latitude lines (parallels) are horizontal and equally spaced near the equator but become more compressed toward the poles.
- Longitude lines (meridians) are curved, bulging outward from the central meridian.
3. Shape and Size Distortion:
- The Robinson projection reduces extreme distortions seen in other projections like the Mercator (which exaggerates the size of regions near the poles).
- For example:
- Greenland appears much smaller compared to Mercator.
- Africa's true size is better represented relative to other continents.
- However, shapes are still slightly distorted—especially near the edges of the map (e.g., eastern Asia and western South America).
4. Poles:
- The North and South Poles are shown as points at the top and bottom of the map, respectively.
- They are not fully accurate in terms of area or scale.
5. Central Meridian:
- The map is centered on the Prime Meridian (0° longitude), which runs through Greenwich, England.
- The map extends approximately 180° east and west of this line.
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- Educational Use: It's commonly used in textbooks and classrooms because it presents a balanced view of the world.
- Aesthetic Appeal: It avoids the extreme stretching seen in some cylindrical projections.
- Balanced Compromise: While no flat map can perfectly represent a spherical Earth, Robinson strikes a good balance among area, shape, distance, and direction.
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- Distortion: Like all flat maps, it distorts reality. Areas near the poles appear smaller than they are, and shapes are stretched horizontally near the edges.
- No True Scale: There is no single point where scale is accurate across the entire map.
---
- Developed by Arthur H. Robinson, an American cartographer.
- Produced here by the Cartographic Research Lab at the University of Alabama, as noted in the bottom-right corner.
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This is a Robinson projection world map that offers a visually balanced representation of Earth's surface. It is ideal for general use due to its aesthetic appeal and reduced distortion, making it suitable for educational and informational purposes. While it doesn’t preserve any one property (like area or shape) perfectly, it provides a fair compromise across all aspects.
If you have a specific question about this map—such as identifying a location, understanding distortions, or comparing it to another projection—feel free to ask!
Let’s break down the key features and characteristics of this map:
---
🔹 What is the Robinson Projection?
- The Robinson projection is a pseudocylindrical map projection.
- It means that:
- The equator is represented as a straight horizontal line.
- Meridians (lines of longitude) are curved, converging toward the poles.
- The poles are points rather than lines.
- It is not conformal (does not preserve angles) or equal-area (does not preserve size), but it provides a visually pleasing compromise between distortion types.
---
🔹 Key Features of the Map:
1. Continents and Oceans:
- All seven continents are visible: North America, South America, Europe, Africa, Asia, Australia, and Antarctica.
- The oceans are shaded in light blue; landmasses in beige.
- Country borders are outlined but not labeled.
2. Grid Lines:
- Latitude and longitude lines form a grid.
- Latitude lines (parallels) are horizontal and equally spaced near the equator but become more compressed toward the poles.
- Longitude lines (meridians) are curved, bulging outward from the central meridian.
3. Shape and Size Distortion:
- The Robinson projection reduces extreme distortions seen in other projections like the Mercator (which exaggerates the size of regions near the poles).
- For example:
- Greenland appears much smaller compared to Mercator.
- Africa's true size is better represented relative to other continents.
- However, shapes are still slightly distorted—especially near the edges of the map (e.g., eastern Asia and western South America).
4. Poles:
- The North and South Poles are shown as points at the top and bottom of the map, respectively.
- They are not fully accurate in terms of area or scale.
5. Central Meridian:
- The map is centered on the Prime Meridian (0° longitude), which runs through Greenwich, England.
- The map extends approximately 180° east and west of this line.
---
🔹 Why Use the Robinson Projection?
- Educational Use: It's commonly used in textbooks and classrooms because it presents a balanced view of the world.
- Aesthetic Appeal: It avoids the extreme stretching seen in some cylindrical projections.
- Balanced Compromise: While no flat map can perfectly represent a spherical Earth, Robinson strikes a good balance among area, shape, distance, and direction.
---
🔹 Limitations:
- Distortion: Like all flat maps, it distorts reality. Areas near the poles appear smaller than they are, and shapes are stretched horizontally near the edges.
- No True Scale: There is no single point where scale is accurate across the entire map.
---
🔹 Who Created It?
- Developed by Arthur H. Robinson, an American cartographer.
- Produced here by the Cartographic Research Lab at the University of Alabama, as noted in the bottom-right corner.
---
✔ Summary:
This is a Robinson projection world map that offers a visually balanced representation of Earth's surface. It is ideal for general use due to its aesthetic appeal and reduced distortion, making it suitable for educational and informational purposes. While it doesn’t preserve any one property (like area or shape) perfectly, it provides a fair compromise across all aspects.
If you have a specific question about this map—such as identifying a location, understanding distortions, or comparing it to another projection—feel free to ask!
Parent Tip: Review the logic above to help your child master the concept of printable world map with latitude and longitude and countries.
![Free World Map with Longitude and Latitude Printable [PDF]](/images2/printable-world-map-with-latitude-and-longitude-and-countries/printable-world-map-with-latitude-and-longitude-and-countries-33.jpeg)
