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JordanA Robinson map is a type of world map projection that was created in 1963 by Arthur H. Robinson. It aims to balance the distortion of shape, area, scale, and distance in a way that provides a more visually appealing representation of the globe compared to other map projections like the Mercator projection. The Robinson map is commonly used in atlases and textbooks.
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Who invented the Robinson map?
The Robinson map was created by Arthur H. Robinson, an American geographer, in 1963. It aimed to balance distortion of size and shape in global maps.
Why was the Robinson Projection Map invented?
The Robinson Projection Map was created in 1963 by Arthur H. Robinson to provide a more visually appealing world map that minimized distortion of shapes and sizes of landmasses. It aimed to balance distortions across the map while maintaining a familiar global layout for better understanding and navigation.
What is another name for an oval-shaped projection map?
Another name for an oval-shaped projection map is called a Robinson Projection Map because it was created by an American cartographer named Arthur Robinson.
Are the shapes and sizes of the continents or the waterways shown more accurately on the Robinson projection map?
The Robinson projection map shows the shapes of the continents more accurately than the Mercator projection map, but both distort the sizes of landmasses, making areas near the poles appear larger than they are. Waterways and continents are more accurately depicted in size and shape on specialized maps like the Winkel Tripel projection, which aims to balance size and shape distortions.
Is it true or false that the Robinson projection shows the size of the continents accurately and the water areas are expanded to fill the extra space?
True. The Robinson projection is a compromise map projection that shows the size and shape of most continents relatively accurately, while also increasing the size of oceans to balance out the distortions of the land areas. However, no map projection can perfectly represent the three-dimensional Earth on a two-dimensional surface.
