Maps are a projection on a flat surface (2 dimensional) of a sphere (3 dimensional). They are therefore a best compromise to aid understanding of the relationships of position of the various continents and oceans.
Flat maps distort Earth's surface because it is impossible to represent a curved, three-dimensional surface like the Earth's on a flat, two-dimensional map without some distortion occurring. Different map projections use different techniques to minimize distortion in certain areas, such as shape, area, distance, or direction, but there will always be some level of distortion present.
The Mercator projection used for maps distorts the size and shape of large objects as the scale increases from the Equator to the poles where it becomes infinite. Whereas areas near the equator have little or no distortion, a latitude greater than 70 degrees has too much distortion to be useful.
One advantage to using a globe is that you can more accurately determine distances than you can with a flat map. Flat maps distort the spherical surface and that distortion can be significant over long distances.
Globes provide a more accurate representation of Earth's shapes and distances because they represent a 3D object on a 3D surface. Maps, on the other hand, often distort shapes and sizes due to the challenge of translating a spherical surface onto a flat plane.
It is not possible to draw an accurate map because the Earth's surface is a three-dimensional sphere, while maps are two-dimensional representations that distort the surface in some way, such as with shape, distance, or area. This distortion is inevitable due to trying to project a curved surface onto a flat plane.
Flat maps distort properties such as size, shape, distance, and direction of geographic features on the Earth's surface due to the challenge of representing a 3D spherical surface on a 2D plane. This distortion becomes more pronounced the further away from the equator you get.
One advantage to using a globe is that you can more accurately determine distances than you can with a flat map. Flat maps distort the spherical surface and that distortion can be significant over long distances.
Flat maps distort Earth's surface because it is impossible to represent a curved, three-dimensional surface like the Earth's on a flat, two-dimensional map without some distortion occurring. Different map projections use different techniques to minimize distortion in certain areas, such as shape, area, distance, or direction, but there will always be some level of distortion present.
Since the world is round, flat maps (rectangular maps) distort the sizes of continents by making them larger than they actually are.
One advantage to using a globe is that you can more accurately determine distances than you can with a flat map. Flat maps distort the spherical surface and that distortion can be significant over long distances.
yes
All flat maps do, globes do not.
The Mercator projection used for maps distorts the size and shape of large objects as the scale increases from the Equator to the poles where it becomes infinite. Whereas areas near the equator have little or no distortion, a latitude greater than 70 degrees has too much distortion to be useful.
The surface of the earth is the outside of a sphere, whereas the pages of an atlas are flat. Right there, you have the fundamental problem common to all maps ... how best to represent a curved surface on a flat picture. The answer is: In order to select one characteristic to depict accurately, you have to distort most everything else.
Africa is not flat. It is a diverse continent with varying landscapes including mountains, plateaus, deserts, and coastal plains. The misconception that Africa is flat may come from maps that distort the true size and shape of countries due to the challenge of representing a spherical surface on a flat map.
DIRECTION
Maps use techniques such as projection and scale to represent the curvature of the Earth on a flat surface. Different map projections distort certain aspects of the globe to create a more accurate representation of the Earth's surface on a flat map. This allows 3D objects to be visualized in 2D while maintaining relative spatial relationships.