map projection
method of representing surface of Earth (3D) on a (2D)
Peters projection
shows all land masses with true area/size but distorts their shape; made the sizes more accurate than Mercator projection
Goode Homolosine projection
avoids shape disorientation by creating interruptions in the map continuity
Polar projection
looks down at Earth from the North/South Pole.
Robinson projection
attempts to create most visually appealing representation of Earth by keeping all types of distortion relatively low over most of the map.