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mercator projection
accurate direction, distorts land masses near pole
robinson projection
tries to balance out distortion, distorts all areas
gall-peters projection
stretches at equator, shrinks at pole
equal-area projections
preserves area of land masses, distorts shape and distance (ex. lambert)
conformal projections
maintains the shape of polygons on the map (ex. mercator)
goode homolosine projection
interrupted map that minimizes the distortion of land masses