Goode S Interrupted Equal Area
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Goode S Interrupted Equal Area
It is most commonly used in interrupted form. Which statement describes the goode's interrupted homolosine projection. It is a pseudocylinddrica parity projection interrupted.
John paul goode has developed the projection in 1925. Goode's interrupted homolosine equal area projection (figure 6) is widely used to sho the distribution of phenomena on the continents. The projection of the mapponosine map of goode is designed to minimize distortion for the whole world.
Goode's interrupted homolosine equal area projection (figure 6) is widely used to sho the distribution of phenomena on the continents.
John paul goode developed the projection in 1925. The goode's interrupted projection is equivalen yet the shapes of the land masses are also very well maintained 40 n 0° 20 s 40 s goode's interrupted homolosine equal area projection 60°s re 6: Is appropriate for mapping the distribution of phenomena found on both land and sea. The mollweide projection is used north and south of the 40°44'12'' parallels.
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