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Geography: The Study of Earth
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GEOGRAPHY The study of the human and nonhuman
features of Earth, our home.
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Cardinal Directions Cardinal directions are North, South, East, and West. (N, S, E, W)
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Intermediate directions
Intermediate directions lie between the cardinal directions. (NE, SE, NW, SW)
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Sphere A round-shaped body
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Latitude Is the distance measured in degrees north or south of the Equator. Lines of latitude run east to west.
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Degrees Are units that measure angles(º)
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Latitude: 34°59′ N Longitude: 90°00′ W
Minutes Smaller units of measure for measuring longitude and latitude.(΄) Coordinates for Southaven, MS Latitude: 34°59′ N Longitude: 90°00′ W
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equator The imaginary line that divides the Earth into the Northern and Southern Hemisphere. The Equator is also known as the 0º degree latitude line.
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Hemisphere Each half of the Earth. Northern and Southern Hemisphere Eastern and Western Hemisphere
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Prime Meridian The imaginary line that divides the Earth into the Eastern and Western Hemisphere. The Prime Meridian is known as the 0º line of longitude.
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longitude Is the distance measured in degrees east or west of the Prime Meridian. Lines of longitude run North and South.
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key Map key explains the symbols and shading on the map.
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Locator Map The locator map shows a larger area than the main map. It shows where the area on the map is located within this larger area. Locator Map
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Scale Bar A scale bar shows how much space on the map represents a given distance on the land.
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A diagram of a compass showing direction.
Compass Rose A diagram of a compass showing direction. Compass rose
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Physical Map Physical maps show physical, or natural features.
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elevation Elevation is the height above sea level.
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Special purpose map Special-purpose maps show the location or distribution of human or physical features.
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Political Map Political maps show political units, such as countries or states.
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Distortion The loss of accuracy in the size or position of objects on a map.
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Ways to map Earth on a flat surface.
projections Ways to map Earth on a flat surface.
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The Equal-Area Projection
An equal-area map shows the correct size of landmasses. However, their shapes are distorted.
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The mercator PRojection
The Mercator projection shows correct shapes and directions, but not true distances or sizes. Mercator maps make areas near the poles look bigger than they are.
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The Robinson projection
The Robinson Projection shows nearly the correct size and shape of most land areas. Distortions are seen in areas around the edges of the map.
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