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Published byHilda Phillips Modified over 9 years ago
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Chapter 3 Section 1 Modeling the Planet Objectives: -Explain how maps are models of Earth -Compare and contrast three types of map projections -Use latitude and longitude to describe a location on Earth
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Maps A flat two-dimensional representation of Earth’s surface Those who make maps are called cartographers
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Mercator Projection Depicts Earth as if a large cylinder of paper had been wrapped around the planet
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Gnomonic (planar) Projection A gnomonic map projection displays all great circles as straight lines. Thus the shortest route between two locations in reality corresponds to that on the map.
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Polyconic Projection A conic projection of a map having distances between meridians equal to those distances on a globe Good for representing large land masses
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Hemispheres Earth divided into halves Northern and Southern hemispheres are separated by the equator Eastern and Western are divided by the prime meridian
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Latitude These lines circle the world from east to west parallel to the equator. All measurements are in relation to the equator – Arctic Circle (60 0 North) – Tropic of Cancer (23.5 0 North) – Equator (0 0 ) – Tropic of Capricorn (23.5 0 South) – Antarctic Circle (60 0 South)
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Longitude These lines circle the world from north to south. Measured east or west of the prime meridian Prime Meridian (0 0 ) International Date Line (180 0 ) – United States lies between 65 0 and 125 0 west longitude.
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Map Scales A ratio relating map size to earth size – For example: 1inch:1mile In this case 1 inch on a map equals 1 mile on earth
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Map Scale:
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