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Finding Locations on Earth
1 Models of the Earth Finding Locations on Earth
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Reference Points The points at which Earth’s axis of rotation intersect Earth’s surface are used as reference points Equator Prime Meridian
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Parallels Parallels – circle that runs east and west around the Earth
Parallel to equator
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Latitude Latitude – angular distance north or south from equator
Degrees
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Latitude 360 degrees in a circle Equator to poles = ¼ of a circle
¼ of a 360 = 90 degrees 1 degree = 1/360 of earth’s circumference = 111 km’s
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Minutes and Seconds 60 minutes in a degree 1 minute = 1.85 km
Washington D.C. 38°53’ N 60 seconds in a minute 38°53’23”N
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Longitude Meridians – semi circles that runs from pole to pole
Greenwich, England – Prime Meridian Longitude – angular distance measured east or west from P.M.
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½ 0f 360° = 180 0 – 180 East or West Washington D.C. 77°00’33” W
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Distance between meridians vary
@ poles it is less than at equator
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International Date Line
180 degree Longitude Goes through Pacific ocean
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Great Circles Divides globe into halves Latitude Longitude
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Finding Direction Geomagnetic vs. geographic poles
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Magnetic Declination Angle between the direction of geographic pole and the direction in which the compass needle points Important for map making and navigation
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GPS Global Positioning System Network of 24 satellites
Commercial – accurate between 10 – 15 m Military - centimeters
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