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Basics to Human Geography Chapter 1 - Map Basics

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Distortion   occurs when putting information on a two dimensional map  
Distortion   the further one goes from the equator, the greater the distortion on the map  
Maps   the basic tools that geographers use to convey information  
Maps   are used to determine some types of geographic phenomena  
Fundamental Problem of Maps   that when attempting to display a three dimensional object on a two dimensional object, paper, distortion occurs  
Less Distortion   larger scale  
Scale   the relationship of the size of the map to the amount of area it represents on the planet  
Scale   the dimension into which one renders the real world  
Small Scale   is more area in less detail  
Large Scale   is a smaller areas in greater detail  
World   smallest scale map  
Three Ways to Write a Scale   in words, with a line, or with a ratio  
Latitude and Longitude   grid systems that geographers set up, which are fictional lines that divide the Earth's surface to assist people in determining an exact location  
Latitudes   are parallel lines that run EAST/WEST on the surface of the Earth  
Latitudes   parallels  
Equator   line that runs in the middle of the Earth  
Equator   0 degrees latitude  
Northern Hemisphere   anything north of the equator  
Southern Hemisphere   anything south of the equator  
90 degrees   highest degree of latitude  
North Pole   90 degrees north  
South Pole   90 degrees south  
Longitudes   are the lines that run NORTH/SOUTH  
Longitudes   meridians  
Prime Meridian   0 degree longitude line  
Prime Meridian   runs through Greenwich, England  
Globe   sphere made up of circles  
Time zone   15 degrees each  
International Dateline   about 180 degrees longitude  
International Dateline   zigzags through the Pacific due to the location of countries  


   


 

 

 

 

 

 
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