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             The 
              Ice Ages 
              Many people tried to figure out why the "Ice Ages" happened. 
              In the 1920s, a meteorologist (a person who studies the weather, 
              not meteors!) named Milutin Milankovich found a possible explanation: 
              changes in the orbit of the Earth. The 
              basic idea is fairly simple. As you probably already know, average 
              temperatures on Earth depend on the Earth's distance from the Sun. 
              If the Earth was closer to the Sun, the climate would be hotter 
              (like Venus), and if the Earth was farther from the Sun, the Earth 
              would be colder (like Mars). Now if the Earth was the only planet 
              going around the Sun, its orbit would never change and its climate 
              would remain constant. But the Moon and other planets are a part 
              of the Sun's family, and their gravity tugs slightly on the Earth 
              as they pass nearby, causing the Earth's orbit, and also its climate, 
              to change by tiny amounts. 
            The 
              three main orbital changes Milankovich 
              studied are:  
            
              1. changes in the shape 
                of Earth's orbit,  
                2. changes in the tilt of Earth's axis, 
                and  
                3. the wobble of Earth's axis.  
             
            Each of 
              these changes are cyclical, that is, they repeat over and over. 
              During the cycle of any one of these three changes, the Earth tends 
              to grow a little warmer, and then a little bit cooler. The three 
              orbital changes are actually all happening at the same time, but 
              the length of the cycle of each change is different. Most of the 
              time, the heating and cooling segment of each cycle cancel each 
              other out, giving Earth a lukewarm climate. But sometimes orbital 
              changes combine together to make the Earth's climate either very 
              warm or very cold. 
            
              
            For example, 
              if the cool segment of the shape cycle occurs at the same time as 
              the cool part of the tilt cycle, and at the same time as the cool 
              segment of the wobble cycle, then Presto-Chang-o, you get an ice 
              age! Its kind of like following directions written by a crazy chef 
              for making a veggie burger. If the directions said: cool the burger, 
              then heat the burger, and then cool the burger again, you would 
              end up with a lukewarm burger. However, if the directions said heat 
              the burger, then heat it again, and then heat it again, you would 
              get "burger flambe." But if the directions said cool the 
              burger, cool it again, and then cool it again, you would get a "glacier 
              burger."  
            Now the 
              question is: Did orbital changes make an ice age that killed the 
              dinosaurs? Is there any evidence in the rocks for an ice age 65 
              million years ago? To help you in your search, you might want to 
              find information about Ice Ages, Ice Epoch, Milankovich cycle, glaciers, 
              glacial deposits, or climate changes. Good luck!  
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