Site hosted by Angelfire.com: Build your free website today!
 
 
 
Aurora Borealis

 
                The sun gives off high-energy charged particles (also called ions) that travel out  into space at speeds of 320 to 704  kilometres per second. A cloud of such  particles is called a plasma. The stream of plasma coming from the sun is known as the solar wind. As the solar wind interacts with the fringes of the earth's magnetic field, some of the particles are trapped by it and they follow the lines of magnetic force down into the ionosphere, the section of the earth's atmosphere that extends from about 60 to 100 kilometers above the earth's surface. When the particles strike the gases in the ionosphere they start to glow, producing the spectacle that we know as the auroras, northern and southern. The variety of colors: red, green, blue and violet that appear in the sky corresponds to the different gases in the ionosphere. 

 
The auroras are affected by two things from the earth. These two things are the earth's magnetic field and the earth's atmosphere. 

The center of the earth is made up of a lot of very dense metal. This metal creates a magnetic field around the earth called the magnetosphere. The magnetosphere is the like a big magnet stuck in the middle of the earth. The magnetosphere is most  strong at the magnetic poles of the earth. This magnetic pull is very strong. It can pull things in from way out in outer space! 

 

Links
http://ph99.bc.edu/grad/Tomek/Auroral_Homepage/Aurora.html
http://sunshine.chpc.utah.edu/research/cosmic/rayinfo/aurora/creation2.htm