Light
The fact that light comes in many different wavelengths or frequencies is the reason for many of the phenomena we see in nature.  For example, the sky at noon is blue - why not green or red or yellow?  The sky overhead is blue because air contains very tiny dust particles that are even smaller than light waves.  Of the many wavelengths of visible light coming from the sun, blue light has the shorter wavelength.  Shorter wavelengths are much more likely to bump into the small particles of dust than are the longer green and red wavelengths.  And when blue light bumps into the dust, it scatters in all directions, some of it reaching our eyes.  The red and green light on the other hand do not so easily scatter by the dust, so they continue straight on through, not scattering to reach our eyes.
So why does the sun look red at sunset?  You can answer this now applying the same reasoning.

The finite size of the wavelength of light also becomes important when you study things as small as bacteria -- they are hardly bigger than the light waves, and this means that our view of them must always be fuzzy.
In everyday life we deal mainly with objects that are much larger than the wavelength of light, and then light acts like a stream of tiny bullets that travel in straight lines. In what follows we will think of light this way.
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Copyright 2000 J. P. Straley and S. S. Kovash