 
Zodiacal light results from the scattering of sunlight off small (1 – 300 micron) interplanetary dust particles lying in the plane of the ecliptic.  This dust originates through the    sublimation    of    cometary nuclei and collisions between   asteroids, and forms a band of dust that completely circles the Sun    and stretches out to the orbit of Jupiter.
At a dark site on a moonless night, it may be possible to see a faint   (comparable in brightness to the Milky Way),  triangular-shaped glow that stretches along the ecliptic from   the Sun.  This is the zodiacal light, which can be observed from low   latitudes all year round.  From mid to high latitudes, it is best observed about 90 minutes after sunset during the   spring, or 90 minutes before sunrise during the autumn, when the   ecliptic is steeply inclined to the horizon.  Under good conditions   it can be seen to extend up to 90 degrees along the ecliptic.
Study Astronomy Online at Swinburne University
All material is © Swinburne University of Technology except where indicated.