These are links to other great web sites about Uranus. But beware: you don't want to get caught in Uranus' Web! Don't stay away from Windows to the Universe for long!
Nine Planets: Uranus
The Planet Uranus Just the facts...
Uranus Just a small Uranus site with general information.
Uranus Mythology Just in case you didn't get enough from our site...
Uranus Photo Gallery
Voyager Home Page
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Do you like spring? It might be your favorite season. But if you lived on Uranus, spring would not be so great. It's very cold and stormy. Not exactly great weather to play in! The temperature can reach...more
The plain bluegreen face of Uranus shows that Uranus is made of of only one thing. Beside clouds, there is also smog. Uranus' atmosphere is still forming. Motions in the cloud patterns indicate that, like...more
Uranus has // Call the moon count function defined in the document head print_moon_count('uranus'); interesting moons and a ring system. At Uranus there is even a half ring, or "ring arc". The moons are...more
The Giant planets do not have the same kind of layers inside that the earth-like planets do. The history of the giant planets was so different that they formed with much more gas on the inside. Uranus...more
Uranus is the tilted planet. The axis through its North and South Poles is tilted by 98°. In other words, Uranus is lying on its side! That's not all - the magnetic field of Uranus is tilted, too. Astronomers...more
The giant planets have definitely changed since their formation. But how much remains to be seen. Most of the original air of the giant planets remains in place. (The earth-like planets lost most of their...more
Uranus' atmosphere is made of methane, a medium sized molecule. At the uppermost reaches of the atmosphere, methane gas breaks apart due to energy from the sun and from the magnetosphere. The remins of...more
Motion of air in the atmosphere means wind. The major winds in the Uranian atmosphere called zonal winds. Motion of air in the atmosphere can also happen by diffusion. There is a continual circulation...more