Uranus is tilted on its side. The South Pole is the bright area on the left in this picture.
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Image courtesy of NASA, ESA, L. Sromovsky and P. Fry (University of Wisconsin), H. Hammel (Space Science Institute), and K. Rages (SETI Institute).
The Poles of Uranus
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. The planet's magnetic field is tilted 59°. A compass wouldn't be much help in finding North on Uranus!
Astronomers aren't sure why Uranus is tilted. One theory claims that an Earth-sized protoplanet might have smashed into Uranus when the Solar System was young and wild. Perhaps a collision like that knocked Uranus onto its side.
It takes Uranus 84 years to orbit the Sun once. The crazy tilt of Uranus, combined with its long year, make for some wacky seasons. Each season lasts more than 20 Earth-years. Spring (in the northern hemisphere of Uranus; Fall in the southern hemisphere) started on Uranus in December 2007. For the next 40 years the North Pole will be sunny all of the time, while the South Pole will be in darkness.
The South Pole of Uranus is covered by a light-colored "hood". Scientists think the hood is made of methane clouds and maybe a type of natural smog. There is not a hood over the North Pole. The South Pole had summertime for many years. Maybe heating from sunlight somehow caused the hood. Maybe a hood will form in the North, since it is becoming summertime there.
On Earth, the magnetic field is tilted about 11° away from Earth's spin axis (the imaginary line that goes through the North and South Poles). On Uranus, the magnetic poles are 59° away from the geographic poles! The main magnetic field of Uranus doesn't even go through the center of the planet.
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Uranus has a strange magnetic field. The magnetic poles of Uranus are not at all close to the geographic poles of Uranus. The main magnetic field of Uranus is tilted 59° away from the planet's spin axis.
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