Uranus is the only planet in the Solar System that rotates on its side, with an axis tilt of 97.77 degrees. This is most likely the result of a large collision not long after the planet formed. Among Uranus’ moons, there is one in particular that has drawn my attention, one that is also likely to be drastically affected by a collision. This moon is Miranda.
![](https://aaronxu041009.files.wordpress.com/2023/04/miranda1.jpg?w=774)
Miranda is the smallest of Uranus’ five large, round moons, and is closest to the planet. Miranda has some of the most bizarre geological features in the Solar System. There are three patches unique to Miranda called “coronae”, valleys and ridges that are lightly cratered (likely younger surface!), named “Elsinore”, “Inverness”, and “Arden”. It is suspected that these patches are caused by convection in Miranda’s ice mantle, and the heat required for this convection likely came from tidal heating due to it being in an elliptical orbit.
![](https://aaronxu041009.files.wordpress.com/2023/04/miranda2.jpg?w=500)
In addition to coronae, Miranda has some of the greatest canyons in the Solar System, some being 12 times deeper than the Grand Canyon. There is also a cliff on Miranda that is twenty kilometers high. It is fascinating how a moon only 500 km in diameter could sport so many strange geological features. The reasons have to be traced back to the moon’s past.
These great canyons and high mountains on Miranda, and the “Frankenstein” look of its surface could suggest that this moon was nearly destroyed in an impact, but it survived and was hastily recombined into what it is now. Another theory is, as introduced earlier, that internal heat caused convections. Miranda was in a 3:1 orbital resonance with Umbriel, another moon of Uranus, and this interaction as well as tidal heating from Uranus generated enough heat to create surface features. Also, meteor strikes could have melted the surface, causing slush to rise up from the mantle and form cliffs and canyons.