Miranda is one of Uranus’s most fascinating and unusual moons, discovered in 1948 by Gerard Kuiper, and is about 470 kilometers in diameter—small, yet incredibly complex. Despite its size, Miranda’s surface looks violently reshaped, featuring massive canyons, patchwork terrains, deep fault lines, and strange chevron-shaped patterns that make it one of the most geologically unique worlds in the Solar System. Its most famous feature is Verona Rupes, a cliff that may be up to 20 kilometers high, making it the tallest known cliff in the Solar System. Scientists believe Miranda’s bizarre landscape may have formed from repeated episodes of internal heating, tidal forces, or even the partial breakup and reassembly of the moon itself. It orbits Uranus at about 130,000 kilometers and is tidally locked, always showing the same face to the planet. Only Voyager 2 has captured close-up images of Miranda during its 1986 flyby, leaving many mysteries about its interior structure, geological history, and the exact cause of its dramatic surface features. The moon is named after Miranda from Shakespeare’s The Tempest, a character known for innocence and wonder—an ironic contrast to the moon’s chaotic and rugged appearance.