Earth's own moon is an example of a [[dwarf planet]]-sized moon. These moons are so large that their own self-gravity forces them to collapse into spheres or spheroids. Some of them, like [[Ganymede]] and [[Titan (moon)|Titan]], are larger even than the planet [[Mercury]]. Earth's moon was, of course, known to the ancients, but the remaining dwarf-planet-sized moons were generally the first to be discovered in orbit around any given primary. [[Galileo Galilei]] discovered the first four of these in orbit about [[Jupiter]] early in the seventeenth century; [[Christiaan Huygens]] then discovered Titan of [[Saturn]] later in that same century. | Earth's own moon is an example of a [[dwarf planet]]-sized moon. These moons are so large that their own self-gravity forces them to collapse into spheres or spheroids. Some of them, like [[Ganymede]] and [[Titan (moon)|Titan]], are larger even than the planet [[Mercury]]. Earth's moon was, of course, known to the ancients, but the remaining dwarf-planet-sized moons were generally the first to be discovered in orbit around any given primary. [[Galileo Galilei]] discovered the first four of these in orbit about [[Jupiter]] early in the seventeenth century; [[Christiaan Huygens]] then discovered Titan of [[Saturn]] later in that same century. |