Triton is the largest
natural satellite of the
planet Neptune. It was discovered on October 10, 1846, by English astronomer
William Lassell. It is the only large moon in the
Solar System with a
retrograde orbit, an orbit in the opposite direction to its planet's rotation. At in diameter, it is the
seventh-largest moon in the Solar System. Because of its retrograde orbit and composition similar to
Pluto's, Triton is thought to have been a
dwarf planet captured from the
Kuiper belt. Triton has a surface of mostly frozen
nitrogen, a mostly
water-ice crust, an icy
mantle and a substantial
core of rock and metal. The core makes up two-thirds of its total mass. Triton has a mean density of and is composed of approximately 15–35% water ice.