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[[File:New_Webb_Images_Capture_Rare_View_of_Neptune’s_Rings_(Labeled).png|left|New Webb Images Capture Rare View of Neptune’s Rings (Labeled)|thumb]] [[File:Orbits_of_inner_moons_of_Neptune_including_S_2004_N_1.jpg|Orbits of inner moons of Neptune including S 2004 N 1|thumb|left]] [[File:Neptune_inner_moons_size_comparison.jpg|Neptune inner moons size comparison|thumb]] [[File:Triton_orbit_&_Neptune.png|left|Triton orbit & Neptune|thumb]] [[File:Irregular_moon_orbits_a_vs._i.jpg|Irregular moon orbits a vs. i|thumb]] '''Moons of Neptune'''

The [[Neptune|planet Neptune]] is known for its complex system of [[moons]], which are fascinating both in terms of their physical characteristics and their dynamic interactions with the planet and each other. As of the current knowledge cutoff in 2023, Neptune has 14 known moons, each with unique features and origins. The discovery of these moons has provided valuable insights into the [[Solar System|solar system's]] formation and evolution.

==Discovery and Exploration==
The first and largest moon of Neptune, [[Triton (moon)|Triton]], was discovered by [[William Lassell]] on October 10, 1846, just 17 days after Neptune itself was discovered. Triton is unique among the large moons of the solar system because it orbits Neptune in a retrograde direction, suggesting that it was captured by Neptune's gravity rather than forming in place. The other moons of Neptune were discovered in the 20th and 21st centuries, with the most recent ones identified using advanced ground-based telescopes and the [[Hubble Space Telescope]].

==Characteristics==
Neptune's moons vary significantly in size, composition, and orbit. Triton, the largest, contains more than 99.5% of the mass in orbit around Neptune and is one of the few geologically active moons in the solar system, with geysers of liquid nitrogen. The other moons are much smaller, and many are irregularly shaped, indicating they may be captured [[Kuiper Belt]] objects or fragments from collisions.

===Triton===
Triton is the seventh-largest moon in the solar system and has a diameter of about 2,710 kilometers. It has a thin atmosphere composed mostly of nitrogen with small amounts of methane. The surface of Triton is relatively young and features a mix of [[cryovolcanism|cryovolcanic]] landscapes, smooth plains, and few impact craters, suggesting internal heating and geological activity.

===Other Moons===
The inner moons of Neptune (Naiad, Thalassa, Despina, Galatea, Larissa, and Proteus) are thought to have formed from the debris left over after Triton's capture. These moons are small and have simple, cratered surfaces. The outer moons (Halimede, Sao, Laomedeia, Psamathe, and Neso) have irregular orbits and are likely captured objects. S/2004 N 1, the smallest and one of the most recently discovered moons, has a diameter of only about 16-20 kilometers.

==Orbital Dynamics==
The moons of Neptune exhibit a wide range of orbital dynamics. Triton's retrograde orbit is slowly decaying, and it is expected to eventually either collide with Neptune or break apart and form a ring system. The inner moons are in a complex dance with Neptune's rings and each other, participating in gravitational interactions that shape their orbits.

==Exploration==
To date, the only spacecraft to have visited the Neptune system is [[Voyager 2]], which flew by in 1989. Voyager 2's observations of Triton revealed a young, active surface and provided the first close-up images of any of Neptune's moons. Future missions to the Neptune system would likely focus on Triton and the unique opportunity it presents to study a body that originated in the outer solar system.

==Conclusion==
The moons of Neptune are a diverse group of celestial bodies that offer a window into the processes that have shaped the solar system. Their varied compositions, orbits, and interactions with Neptune and each other continue to be subjects of scientific study and fascination.

[[Category:Astronomy]]
[[Category:Moons of Neptune]]
{{Astronomy-stub}}

Moons of Neptune - Revision history

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