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Following capture, Triton's orbit would have been highly eccentric, circularizing post-capture to its present, nearly circular orbit. In this early eccentric state, tides raised on Triton by Neptune would have been extreme, dissipating large amounts of energy within Triton and contributing to the circularization of its orbit.
Triton's atmosphere supports clouds of nitrogen ice crystals and a layer of organic atmospheric haze. Triton was the first Neptunian moon to be discovered, on October 10, 1846, by English astronomer William Lassell. The 1989 flyby of Triton by the Voyager 2 spacecraft remains the only up-close visit to the moon as of 2024.
Triton follows a retrograde and quasi-circular orbit, and is thought to be a gravitationally captured satellite. It was the second moon in the Solar System that was discovered to have a substantial atmosphere, which is primarily nitrogen with small amounts of methane and carbon monoxide. [26] The pressure on Triton's surface is about 14 μbar. [26]
As a result, Triton's surface geology is largely driven by the dynamics of water ice and other volatiles such as nitrogen and methane. Triton's geology is vigorous, and has been and continues to be influenced by its unusual history of capture, high internal heat, and its thin but significant atmosphere.
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On January 20, 1960, Triton got underway to conduct an accelerated series of at-sea testing. Triton returned on February 1 as preparations continued for her forthcoming shakedown cruise , scheduled for departure on February 16, 1960, which involved operating with the command ship Northampton , flagship of the U.S.
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