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A close-up view of TritonTriton, the only large moon in the solar system with a retrograde motion, is investigated. The moon rotates about Neptune every 5.88 days and its annual cycle lasts 165 years. The orbit of Triton is 355,000 km from Neptune and it is inclined 23 deg relative to Neptune's equator. The precession of its orbital plane causes complications in its seasonal progression. Triton has a radius of 1353 km and a density of 2.07 gm/cu cm. Triton is believed to have a core of rock surrounded by water ice and a surface veneer of methane and nitrogen ice. The bright haze in its atmosphere could be small grains of particulates. Triton's surface features suggest that the moon should have remained molten until about 1 billion years ago. In order to explain the active geyser-like plumes observed near the subsolar latitude of about 50 deg south, various mechanisms are suggested including explosive escape of nitrogen gas, surface winds, and buoyancy of warmer gas. Voyager 2, which left Neptune and Triton in August 1989 and is now moving out of the solar system, is expected to provide the first glimpses of interstellar material.
Document ID
19910036027
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Tsurutani, Bruce T.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Miner, Ellis D.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Collins, Stewart A.
(JPL Pasadena, CA, United States)
Date Acquired
August 15, 2013
Publication Date
December 1, 1990
Publication Information
Publication: Earth in Space
Volume: 3
ISSN: 1040-3124
Subject Category
Lunar And Planetary Exploration
Accession Number
91A20650
Distribution Limits
Public
Copyright
Other

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