1550:
1432:, a caldera-like feature roughly 100 km in diameter seen near the equator. Surrounding this caldera is a massive cryovolcanic plain, Cipango Planum, which is at least 490,000 km in area; assuming Leviathan Patera is the primary vent, Leviathan Patera is one of the largest volcanic or cryovolcanic constructs in the Solar System. This feature is also connected to two enormous cryolava lakes seen northwest of the caldera. Because the cryolava on Triton is believed to be primarily water ice with some ammonia, these lakes would qualify as stable bodies of surface liquid water while they were molten. This is the first place such bodies have been found apart from Earth, and Triton is the only icy body known to feature cryolava lakes, although similar cryomagmatic extrusions can be seen on
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object, either one that happened to be passing by
Neptune (which is unlikely), or a moon or proto-moon in orbit around Neptune (which is more likely). A more recent hypothesis suggests that, before its capture, Triton was part of a binary system. When this binary encountered Neptune, it interacted in such a way that the binary dissociated, with one portion of the binary expelled, and the other, Triton, becoming bound to Neptune. This event is more likely for more massive companions. This hypothesis is supported by several lines of evidence, including binaries being very common among the large Kuiper belt objects. The event was brief but gentle, saving Triton from collisional disruption. Events like this may have been common during the formation of Neptune, or later when it
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1114:. It is also the largest retrograde moon in the Solar System. It accounts for more than 99.5% of all the mass known to orbit Neptune, including the planet's rings and thirteen other known moons, and is also more massive than all known moons in the Solar System smaller than itself combined. Also, with a diameter 5.5% that of Neptune, it is the largest moon of a gas giant relative to its planet in terms of diameter, although Titan is bigger relative to Saturn in terms of mass (the ratio of Triton's mass to that of Neptune is approximately 1:4788). It has a radius, density (2.061 g/cm), temperature and chemical composition similar to that of
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1268:'s atmosphere, the atmosphere of Triton is thought to result from the evaporation of nitrogen from its surface. Its surface temperature is at least 35.6 K (−237.6 °C) because Triton's nitrogen ice is in the warmer, hexagonal crystalline state, and the phase transition between hexagonal and cubic nitrogen ice occurs at that temperature. An upper limit in the low 40s (K) can be set from vapor pressure equilibrium with nitrogen gas in Triton's atmosphere. This is colder than Pluto's average equilibrium temperature of 44 K (−229.2 °C). Triton's surface atmospheric pressure is only about 1.4–1.9
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1536:(880 lb/s). This is similar to that which is estimated for Enceladus's cryovolcanic plumes at 200 kg/s (440 lb/s). However, if Triton's plumes are cryovolcanically driven, it remains to be explained why they predominantly appear over its southern polar cap. Triton's high surface heat flux may directly melt or vaporize nitrogen ice at the base of its polar caps, creating 'hot spots' which break through the ice or move to the ice caps' margins, before erupting explosively.
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1004:"They had to have formed beyond the water-ice line," says Mandt, referring to the distance from the sun where water would freeze into ice or snow, which is why Triton and Pluto have similar amounts of certain key elements. "One possibility is that the giant planets moved closer to the sun early in the first 100 million years or so of the Solar System, which may have disrupted the orbits of some bodies like Triton.", says Mandt.
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1667:(although they have a larger scale), and which may have a similar origin, possibly shear heating from strike-slip motion along faults caused by diurnal tidal stresses experienced before Triton's orbit was fully circularized. These faults with parallel ridges expelled from the interior cross complex terrain with valleys in the equatorial region. The ridges and furrows, or
1399:. Analysis of crater density and distribution has suggested that in geological terms, Triton's surface is extremely young, with regions varying from an estimated 50 million years old to just an estimated 6 million years old. Fifty-five percent of Triton's surface is covered with frozen nitrogen, with water ice comprising 15–35% and
4459:; Donahue, T. M.; Forrester, W. T.; Hall, D. T.; Herbert, F.; Holberg, J. B.; Hunter, D. M.; Krasnopolsky, V. A.; Linick, S.; Lunine, Jonathan I.; McConnell, J. C.; Moos, H. W.; Sandel, B. R.; Schneider, N. M.; Shemansky, D. E.; Smith, G. R.; Strobel, D. F.; Yelle, R. V. (1989). "Ultraviolet Spectrometer Observations of Neptune and Triton".
1353:, it is sensitive to small variations in spectral albedo. Based on the increase in atmospheric pressure between 1989 and 1997, it is estimated that by 2010 Triton's atmospheric pressure may have increased to as much as 4 Pa. By 2017, however, Triton's atmospheric surface pressure had nearly returned to
1815:
The orbital properties of Triton were already determined with high accuracy in the 19th century. It was found to have a retrograde orbit, at a very high angle of inclination to the plane of
Neptune's orbit. The first detailed observations of Triton were not made until 1930. Little was known about the
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Four roughly circular "walled plains" have been identified on Triton. They are the flattest regions so far discovered, with a variance in altitude of less than 200 m. They are thought to have formed from the eruption of icy lava. The plains near Triton's eastern limb are dotted with black spots,
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However, the significant geological activity on Triton has led to alternative proposals that the plumes may be cryovolcanic in nature, rather than driven by solar radiation. A cryovolcanic origin better explains the estimated output of Triton’s plumes, which possibly exceeds 400 kilograms per second
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of
Neptune's rotation to Neptune's orbit, 30°, and the inclination of Triton's orbit to Neptune's rotation, 157° (an inclination over 90° indicates retrograde motion). Triton's orbit precesses forward relative to Neptune's rotation with a period of about 678 Earth years (4.1 Neptunian years), making
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Studying prior data on the two bodies, the team found that both have a large amount of nitrogen and trace amounts of methane and carbon monoxide, which could have accumulated in the outer regions of the young nebula "For some reason,Triton was then ejected from this region and ensnared by
Neptune".
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The few impact craters on Triton are almost all concentrated in the leading hemisphere—that facing the direction of the orbital motion—with the majority concentrated around the equator between 30° and 70° longitude, resulting from material swept up from orbit around
Neptune. Because it orbits with
6028:
Steckel, Amanda; Conrad, Jack
William; Dekarske, Jason; Dolan, Sydney; Downey, Brynna Grace; Felton, Ryan; Hanson, Lavender Elle; Giesche, Alena; Horvath, Tyler; Maxwell, Rachel; Shumway, Andrew O; Siddique, Anamika; Strom, Caleb; Teece, Bronwyn; Todd, Jessica; Trinh, Kevin T; Velez, Michael A;
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Hofgartner, Jason D.; Birch, Samuel P. D.; Castillo, Julie; Grundy, Will M.; Hansen, Candice J.; Hayes, Alexander G.; Howett, Carly J. A.; Hurford, Terry A.; Martin, Emily S.; Mitchell, Karl L.; Nordheim, Tom A.; Poston, Michael J.; Prockter, Louise M.; Quick, Lynnae C.; Schenk, Paul (March 15,
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Two types of mechanisms have been proposed for Triton's capture. To be gravitationally captured by a planet, a passing body must lose sufficient energy to be slowed down to a speed less than that required to escape. An early model of how Triton may have been slowed was by collision with another
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This has been further supported in a 2024 study of the chemical composition of Pluto and Triton which suggests they originated in the same region of the outer Solar System before the latter was pulled into
Neptune’s orbit. Kathleen Mandt at NASA's Goddard Space Flight Center in Maryland and her
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imaged only 40% of Triton's surface, so this remains uncertain. However, the observed cratering asymmetry exceeds what can be explained based on the impactor populations, and implies a younger surface age for the crater-free regions (≤ 6 million years old) than for the cratered regions (≤
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data. Other observations have shown an increase in temperature by 5% from 1989 to 1998. These observations indicated Triton was approaching an unusually warm southern hemisphere summer season that happens only once every few hundred years. Hypotheses for this warming include a change of frost
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was frequently included in those plans. No efforts aimed at
Neptune and Triton went beyond the proposal phase and NASA's funding for missions to the outer Solar System is currently focused on the Jupiter and Saturn systems. A proposed lander mission to Triton, called
1656:. Some maculae are simple dark spots with diffuse boundaries, and others comprise a dark central patch surrounded by a white halo with sharp boundaries. The maculae typically have diameters of about 100 km and widths of the halos of between 20 and 30 km.
1000:
colleagues hypothesize that Triton and Pluto formed close to each other before the Solar System settled down. "They probably formed in the same region, which wouldn't be where the Kuiper belt is now—it would have been either closer or further away," says Mandt.
1295:(a "weather region") rising to an altitude of 8 km. Streaks on Triton's surface left by geyser plumes suggest that the troposphere is driven by seasonal winds capable of moving material over a micrometer in size. Unlike other atmospheres, Triton's lacks a
5388:
Elliot, J. L.; Hammel, H. B.; Wasserman, L. H.; Franz, O. G.; McDonald, S. W.; Person, M. J.; Olkin, C. B.; Dunham, E. W.; Spencer, J. R.; Stansberry, J. A.; Buie, M. W.; Pasachoff, J. M.; Babcock, B. A.; McConnochie, T. H. (1998). "Global warming on Triton".
699:. Triton's atmosphere is relatively thin and strongly variable, with its atmospheric surface pressure varying by up to a factor of three within the past 30 years. Triton's atmosphere supports clouds of nitrogen ice crystals and a layer of organic atmospheric
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in 1954. He obtained a value of 3,800 km. Subsequent measurement attempts arrived at values ranging from 2,500 to 6,000 km, or from slightly smaller than the Moon (3,474.2 km) to nearly half the diameter of Earth. Data from the approach of
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The high plains found on Triton's eastern hemisphere, such as
Cipango Planum, cover over and blot out older features, and are therefore almost certainly the result of icy lava washing over the previous landscape. The plains are dotted with pits, such as
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of its interior, which could have kept Triton fluid for a billion years; this inference is supported by evidence of differentiation in Triton's interior. This source of internal heat disappeared following tidal locking and circularization of the orbit.
1893:, would mine nitrogen ice from the surface of Triton and process it to be used as a propellant for a small rocket, enabling it to fly or 'hop' across the surface. Another concept, involving a flyby, was formally proposed in 2019 as part of NASA's
781:
received news of
Neptune's discovery, he wrote to Lassell suggesting he search for possible moons. Lassell discovered Triton eight days later. Lassell also claimed for a period to have discovered rings. Although Neptune was later confirmed to
900:
to be synchronous with its orbit around Neptune: it keeps one face oriented toward the planet at all times. Its equator is almost exactly aligned with its orbital plane. At present, Triton's rotational axis is about 40° from Neptune's
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Triton's south polar region is covered by a highly reflective cap of frozen nitrogen and methane sprinkled by impact craters and openings of geysers. Little is known about the north pole because it was on the night side during the
1476:
dust from beneath the surface of Triton in plumes up to 8 km high. Triton is thus one of the few bodies in the Solar System on which active eruptions of some sort have been observed. The best-observed examples are the
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However, simulations in 2017 showed that after Triton's capture, and before its orbital eccentricity decreased, it probably did collide with at least one other moon, and caused collisions between other moons.
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one side permanently facing the planet, astronomers expect that Triton should have fewer impacts on its trailing hemisphere, due to impacts on the leading hemisphere being more frequent and more violent.
905:, hence as Neptune orbits the Sun, Triton's polar regions take turns facing the Sun, resulting in seasonal changes as one pole, then the other moves into the sunlight. Such changes were observed in 2010.
1860:
of nearby stars, which indicated the presence of an atmosphere and an exotic surface. Observations in late 1997 suggest that Triton is heating up and the atmosphere has become significantly denser since
1128:. Only 40% of Triton's surface has been observed and studied, but it may be entirely covered in such a thin sheet of nitrogen ice. Triton's surface consists of 55% nitrogen ice with other ices mixed in.
1571:
is seen to the upper left. Just off-screen to the lower left is a fault zone aligned radially with the caldera, indicating a close connection between the tectonics and volcanology of this geologic unit.
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There are extensive ridges and valleys in complex patterns across Triton's surface, probably the result of freeze–thaw cycles. Many also appear to be tectonic and may result from an extension or
1345:, which would allow more heat to be absorbed. Another hypothesis argues that temperature changes are a result of the deposition of dark, red material from geological processes. Because Triton's
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Triton dominates the Neptunian moon system, with over 99.5% of its total mass. This imbalance may reflect the elimination of many of Neptune's original satellites following Triton's capture.
1511:
until enough pressure accumulates for it to erupt through the translucent layer. This model is largely supported by the observation that Triton was near peak southern summer at the time of
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revealed blocky outcrops, ridges, troughs, furrows, hollows, plateaus, icy plains and a few craters. Triton is relatively flat; its observed topography never varies beyond a kilometer. The
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are believed to generate enough additional heat to accomplish this and produce the observed signs of recent surface geological activity. The black material ejected is suspected to contain
2341:
Lassell rejected his previous claim of discovery when he found that the orientation of the supposed rings changed when he rotated his telescope tube; see p. 9 of Smith & Baum, 1984.
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its Neptune-orbit-relative inclination vary between 127° and 173°. That inclination is currently 130°; Triton's orbit is now near its maximum departure from coplanarity with Neptune's.
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Tryka, K. A.; Brown, R. H.; Anicich, V.; Cruikshank, D. P.; Owen, T. C. (1993). "Spectroscopic Determination of the Phase Composition and Temperature of Nitrogen Ice on Triton".
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Triton is one of the most geologically active worlds in the Solar System, with an estimated average surface age of less than 100 million years old. Its surface is covered by
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1686:, are thought to be of intermediate age in Triton's geological history, and in many cases to have formed concurrently. They tend to be clustered in groups or "packets".
586:
2959:
Lellouch, E.; de Bergh, C.; Sicardy, B.; Ferron, S.; Käufl, H.-U. (2010). "Detection of CO in Triton's atmosphere and the nature of surface-atmosphere interactions".
1731:, the rising of "lumps" of less dense material through a stratum of denser material. Alternative hypotheses include formation by collapses, or by flooding caused by
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with Neptune. Triton is only slightly larger than Pluto and is nearly identical in composition, which has led to the hypothesis that the two share a common origin.
1164:(including relatively small amounts of volatile ices), with the remainder being rocky material. Triton's surface area is 23 million km, which is 4.5% of
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as the planets they orbit. Therefore Triton must have been captured from elsewhere in the Solar System. Astrophysicists believe it might have originated in the
144:
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Nelson, R.M.; Smythe, W.D.; Wallis, B.D.; Horn, L.J.; et al. (1990). "Temperature and Thermal Emissivity of the Surface of Neptune's Satellite Triton".
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scientists on numerous occasions over the last decades. All of them identified Triton as being a prime target and a separate Triton lander comparable to the
4164:
1646:, which are probably the vents from which this lava emerged. The composition of the lava is unknown, although a mixture of ammonia and water is suspected.
1323:
created by the action of sunlight on methane. Triton's atmosphere also has clouds of condensed nitrogen that lie between 1 and 3 km from its surface.
786:, they are so faint and dark that it is not plausible he saw them. A brewer by trade, Lassell spotted Triton with his self-built 61 cm (24 in)
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The precise mechanism behind Triton's plumes is debated; one hypothesis is that Triton's plumes are driven by solar heating underneath a transparent or
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Triton's western hemisphere consists of a strange series of fissures and depressions known as "cantaloupe terrain" because it resembles the skin of a
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Martin-Herrero, Alvaro; Romeo, Ignacio; Ruiz, Javier (2018). "Heat flow in Triton: Implications for heat sources powering recent geologic activity".
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in 1949, Triton was commonly referred to as "the satellite of Neptune". Lassell did not name his discovery; he later successfully suggested the name
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and several other icy outer Solar System worlds. This is not thought to be adequate to power convection in Triton's icy crust. However, the strong
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1727:) are probably not impact craters because they are all of the similar size and have smooth curves. The leading hypothesis for their formation is
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by NASA that would launch in 2033 and arrive at the Neptune system in 2049. Two lower-cost mission concepts were subsequently developed for the
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melon. Although it has few craters, it is thought that this is the oldest terrain on Triton. It probably covers much of Triton's western half.
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Smith, B. A.; Soderblom, L. A.; Banfield, D.; Barnet, C.; Basilevsky, A. T.; Beebe, R. F.; Bollinger, K.; Boyce, J. M.; Brahic, A. (1989).
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1775:. The largest crater observed on Triton thought to have been created by an impact is a 27-kilometer-diameter (17 mi) feature called
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was only able to study about 40% of the moon's surface, multiple concept missions have been developed to revisit Triton. These include a
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terrains suggest a complex geological history. The atmosphere of Triton is composed primarily of nitrogen, with minor components of
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in the Solar System, comprises Triton's mantle, enveloping a core of rock and metal. There is enough rock in Triton's interior for
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and Neptune. However, these moons are all much more distant from their primaries and are small in comparison; the largest of them (
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is to Earth, to gradually decay further; predictions are that 3.6 billion years from now, Triton will pass within Neptune's
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Because Triton's surface indicates a long history of melting, models of its interior posit that Triton is differentiated, like
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1507:". As solar radiation warms the darker material beneath, this causes a rapid increase in pressure as the nitrogen begins to
5162:
Soderblom, L. A.; Kieffer, S. W.; Becker, T. L.; Brown, R. H.; Cook, A. F. II; Hansen, C. J.; Johnson, T. V.; Kirk, R. L.;
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Cruikshank, D. P.; Stockton, A.; Dyck, H. M.; Becklin, E. E.; Macy, W. (1979). "The diameter and reflectance of Triton".
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seas and a nitrogen/methane atmosphere with a density as much as 30% that of Earth. Like the famous overestimates of the
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1968:
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In Lunar and Planetary Inst., Twenty-fourth Lunar and Planetary Science Conference. Part 1: A-F (SEE N94-12015 01-91)
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is a mission concept for a Neptune orbiter with a focus on Triton being studied beginning April 2021 as a possible
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59:
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Schenk, P.; Jackson, M. P. A. (April 1993). "Diapirism on Triton: A record of crustal layering and instability".
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1954:
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from altitudes of 8 to 950 km and an exosphere above that. The temperature of Triton's upper atmosphere, at
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4224:"Subsurface oceans and deep interiors of medium-sized outer planet satellites and large trans-neptunian objects"
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4165:"Spectroscopy of Pluto and Triton at 3–4 Microns: Possible Evidence for Wide Distribution of Nonvolatile Solids"
3333:
Smith, R. W.; Baum, R. (1984). "William Lassell and the Ring of Neptune: A Case Study in Instrumental Failure".
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Cantaloupe terrain, which is mostly dirty water ice, is only known to exist on Triton. It contains depressions
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metal mirror reflecting telescope (also known as the "two-foot" reflector). This telescope was donated to the
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The proposed capture of Triton may explain several features of the Neptunian system, including the extremely
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Departing image of Triton, showing its hazy atmosphere illuminated by sunlight and "extending" its crescent
940:. This will result in either a collision with Neptune's atmosphere or the breakup of Triton, forming a new
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imagery. Triton's massive south polar cap dominates most of the image, with cryovolcanic features such as
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3380:"The Royal Observatory Greenwich – where east meets west: Telescope: The Lassell 2-foot Reflector (1847)"
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levels; the cause for the rapid spike in atmospheric pressure between 1989 and 2017 remains unexplained.
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The current understanding of moons in retrograde orbits means they cannot form in the same region of the
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1751:"walled plains". The paucity of craters is evidence of extensive, relatively recent, geologic activity.
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Dark streaks across Triton's south polar cap surface, thought to be dust deposits left by eruptions of
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around its planet (i.e. it orbits in a direction opposite to the planet's rotation). Most of the outer
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Strom, Robert G.; Croft, Steven K.; Boyce, Joseph M. (1990). "The Impact Cratering Record on Triton".
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All detailed knowledge of the surface of Triton was acquired from a distance of 40,000 km by the
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atmosphere, with trace amounts of carbon monoxide and small amounts of methane near its surface. Like
993:
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to Neptune on August 25, 1989, led to a more accurate estimate of Triton's diameter (2,706 km).
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597:— revolving in the opposite direction to the parent planet's rotation — the only large moon in the
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Walter, Callum Andrew; Lowes, Leslie L; Hudson, Troy; Scully, Jennifer E. C. (December 12, 2023).
3571:; Jankowski, D. G.; Nicholson, P. D. (July 1989). "Tidal evolution in the Neptune-Triton system".
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s flyby, ensuring its southern polar cap was receiving prolonged sunlight. If this were the case,
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5358:
4292:"Powering Triton's recent geological activity by obliquity tides: Implications for Pluto geology"
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in the Solar System, the second-largest planetary moon in relation to its primary (after Earth's
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Lunine, Jonathan I.; Nolan, Michael C. (November 1992). "A massive early atmosphere on Triton".
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1841:, this proved incorrect. As with Mars, a denser atmosphere is postulated for its early history.
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Stone, EC; Miner, ED (December 15, 1989). "The Voyager 2 Encounter with the Neptunian System".
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Ingersoll, Andrew P.; Tryka, Kimberly A. (1990). "Triton's Plumes: The Dust Devil Hypothesis".
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Irwin, L. N.; Schulze-Makuch, D. (2001). "Assessing the Plausibility of Life on Other Worlds".
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1615:. These features are unusually crater free, indicating they are young and were recently molten.
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976:, a ring of small icy objects extending from just inside the orbit of Neptune to about 50
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5105:"Triton: Topography and Geology of a Probable Ocean World with Comparison to Pluto and Charon"
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1311:, is higher than that at its surface, due to heat absorbed from solar radiation and Neptune's
1019:. Triton's initially eccentric orbit would have intersected the orbits of irregular moons and
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Boyce, Joseph M. (March 1993). "A structural origin for the cantaloupe terrain of Triton".
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Schenk, Paul M.; Zahnle, Kevin (December 2007). "On the negligible surface age of Triton".
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observed from Earth, the belt is also home to several large, planet-like bodies including
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1779:. Although larger craters have been observed, they are generally thought to be volcanic.
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5327:
5188:
5120:
4992:
4859:
4826:
4720:
4702:
4663:
4605:
4554:
4541:
Duxbury, N S; Brown, R H (August 1993). "The Phase Composition of Triton's Polar Caps".
4472:
4422:
4353:
4310:
4241:
4185:
4125:
3990:
3915:
3857:
3757:
3706:
3620:
3524:
3346:
3306:
3272:
3238:
3194:
3065:
2906:
2880:
2672:
1856:
In the 1990s, various observations from Earth were made of the limb of Triton using the
1763:
found only 179 that were incontestably of impact origin, compared with 835 observed for
964:(green), in the Solar System's outskirts, is where Triton is thought to have originated.
817:, and was officially adopted many decades later. Until the discovery of the second moon
9308:
9296:
9184:
9015:
9005:
8995:
8985:
8956:
8946:
8924:
8902:
8872:
8862:
8789:
8779:
8769:
8717:
8654:
8644:
8614:
8594:
8564:
8542:
8532:
8489:
8454:
8424:
8414:
8404:
8361:
7796:
7690:
7238:
6806:
6495:
5951:
5843:
5722:
5671:
5499:
5414:
5313:
5255:
5208:
5085:
5041:
4958:
4938:
4881:
4683:
4625:
4574:
4492:
4434:
4322:
4197:
4145:
3876:
3843:
3831:
3777:
3743:
3642:
3404:
3358:
3085:
2994:
2968:
2918:
2681:
2654:
2056:
2023:
1838:
1396:
929:
810:
798:
489:
134:
4839:
4754:"Hubble Space Telescope Helps Find Evidence that Neptune's Largest Moon Is Warming Up"
3923:
8852:
8842:
8727:
8584:
8574:
8206:
7739:
7481:
7443:
7423:
7313:
7267:
6964:
6749:
6636:
6631:
6166:
6161:
5835:
5796:
5761:
5714:
5663:
5638:
5592:
5339:
5200:
5175:
5089:
4962:
4885:
4873:
4675:
4617:
4566:
4518:
4484:
4365:
4223:
4137:
4002:
3881:
3781:
3769:
3646:
3632:
3568:
3460:
3450:
3362:
3077:
2787:
2051:
1894:
1660:
1504:
1366:
1247:
1208:
988:, which is now recognized as the largest in a population of Kuiper belt objects (the
977:
732:
575:
279:
7948:
6096:
5726:
5675:
5418:
5259:
4687:
4629:
4578:
4496:
4326:
4201:
4149:
3796:
2998:
2907:"Constraints on the evolution of the Triton atmosphere from occultations: 1989-2022"
1664:
1543:
spacecraft, it is estimated that a plume eruption on Triton may last up to a year.
1387:
spacecraft during a single encounter in 1989. The 40% of Triton's surface imaged by
9272:
8836:
8707:
8604:
8444:
8341:
8163:
8130:
7676:
7659:
7490:
7361:
7346:
7261:
6974:
6887:
6854:
6832:
6772:
6725:
6589:
6537:
6240:
6230:
5900:
5895:
5847:
5827:
5792:
5757:
5706:
5655:
5609:
5503:
5491:
5406:
5331:
5247:
5212:
5192:
5124:
5103:
Schenk, Paul; Beddingfield, Chloe; Bertrand, Tanguy; et al. (September 2021).
5077:
4996:
4948:
4904:
4863:
4846:
4724:
4667:
4609:
4558:
4476:
4438:
4426:
4357:
4314:
4245:
4228:
4189:
4129:
3994:
3919:
3871:
3861:
3761:
3710:
3624:
3528:
3350:
3310:
3276:
3242:
3198:
3089:
3069:
2986:
2936:
2884:
2676:
2655:"The Orbits of the Neptunian Satellites and the Orientation of the Pole of Neptune"
2037:
1669:
1643:
1604:
1556:
1482:
1429:
1315:. A haze permeates most of Triton's troposphere, thought to be composed largely of
1227:
1212:
1192:
862:
854:
783:
594:
195:
152:
99:
45:
5831:
4671:
4480:
2990:
2940:
1708:-like double ridges. Slidr Sulci (vertical) and Tano Sulci form the prominent "X".
1567:
extend radially from the caldera to the right and upper-right of the image, while
9135:
8278:
8253:
8239:
8187:
8004:
7958:
7908:
7838:
7818:
7641:
7433:
7428:
7413:
7356:
7351:
7211:
7169:
6984:
6929:
6909:
6867:
6827:
6822:
6690:
6685:
6569:
6421:
6394:
6346:
6102:
5710:
5659:
5335:
5282:
5196:
5000:
4783:
4613:
4562:
4318:
4249:
4133:
3998:
3553:
3218:
3047:"Neptune's capture of its moon Triton in a binary–planet gravitational encounter"
1904:
1868:
1834:
1826:
1525:
1437:
1196:
1145:
1008:
980:
from the Sun. Thought to be the point of origin for the majority of short-period
822:
770:
711:
696:
649:
562:
417:
390:
64:
5635:
5272:
5161:
1759:
on Triton's surface are relatively rare. A census of Triton's craters imaged by
323:
8823:
8516:
8325:
8307:
8173:
7989:
7928:
7918:
7888:
7878:
7863:
7753:
7723:
7698:
7562:
7408:
7217:
7015:
6892:
6882:
6877:
6872:
6720:
6604:
6594:
6584:
6579:
6574:
6469:
6235:
4840:
Buratti, Bonnie J.; Hicks, Michael D.; Newburn, Ray L. Jr. (January 21, 1999).
4361:
3866:
3354:
3146:
2576:
2567:
2473:
2441:
2417:
2393:
2363:
2359:
2351:
1804:
1768:
1638:
encounter, but it is thought that Triton must also have a north polar ice cap.
1568:
1519:
1486:
1188:
1133:
1125:
941:
921:
897:
866:
707:
676:
657:
229:
7730:
6060:
5302:"Hypotheses for Triton's plumes: New analyses and future remote sensing tests"
5081:
5015:
4701:
Stevens, M. H.; Strobel, D. F.; Summers, M. E.; Yelle, R. V. (April 3, 1992).
4111:
3628:
3281:
3256:
3119:"NASA Selects Four Possible Missions to Study the Secrets of the Solar System"
908:
Triton's revolution around Neptune has become a nearly perfect circle with an
648:, with the rest being mostly rock and metal. Triton is differentiated, with a
9330:
8294:
8080:
7963:
7953:
7943:
7903:
7883:
7873:
7853:
7759:
7670:
7627:
7604:
7525:
7461:
7456:
7341:
7180:
7023:
6904:
6654:
6444:
6256:
5343:
4456:
3773:
3436:
3315:
3290:
2457:
2425:
2401:
2355:
2062:
1889:
1845:
1756:
1732:
1705:
1560:
1441:
1392:
1376:
1312:
1269:
1223:
1216:
1031:
1012:
902:
882:
826:
818:
778:
680:
669:
250:
5539:. State University of New York (published 1991): 613–19. 1991IAUTA..21..613A
3730:
Sheppard, Scott S.; Jewitt, David (2004). "Extreme Kuiper Belt Object 2001 Q
3715:
3690:
3464:
3247:
3222:
9284:
8526:
8521:
8149:
8061:
8014:
8009:
7923:
7898:
7893:
7833:
7767:
7704:
7569:
7517:
7475:
7403:
7317:
7028:
6862:
6564:
6555:
6087:
5839:
5718:
5667:
5523:
5204:
4953:
4926:
4784:"MIT researcher finds evidence of global warming on Neptune's largest moon"
4679:
4621:
4570:
4488:
4369:
4141:
3885:
3203:
3081:
2888:
2449:
2433:
1883:
1772:
1748:
1612:
1478:
1445:
1433:
1425:
1350:
1300:
1296:
1104:
1016:
969:
913:
841:
684:
629:
602:
598:
35:
20:
4877:
4813:
MacGrath, Melissa (June 28, 1998). "Solar System Satellites and Summary".
1160:. Triton's mean density implies that it probably consists of about 30–45%
660:
at its center. Although Triton's orbit is nearly circular with a very low
8511:
8388:
8335:
8330:
7868:
7717:
7649:
7599:
7594:
7511:
7000:
6934:
6695:
6362:
6266:
5495:
3827:
3748:
2409:
1946:
1857:
1755:
Due to constant erasure and modification by ongoing geological activity,
1694:
1608:
1500:
1419:
1346:
1331:
1316:
1292:
1177:
1157:
1024:
973:
961:
937:
728:
606:
478:
6031:"The Science Case for Nautilus: A Multi-Flyby Mission Concept to Triton"
4908:
4815:
Hubble's Science Legacy: Future Optical/Ultraviolet Astronomy from Space
3073:
2905:
Sicardy, B.; Tej, A.; Gomez-Júnior, A. R.; et al. (February 2024).
2705:
1747:
Tuonela Planitia (left) and Ruach Planitia (center) are two of Triton's
1215:
to this day, similar to what is thought to exist beneath the surface of
9217:
9071:
9059:
9047:
9025:
8966:
8912:
8552:
8383:
8102:
7984:
7684:
7654:
7635:
7577:
7542:
7106:
7082:
7070:
7034:
6939:
6919:
6914:
6700:
6664:
6659:
6261:
6083:
5274:
USGS Astrogeology Research Program: Gazetteer of Planetary Nomenclature
5251:
5129:
5104:
1800:
NASA illustration detailing the studies of the proposed Trident mission
1713:
1564:
1273:
932:
also cause Triton's orbit, which is already closer to Neptune than the
724:
457:
5688:
4728:
3532:
2811:
9119:
9107:
9095:
9083:
8934:
8757:
8674:
8464:
8302:
8225:
7913:
7843:
7556:
7530:
7467:
7142:
7094:
7058:
7046:
6924:
6669:
6400:
6074:
5972:
4430:
2492:
10. So, the total mass of all moons smaller than Triton is about 1.68
2465:
1818:
1700:
1489:
1464:
1336:
1220:
1153:
889:
720:
8192:
7938:
7773:
5739:
5227:
4647:
3445:. Wiley-Praxis Series in Astronomy and Astrophysics (2nd ed.).
3176:
2620:
1975:
1915:: the first the following June and the second in 2023. The first is
1629:
Triton's bright south polar cap above a region of cantaloupe terrain
1371:
8200:
8095:
6506:
5318:
5168:"Triton's Geyser-Like Plumes: Discovery and Basic Characterization"
4943:
4193:
3848:
3765:
2923:
1919:, which would launch in 2031 and arrive in 2047, and the second is
1600:
1584:
1261:
861:
Triton is unique among all large moons in the Solar System for its
802:
787:
688:
554:
267:
6021:
5768:
5410:
4868:
4841:
2973:
2379:
10 kg. Combined mass of 12 other known moons of Neptune: 7.53
1030:
Triton's eccentric post-capture orbit would have also resulted in
877:
also have retrograde orbits, as do some of the irregular moons of
761:
9208:
8978:
8375:
8107:
8090:
7621:
7371:
6795:
6547:
5266:
4455:
Broadfoot, A. L.; Atreya, S. K.; Bertaux, J. L.; Blamont, J. E.;
3832:"Triton's evolution with a primordial Neptunian satellite system"
2074:
1400:
1320:
1149:
1141:
1137:
1060:
989:
885:) has only 8% of the diameter (and 0.03% of the mass) of Triton.
870:
692:
633:
614:
582:
558:
405:
376:
284:
8030:
5924:"Triton Hopper: Exploring Neptune's Captured Kuiper Belt Object"
5439:. Abstracts of the 25th Lunar and Planetary Science Conference.
4409:
Ingersoll, Andrew P. (1990). "Dynamics of Triton's atmosphere".
1844:
The first attempt to measure the diameter of Triton was made by
1625:
8220:
8214:
8181:
7418:
7383:
7174:
5947:"Neptune's Moon Triton Is Destination of Proposed NASA Mission"
5465:
Prockter, L. M.; Nimmo, F.; Pappalardo, R. T. (July 30, 2005).
4517:(3rd ed.). Thailand: Workman Publishing. pp. 172–73.
4509:
2786:(3rd ed.). Amsterdam; Boston: Elsevier. pp. 861–882.
1764:
1728:
1469:
1407:
1406:
forming the remaining 10–20%. The surface also has deposits of
1342:
1173:
1169:
945:
920:
Triton's orbit in the time since the origin of the system, and
878:
874:
830:
727:
remains the only up-close visit to the moon as of 2024. As the
620:
At 2,710 kilometers (1,680 mi) in diameter, Triton is the
579:
468:
336:
5043:
Triton Hopper: Exploring Neptune's Captured Kuiper Belt Object
1410:, a dark, tarry slurry of various organic chemical compounds.
1279:
1168:, or 15.5% of Earth's land area. Triton has an unusually high
117:
8157:
7933:
5774:
5298:
4454:
4222:
Hussmann, Hauke; Sohl, Frank; Spohn, Tilman (November 2006).
2958:
2481:
1493:
1327:
1265:
1200:
1184:
1165:
1129:
1115:
1107:
985:
981:
710:
to be discovered, on October 10, 1846, by English astronomer
6006:
Hansen-Koharcheck, Candice; Fielhauer, Karl (June 7, 2021).
5441:
Abstracts of the 25th Lunar and Planetary Science Conference
4978:
3972:"Heat flow and depth to a possible internal ocean on Triton"
3546:
Seasons Discovered on Neptune's Moon Triton — Space.com
1808:
Neptune (top) and Triton (bottom) three days after flyby of
7848:
7336:
5803:
5614:
10.1130/0091-7613(1993)021<0299:DOTARO>2.3.CO;2
5437:
Triton's Lineaments: Complex Morphology and Stress Patterns
5146:"Candidate Cryovolcanic Features in the Outer Solar System"
4591:
4163:
Grundy, W. M.; Buie, M. W.; Spencer, J. R. (October 2002).
3944:
3825:
3723:
1923:, which would launch August 2042 and arrive in April 2057.
1872:
933:
700:
645:
625:
348:
179:
176:
170:
161:
111:
9279:
7312:
6764:
6027:
6005:
5524:
Aksnes, K; Brahic, A; Fulchignoni, M; Marov, M Ya (1990).
5387:
5102:
4700:
2860:
Elliot, J.L.; Strobel, D.F.; Zhu, X.; et al. (2000).
2782:. In Tilman Spohn; Doris Breuer; Torrence Johnson (eds.).
2383:
10 kg, or 0.35%. The mass of the rings is negligible.
6114:
5973:
Abigail Rymer; Brenda Clyde; Kirby Runyon (August 2020).
5896:"Why We Should Use This Jumping Robot to Explore Neptune"
3664:"Pluto and the largest moon of Neptune might be siblings"
3501:
2709:
2616:
1161:
928:
debris disc is likely to have played a substantial role.
916:
damping from tides alone is not thought to be capable of
641:
5219:
4899:
Gray, D (1989). "Voyager 2 Neptune navigation results".
4694:
1152:
ice on the surface, as there are indications of ammonia
1121:
Triton's surface is covered with a transparent layer of
1023:
those of smaller regular moons, dispersing them through
5975:"Neptune Odyssey: Mission to the Neptune-Triton System"
5589:
5517:
5464:
5059:
4585:
4020:
3567:
3442:
The planet Neptune: an historical survey before Voyager
4645:
4540:
4515:
The Grand Tour: A Traveler's Guide to the Solar System
4333:
3539:
3141:
3139:
2904:
2773:
2771:
2769:
2767:
2765:
2763:
2761:
2759:
2757:
2755:
2753:
2751:
1395:
observed are concentrated almost entirely in Triton's
585:. It is the only moon of Neptune massive enough to be
9256:
5435:
Collins, Geoffrey; Schenk, Paul (March 14–18, 1994).
4641:
4639:
4385:"Does Neptune's moon Triton have a subsurface ocean?"
4270:"Overlooked Ocean Worlds Fill the Outer Solar System"
3691:"The coupled orbital and thermal evolution of Triton"
3605:"Triton, Pluto, Centaurs, and Trans-Neptunian Bodies"
3223:"Discovery of Supposed Ring and Satellite of Neptune"
2862:"The Thermal Structure of Triton's Middle Atmosphere"
2749:
2747:
2745:
2743:
2741:
2739:
2737:
2735:
2733:
2731:
2291:
2228:
2164:
2114:
182:
173:
40:
A black-and-white mosaic of Triton, constructed from
5863:"USA.gov: The U.S. Government's Official Web Portal"
5682:
5359:"Gas jet plumes unveil mystery of 'spiders' on Mars"
4752:
Savage, D.; Weaver, D.; Halber, D. (June 24, 1998).
4221:
2837:. Argelander-Institut für Astronomie. Archived from
2606:
1999:
1260:
Triton has a tenuous but well-structured and global
1103:
in the Solar System and is modestly larger than the
167:
158:
155:
114:
108:
105:
4703:"On the thermal structure of Triton's thermosphere"
4339:
3688:
3403:
3170:
3168:
3136:
2488:
10. The total mass of remaining moons is about 0.12
1015:and the scarcity of moons as compared to the other
857:'s orbit (green) in the plane of Neptune's equator.
640:, reflecting a composition of approximately 30–45%
164:
102:
5809:
5733:
5381:
4751:
4636:
4536:
4534:
3507:
3479:"Planet and Satellite Names and their Discoverers"
3147:"Planetary Science Summer School · Jason Dekarske"
2728:
2700:
2698:
2696:
2694:
2692:
2536:
2532:
2530:
2528:
2315:
2253:
2190:
2133:
1957:Enhanced-color map; leading hemisphere is on right
1698:Cantaloupe terrain viewed from 130,000 km by
6546:Listed in approximately increasing distance from
5526:"Working Group for Planetary System Nomenclature"
4931:Monthly Notices of the Royal Astronomical Society
4927:"The origin of the cratering asymmetry on Triton"
4812:
4162:
3598:
3596:
3471:
3295:Monthly Notices of the Royal Astronomical Society
3261:Monthly Notices of the Royal Astronomical Society
3227:Monthly Notices of the Royal Astronomical Society
3182:Monthly Notices of the Royal Astronomical Society
2648:
2646:
2644:
2642:
2640:
2638:
2602:
2600:
2598:
2596:
2594:
2562:
2560:
1503:layer of nitrogen ice, creating a sort of "solid
1341:patterns on Triton's surface and a change in ice
888:Triton's orbit is associated with two tilts, the
773:on October 10, 1846, just 17 days after the
9328:
5562:
4806:
3328:
3326:
3254:
3217:
3174:
3165:
2859:
2778:McKinnon, William B.; Kirk, Randolph L. (2014).
1140:) the remaining 10–20%. Trace ices include 0.1%
601:to do so. Triton is thought to have once been a
6099:from Paul Schenk, Lunar and Planetary Institute
4648:"Voyager 2 at Neptune: Imaging Science Results"
4531:
3005:
2954:
2952:
2950:
2689:
2525:
2264:
2201:
1869:New concepts for missions to the Neptune system
1833:, astronomers suspected that Triton might have
1620:
5868:. Nasa.gov. September 27, 2013. Archived from
5855:
5049:. Planetary Science Vision 2050 Workshop 2017.
4402:
4263:
4261:
4259:
3729:
3593:
3397:
2900:
2898:
2635:
2591:
2572:"Bound for Pluto, Carrying Memories of Triton"
2557:
1871:to be conducted in the 2010s were proposed by
1791:
8046:
7298:
6780:
6522:
6130:
5558:
5556:
5554:
5467:"A shear heating origin for ridges on Triton"
5434:
4974:
4972:
4747:
4745:
4382:
4026:
3323:
3044:
2609:"Planetary Satellite Mean Orbital Parameters"
2332:With respect to Triton's orbit about Neptune.
1472:-like eruptions of nitrogen gas or water and
794:in the 1880s, but was eventually dismantled.
6111:from the USGS Planetary Nomenclature website
6008:"Triton Ocean Worlds Surveyor concept study"
5852:And the following 12 articles pp. 1422–1501.
4285:
4283:
3969:
3211:
2947:
2777:
2095:Calculated on the basis of other parameters.
2077:, a proposed mission that would flyby Triton
769:Triton was discovered by British astronomer
5938:
5915:
5460:
5458:
4256:
4215:
3508:Davies, M.; Rogers, P.; Colvin, T. (1991).
3291:"Observations of Neptune and his satellite"
3288:
2895:
2826:
2386:
2369:
2098:
1771:, which has only three percent of Triton's
1458:Geology of Triton § South polar plumes
1050:
656:of liquid water and a solid rocky-metallic
8277:
8271:
8053:
8039:
7305:
7291:
6787:
6773:
6529:
6515:
6137:
6123:
5551:
5443:. Vol. 25. Houston, TX. p. 277.
5155:
5143:
5096:
5033:
4969:
4924:
4920:
4918:
4776:
4742:
4450:
4448:
3935:
3933:
3788:
3602:
3040:
3038:
3036:
3034:
2853:
1974:
1945:
1559:, the caldera in the center of the image.
1539:Though only observed up close once by the
805:(the Greek god corresponding to the Roman
34:
6338:
5631:
5629:
5627:
5625:
5623:
5583:
5317:
5128:
4952:
4942:
4867:
4821:. Space Telescope Science Institute: 93.
4408:
4376:
4280:
3875:
3865:
3847:
3747:
3714:
3332:
3314:
3280:
3246:
3202:
2972:
2922:
2800:
2706:"Planetary Satellite Physical Parameters"
2680:
2392:The masses of other spherical moons are:
2326:
2089:
1986:Enhanced-color polar maps; south is right
1291:Turbulence at Triton's surface creates a
765:William Lassell, the discoverer of Triton
679:and is geologically young, with very few
668:, Triton's interior may still experience
5893:
5455:
5430:
5428:
5039:
5013:
4892:
4842:"Does global warming make Triton blush?"
3689:Ross, MN; Schubert, G (September 1990).
3682:
3563:
3561:
3014:"Dark Spots in Our Knowledge of Neptune"
2808:"Classic Satellites of the Solar System"
2652:
2537:Williams, David R. (November 23, 2006).
2344:
1803:
1795:
1742:
1693:
1624:
1607:. Combined, they are nearly the size of
1370:
1278:
1251:
955:
840:
797:Triton is named after the Greek sea god
760:
9357:Objects observed by stellar occultation
9352:Astronomical objects discovered in 1846
6063:Voyager 2 Encounters Neptune and Triton
6057:at NASA's Solar System Exploration site
5356:
4915:
4898:
4445:
3963:
3951:from the original on September 27, 2011
3930:
3734:and the Fraction of Contact Binaries".
3670:. June 18, 2024. pp. Space section
3031:
2832:
2619:(Solar System Dynamics). Archived from
2566:
2191:{\displaystyle {\frac {4}{3}}\pi r^{3}}
1283:Clouds observed above Triton's limb by
1099:Triton is the seventh-largest moon and
756:
9329:
5921:
5620:
5350:
5225:
4833:
4156:
3794:
3429:
3255:Lassell, William (December 11, 1846).
3175:Lassell, William (November 12, 1847).
3045:Agnor, C. B.; Hamilton, D. P. (2006).
2607:Jacobson, R. A. — AJ (April 3, 2009).
2270:Escape velocity derived from the mass
2207:Surface gravity derived from the mass
2144:
8034:
7286:
6768:
6510:
6118:
5966:
5944:
5425:
5369:from the original on October 14, 2013
5294:
5292:
5290:
5228:"Cryovolcanism on the icy satellites"
5040:Oleson, Steven R.; Landis, Geoffrey.
4794:from the original on October 16, 2011
4788:Massachusetts Institute of Technology
4503:
4289:
3900:"Triton crashed into Neptune's moons"
3658:
3656:
3558:
3435:
3374:
3372:
3011:
2833:Fischer, Daniel (February 12, 2006).
2104:Surface area derived from the radius
1689:
1555:Close up of the volcanic province of
836:
613:into Neptune's orbit by the latter's
6536:
5999:
4267:
3335:Journal for the History of Astronomy
3123:NASA Jet Propulsion Laboratory (JPL)
2835:"Kuiperoids & Scattered Objects"
2810:. Observatorio ARVAL. Archived from
2716:from the original on August 14, 2009
2498:List of Solar System objects by size
1468:probe in 1989 observed a handful of
944:system similar to that found around
628:), and larger than all of the known
5894:Ferreira, Becky (August 28, 2015).
5357:Burnham, Robert (August 16, 2006).
5277:, search for "Hili" and "Mahilani"
4513:; Hartmann, William K. (May 2005).
4383:Doyle, Amanda (September 6, 2012).
4290:Nimmo, Francis (January 15, 2015).
3012:Chang, Kenneth (October 18, 2014).
2254:{\displaystyle {\frac {Gm}{r^{2}}}}
1360:
591:thin but well-structured atmosphere
13:
6841:
5945:Brown, David W. (March 19, 2019).
5287:
3807:from the original on July 16, 2011
3653:
3417:from the original on March 1, 2012
3369:
3257:"Physical observations on Neptune"
809:). The name was first proposed by
14:
9373:
8060:
6048:
5238:(1–3) (published 1995): 101–113.
4764:from the original on May 16, 2008
3384:www.royalobservatorygreenwich.org
2653:Jacobson, R. A. (April 3, 2009).
1738:
1330:were made of Triton's limb as it
652:of primarily ice atop a probable
9314:
9302:
9290:
9278:
9266:
9241:
9240:
7382:
7376:
7370:
7266:
7257:
7256:
6846:True color NASA image of Neptune
6748:
6739:
6738:
6321:
5151:. Lunar and Planetary Institute.
5144:Schenk, Paul; Prockter, Louise.
5014:Williams, Matt (July 28, 2015).
3483:International Astronomical Union
3177:"Lassell's Satellite of Neptune"
2784:Encyclopedia of the Solar System
2539:"Neptunian Satellite Fact Sheet"
2030:
2016:
2002:
1967:
1938:
1592:
1576:
1548:
1413:
1132:ice comprises 15–35% and frozen
1073:
1059:
151:
98:
5887:
5137:
5053:
5007:
4105:
4079:
4065:
4051:
3910:(3152): 16. November 18, 2017.
3892:
3819:
3111:
2335:
2316:{\displaystyle {\sqrt {2Gm/r}}}
1930:
1909:large strategic science mission
272:156.885° (to Neptune's equator)
8073:List of possible dwarf planets
7006:Neptune-crossing minor planets
6105:from the NASA/JPL Photojournal
5922:Oleson, Steven (May 7, 2015).
4268:Wenz, John (October 4, 2017).
3970:Ruiz, Javier (December 2003).
2513:
1723:in diameter. The depressions (
1603:lakes on Triton, seen west of
1528:are thought to erupt from its
1:
9362:Moons with a retrograde orbit
5832:10.1126/science.246.4936.1417
4925:Mah, J.; Brasser, R. (2019).
4672:10.1126/science.246.4936.1422
4481:10.1126/science.246.4936.1459
3924:10.1016/S0262-4079(17)32247-9
3510:"A Control Network of Triton"
2507:
2362:(160 km), and Jupiter's
2066:, a proposed lander to Triton
1532:each spring in the same way.
1237:
845:The orbit of Triton (red) is
593:. Triton orbits Neptune in a
587:rounded under its own gravity
274:129.608° (to Neptune's orbit)
5926:. NASA Glenn Research Center
5797:10.1016/0019-1035(79)90057-5
5762:10.1016/0019-1035(92)90031-2
5711:10.1126/science.250.4979.435
5660:10.1126/science.250.4979.437
5475:Geophysical Research Letters
5336:10.1016/j.icarus.2021.114835
5197:10.1126/science.250.4979.410
5001:10.1016/j.icarus.2007.07.004
4708:Geophysical Research Letters
4614:10.1126/science.261.5122.751
4563:10.1126/science.261.5122.748
4319:10.1016/j.icarus.2014.01.044
4250:10.1016/j.icarus.2006.06.005
4134:10.1126/science.250.4979.429
3999:10.1016/j.icarus.2003.09.009
3797:"Binary Kuiper Belt Objects"
3695:Geophysical Research Letters
3603:Cruikshank, Dale P. (2004).
3519:. 96(E1) (E1): 15675–15681.
3449:. pp. 150 (see p. 68).
2961:Astronomy & Astrophysics
2911:Astronomy & Astrophysics
2682:10.1088/0004-6256/137/5/4322
1788:50 million years old).
1621:Polar cap, plains and ridges
1428:features found on Triton is
1349:is among the highest in the
792:Royal Observatory, Greenwich
747:Triton Ocean Worlds Surveyor
7:
6794:
5062:Planetary and Space Science
3552:September 17, 2011, at the
2991:10.1051/0004-6361/201014339
2941:10.1051/0004-6361/202348756
1995:
1917:Triton Ocean World Surveyor
1839:atmospheric density of Mars
1792:Observation and exploration
1496:sea spirit, respectively).
1326:In 1997, observations from
463:0° (to orbit about Neptune)
451:5 d, 21 h, 2 min, 53 s
10:
9378:
6144:
5281:February 26, 2009, at the
4362:10.1089/153110701753198918
4033:Sky and Telescope Magazine
3574:Astronomy and Astrophysics
3355:10.1177/002182868401500101
2134:{\displaystyle 4\pi r^{2}}
2047:List of natural satellites
1455:
1417:
1364:
1241:
951:
483:38 K (−235.2 °C)
18:
9236:
9207:
9134:
8822:
8689:
8502:
8479:
8374:
8316:
8293:
8286:
8269:
8116:
8068:
7975:
7809:
7442:
7391:
7368:
7324:
7252:
7231:
7197:
7155:
7134:
7125:
7014:
6993:
6955:
6948:
6853:
6839:
6815:
6802:
6734:
6713:
6678:
6647:
6612:
6603:
6554:
6544:
6483:
6454:
6412:
6387:
6380:
6355:
6337:
6330:
6319:
6291:
6275:
6249:
6208:
6188:
6175:
6152:
6092:Views of the Solar System
5082:10.1016/j.pss.2018.03.010
3629:10.1007/s11214-005-1964-0
2712:(Solar System Dynamics).
1451:
994:locked in resonant orbits
829:, for the eighth moon of
672:through obliquity tides.
548:
519:
514:
499:
487:
477:
467:
455:
443:
429:
415:
388:
373:
347:
335:
321:
295:
290:
278:
260:
247:
230:Orbital period (sidereal)
227:
215:
201:
194:
143:
128:
93:
83:
78:
70:
58:
53:
33:
7827:: 5268 km / 0.413 Earths
5363:Arizona State University
5232:Earth, Moon, and Planets
4901:Astrodynamics Conference
4173:The Astronomical Journal
4073:"Triton: Neptune's Moon"
4059:"12.3: Titan and Triton"
3867:10.3847/1538-3881/aa9184
3836:The Astronomical Journal
3736:The Astronomical Journal
3668:New Scientist UK edition
2660:The Astronomical Journal
2358:(210 km), Uranus's
2154:derived from the radius
2082:
1332:passed in front of stars
1101:sixteenth-largest object
1084:) compared to the Moon (
1051:Physical characteristics
502:Absolute magnitude
446:Sidereal rotation period
291:Physical characteristics
19:Not to be confused with
6980:Heinrich Louis d'Arrest
5244:1995EM&P...67..101K
5074:2018P&SS..160...19M
5016:"Neptune's Moon Triton"
4087:"Triton - NASA Science"
3716:10.1029/GL017i010p01749
3587:1989A&A...219L..23C
3282:10.1093/mnras/7.10.165a
2983:2010A&A...512L...8L
2933:2024A&A...682L..24S
2613:JPL satellite ephemeris
1926:
1234:for some form of life.
833:when he discovered it.
825:, previously chosen by
432:Synodic rotation period
196:Orbital characteristics
16:Largest moon of Neptune
6970:Johann Gottfried Galle
6847:
4027:Medkeff, Jeff (2002).
3316:10.1093/mnras/7.17.307
2889:10.1006/icar.1999.6312
2541:. NASA. Archived from
2317:
2276:gravitational constant
2255:
2213:gravitational constant
2192:
2135:
1812:
1801:
1752:
1709:
1630:
1380:
1288:
1257:
1148:. There could also be
965:
858:
853:compared to a typical
766:
342:10,384,000,000 km
48:located left of center
8077:Former dwarf planets
6845:
4211:on February 18, 2019.
3795:Jewitt, Dave (2005).
3609:Space Science Reviews
3447:John Wiley & Sons
3248:10.1093/mnras/7.9.154
3221:(November 13, 1846).
2841:on September 26, 2011
2521:Hercules, My Shipmate
2519:Robert Graves (1945)
2318:
2256:
2193:
2136:
1913:New Frontiers program
1807:
1799:
1746:
1697:
1628:
1418:Further information:
1374:
1282:
1255:
1211:to maintain a liquid
959:
896:Triton's rotation is
847:opposite in direction
844:
801:(Τρίτων), the son of
764:
706:Triton was the first
550:Composition by volume
9347:Former dwarf planets
9342:Irregular satellites
8000:Planetary-mass moons
6368:Former dwarf planets
5987:on December 15, 2020
5533:Reports on Astronomy
5496:10.1029/2005GL022832
5166:(October 19, 1990).
4954:10.1093/mnras/stz851
4008:on December 12, 2019
3830:(November 5, 2017).
3801:University of Hawaii
3489:on February 12, 2008
3410:Astronomie populaire
3289:Lassell, W. (1847).
3204:10.1093/mnras/10.1.8
2570:(November 5, 2014).
2375:Mass of Triton: 2.14
2289:
2226:
2162:
2112:
1704:, with crosscutting
1661:strike-slip faulting
1244:Atmosphere of Triton
1203:, the most abundant
815:Astronomie Populaire
775:discovery of Neptune
757:Discovery and naming
662:orbital eccentricity
622:seventh-largest moon
6109:Triton nomenclature
6088:labelled Triton map
5875:on October 25, 2012
5824:1989Sci...246.1417S
5789:1979Icar...40..104C
5754:1992Icar..100..221L
5703:1990Sci...250..435I
5652:1990Sci...250..437S
5606:1993Geo....21..299S
5577:1993LPI....24..165B
5488:2005GeoRL..3214202P
5449:1994LPI....25..277C
5403:1998Natur.393..765E
5328:2022Icar..37514835H
5226:Kargel, JS (1994).
5189:1990Sci...250..410S
5121:2021RemS...13.3476S
4993:2007Icar..192..135S
4909:10.2514/6.1990-2876
4860:1999Natur.397..219B
4827:2003ASPC..291...93M
4721:1992GeoRL..19..669S
4664:1989Sci...246.1422S
4658:(4936): 1422–1449.
4606:1993Sci...261..751T
4555:1993Sci...261..748D
4473:1989Sci...246.1459B
4423:1990Natur.344..315I
4354:2001AsBio...1..143I
4311:2015Icar..246....2N
4274:Scientific American
4242:2006Icar..185..258H
4186:2002AJ....124.2273G
4126:1990Sci...250..429N
3991:2003Icar..166..436R
3916:2017NewSc.236...16.
3858:2017AJ....154..208R
3758:2004AJ....127.3023S
3707:1990GeoRL..17.1749R
3621:2005SSRv..116..421C
3525:1991JGR....9615675D
3405:Flammarion, Camille
3347:1984JHA....15....1S
3307:1847MNRAS...7..307L
3273:1847MNRAS...7..297L
3239:1846MNRAS...7..157L
3195:1847MNRAS...8....9B
3153:. December 19, 2023
3099:on October 14, 2016
3074:10.1038/nature04792
3066:2006Natur.441..192A
2881:2000Icar..143..425E
2673:2009AJ....137.4322J
2623:on October 14, 2011
2545:on October 20, 2011
2010:Solar System portal
1865:flew past in 1989.
1424:One of the largest
683:. Young, intricate
544:10 atm) (2022)
540:1.454 Pa (1.43
538:10 atm) (1997)
532:10 atm) (1989)
367:0.00359 Earths
71:Discovery date
30:
7980:Discovery timeline
7314:Natural satellites
6848:
6807:Outline of Neptune
6299:Cantaloupe terrain
5952:The New York Times
5252:10.1007/BF00613296
5130:10.3390/rs13173476
4093:on January 7, 2024
4061:. October 7, 2016.
3941:"Triton (Voyager)"
2313:
2251:
2188:
2131:
2057:Neptune in fiction
2024:Outer space portal
1813:
1802:
1753:
1710:
1690:Cantaloupe terrain
1631:
1397:leading hemisphere
1381:
1299:and instead has a
1289:
1272:(0.014–0.019
1258:
1176:under exposure to
1011:of Neptune's moon
966:
930:Tidal interactions
859:
837:Orbit and rotation
811:Camille Flammarion
767:
490:Apparent magnitude
330:23,018,000 km
60:Discovered by
28:
9254:
9253:
9232:
9231:
8028:
8027:
7828:
7280:
7279:
7227:
7226:
7148:
7121:
7120:
6965:Urbain Le Verrier
6762:
6761:
6709:
6708:
6504:
6503:
6479:
6478:
6376:
6375:
6317:
6316:
5818:(4936): 1417–21.
5697:(4979): 435–437.
5397:(6687): 765–767.
5183:(4979): 410–415.
4790:. June 24, 1998.
4760:. STScI-1998-23.
4729:10.1029/92GL00651
4549:(5122): 748–751.
4524:978-0-7611-3547-0
4467:(4936): 1459–66.
4417:(6264): 315–317.
3701:(10): 1749–1752.
3638:978-1-4020-3362-9
3533:10.1029/91JE00976
3456:978-0-471-96015-7
2793:978-0-12-416034-7
2311:
2249:
2173:
2052:Geology of Triton
1993:
1992:
1895:Discovery Program
1822:flew by in 1989.
1505:greenhouse effect
1367:Geology of Triton
1248:Climate of Triton
1228:organic compounds
1209:radioactive decay
813:in his 1880 book
718:of Triton by the
576:natural satellite
569:
568:
534:1.9 Pa (1.88
528:1.4 Pa (1.38
280:Satellite of
266:129.812° (to the
9369:
9319:
9318:
9317:
9307:
9306:
9305:
9295:
9294:
9293:
9283:
9282:
9271:
9270:
9269:
9262:
9244:
9243:
9225:
9223:
9222:
9200:
9190:
9180:
9170:
9160:
9150:
9136:Detached objects
9127:
9125:
9124:
9115:
9113:
9112:
9103:
9101:
9100:
9091:
9089:
9088:
9079:
9077:
9076:
9067:
9065:
9064:
9055:
9053:
9052:
9043:
9033:
9031:
9030:
9021:
9011:
9001:
8991:
8981:
8974:
8972:
8971:
8962:
8952:
8942:
8940:
8939:
8930:
8920:
8918:
8917:
8908:
8898:
8888:
8878:
8868:
8858:
8848:
8815:
8805:
8795:
8785:
8775:
8765:
8763:
8762:
8753:
8743:
8733:
8723:
8713:
8703:
8682:
8680:
8679:
8670:
8660:
8650:
8640:
8630:
8620:
8610:
8600:
8590:
8580:
8570:
8560:
8558:
8557:
8548:
8538:
8495:
8472:
8470:
8469:
8460:
8450:
8440:
8430:
8420:
8410:
8400:
8367:
8357:
8347:
8291:
8290:
8281:
8275:
8055:
8048:
8041:
8032:
8031:
7823:
7802:
7790:
7776:
7762:
7745:
7733:
7726:
7707:
7693:
7679:
7644:
7630:
7616:
7611:
7589:
7584:
7572:
7565:
7551:
7537:
7520:
7503:
7493:
7484:
7470:
7386:
7380:
7374:
7307:
7300:
7293:
7284:
7283:
7270:
7260:
7259:
7146:
7132:
7131:
7114:
7112:
7111:
7102:
7100:
7099:
7090:
7088:
7087:
7078:
7076:
7075:
7066:
7064:
7063:
7054:
7052:
7051:
7042:
7040:
7039:
6975:John Couch Adams
6953:
6952:
6789:
6782:
6775:
6766:
6765:
6752:
6742:
6741:
6726:Rings of Neptune
6610:
6609:
6538:Moons of Neptune
6531:
6524:
6517:
6508:
6507:
6385:
6384:
6335:
6334:
6325:
6324:
6241:Tuonela Planitia
6231:Leviathan Patera
6186:
6185:
6139:
6132:
6125:
6116:
6115:
6079:The Nine Planets
6066:
6043:
6042:
6040:
6038:
6025:
6019:
6018:
6012:
6003:
5997:
5996:
5994:
5992:
5986:
5980:. Archived from
5979:
5970:
5964:
5963:
5961:
5959:
5942:
5936:
5935:
5933:
5931:
5919:
5913:
5912:
5910:
5908:
5901:Vice Motherboard
5891:
5885:
5884:
5882:
5880:
5874:
5867:
5859:
5853:
5851:
5807:
5801:
5800:
5772:
5766:
5765:
5737:
5731:
5730:
5686:
5680:
5679:
5646:(4979): 437–39.
5633:
5618:
5617:
5587:
5581:
5580:
5560:
5549:
5548:
5546:
5544:
5530:
5521:
5515:
5514:
5512:
5510:
5471:
5462:
5453:
5452:
5432:
5423:
5422:
5385:
5379:
5378:
5376:
5374:
5354:
5348:
5347:
5321:
5296:
5285:
5270:
5264:
5263:
5223:
5217:
5216:
5172:
5164:Shoemaker, E. M.
5159:
5153:
5152:
5150:
5141:
5135:
5134:
5132:
5100:
5094:
5093:
5057:
5051:
5050:
5048:
5037:
5031:
5030:
5028:
5026:
5011:
5005:
5004:
4976:
4967:
4966:
4956:
4946:
4922:
4913:
4912:
4896:
4890:
4889:
4871:
4854:(6716): 219–20.
4837:
4831:
4830:
4810:
4804:
4803:
4801:
4799:
4780:
4774:
4773:
4771:
4769:
4749:
4740:
4739:
4737:
4735:
4698:
4692:
4691:
4643:
4634:
4633:
4589:
4583:
4582:
4538:
4529:
4528:
4507:
4501:
4500:
4452:
4443:
4442:
4431:10.1038/344315a0
4406:
4400:
4399:
4397:
4395:
4380:
4374:
4373:
4337:
4331:
4330:
4296:
4287:
4278:
4277:
4265:
4254:
4253:
4219:
4213:
4212:
4210:
4204:. Archived from
4180:(4): 2273–2278.
4169:
4160:
4154:
4153:
4120:(4979): 429–31.
4109:
4103:
4102:
4100:
4098:
4089:. Archived from
4083:
4077:
4076:
4069:
4063:
4062:
4055:
4049:
4048:
4046:
4044:
4035:. Archived from
4024:
4018:
4017:
4015:
4013:
4007:
4001:. Archived from
3976:
3967:
3961:
3960:
3958:
3956:
3947:. June 1, 2005.
3937:
3928:
3927:
3896:
3890:
3889:
3879:
3869:
3851:
3826:Raluca Rufu and
3823:
3817:
3816:
3814:
3812:
3792:
3786:
3785:
3751:
3749:astro-ph/0402277
3742:(5): 3023–3033.
3727:
3721:
3720:
3718:
3686:
3680:
3679:
3677:
3675:
3660:
3651:
3650:
3615:(1–2): 421–439.
3600:
3591:
3590:
3581:(1–2): L23–L26.
3565:
3556:
3543:
3537:
3536:
3514:
3505:
3499:
3498:
3496:
3494:
3485:. Archived from
3475:
3469:
3468:
3433:
3427:
3426:
3424:
3422:
3401:
3395:
3394:
3392:
3390:
3376:
3367:
3366:
3330:
3321:
3320:
3318:
3286:
3284:
3252:
3250:
3219:Lassell, William
3215:
3209:
3208:
3206:
3172:
3163:
3162:
3160:
3158:
3143:
3134:
3133:
3131:
3129:
3115:
3109:
3108:
3106:
3104:
3098:
3092:. Archived from
3051:
3042:
3029:
3028:
3026:
3024:
3009:
3003:
3002:
2976:
2956:
2945:
2944:
2926:
2902:
2893:
2892:
2866:
2857:
2851:
2850:
2848:
2846:
2830:
2824:
2823:
2821:
2819:
2804:
2798:
2797:
2775:
2726:
2725:
2723:
2721:
2702:
2687:
2686:
2684:
2667:(5): 4322–4329.
2650:
2633:
2632:
2630:
2628:
2604:
2589:
2588:
2586:
2584:
2564:
2555:
2554:
2552:
2550:
2534:
2523:
2517:
2501:
2495:
2491:
2487:
2479:
2471:
2463:
2455:
2447:
2439:
2431:
2423:
2415:
2407:
2399:
2390:
2384:
2382:
2378:
2373:
2367:
2348:
2342:
2339:
2333:
2330:
2324:
2322:
2320:
2319:
2314:
2312:
2307:
2293:
2268:
2262:
2260:
2258:
2257:
2252:
2250:
2248:
2247:
2238:
2230:
2205:
2199:
2197:
2195:
2194:
2189:
2187:
2186:
2174:
2166:
2148:
2142:
2140:
2138:
2137:
2132:
2130:
2129:
2102:
2096:
2093:
2040:
2038:Astronomy portal
2035:
2034:
2033:
2026:
2021:
2020:
2019:
2012:
2007:
2006:
2005:
1978:
1971:
1949:
1942:
1931:
1816:satellite until
1722:
1644:Leviathan Patera
1605:Leviathan Patera
1596:
1580:
1557:Leviathan Patera
1552:
1517:
1430:Leviathan Patera
1377:geomorphological
1361:Surface features
1310:
1308:
1213:subsurface ocean
1077:
1063:
1041:migrated outward
912:of almost zero.
863:retrograde orbit
667:
654:subsurface ocean
639:
595:retrograde orbit
543:
537:
531:
425:
410:
401:
384:
368:
363:
361:
357:
343:
331:
309:
307:
237:
223:
211:
189:
188:
185:
184:
181:
178:
175:
172:
169:
166:
163:
160:
157:
124:
123:
120:
119:
116:
113:
110:
107:
104:
74:October 10, 1846
46:Leviathan Patera
38:
31:
27:
9377:
9376:
9372:
9371:
9370:
9368:
9367:
9366:
9327:
9326:
9325:
9315:
9313:
9303:
9301:
9291:
9289:
9277:
9267:
9265:
9257:
9255:
9250:
9228:
9220:
9219:
9216:
9203:
9198:
9193:
9188:
9183:
9178:
9173:
9168:
9163:
9158:
9153:
9148:
9143:
9130:
9122:
9121:
9118:
9110:
9109:
9106:
9098:
9097:
9094:
9086:
9085:
9082:
9074:
9073:
9070:
9062:
9061:
9058:
9050:
9049:
9046:
9041:
9036:
9028:
9027:
9024:
9019:
9014:
9009:
9004:
8999:
8994:
8989:
8984:
8977:
8969:
8968:
8965:
8960:
8955:
8950:
8945:
8937:
8936:
8933:
8928:
8923:
8915:
8914:
8911:
8906:
8901:
8896:
8891:
8886:
8881:
8876:
8871:
8866:
8861:
8856:
8851:
8846:
8841:
8818:
8813:
8808:
8803:
8798:
8793:
8788:
8783:
8778:
8773:
8768:
8760:
8759:
8756:
8751:
8746:
8741:
8736:
8731:
8726:
8721:
8716:
8711:
8706:
8701:
8696:
8685:
8677:
8676:
8673:
8668:
8663:
8658:
8653:
8648:
8643:
8638:
8633:
8628:
8623:
8618:
8613:
8608:
8603:
8598:
8593:
8588:
8583:
8578:
8573:
8568:
8563:
8555:
8554:
8551:
8546:
8541:
8536:
8531:
8498:
8493:
8488:
8475:
8467:
8466:
8463:
8458:
8453:
8448:
8443:
8438:
8433:
8428:
8423:
8418:
8413:
8408:
8403:
8398:
8393:
8370:
8365:
8360:
8355:
8350:
8345:
8340:
8312:
8282:
8276:
8267:
8112:
8064:
8059:
8029:
8024:
7990:Irregular moons
7971:
7811:
7805:
7800:
7795:
7786:
7772:
7758:
7743:
7738:
7729:
7722:
7703:
7689:
7675:
7667:Jupiter trojans
7640:
7626:
7614:
7609:
7587:
7582:
7568:
7561:
7547:
7535:
7516:
7501:
7496:
7489:
7480:
7466:
7445:
7438:
7394:
7387:
7381:
7375:
7366:
7327:
7320:
7311:
7281:
7276:
7248:
7223:
7212:Mariner Mark II
7193:
7170:Neptune Odyssey
7151:
7117:
7109:
7108:
7105:
7097:
7096:
7093:
7085:
7084:
7081:
7073:
7072:
7069:
7061:
7060:
7057:
7049:
7048:
7045:
7037:
7036:
7033:
7010:
6989:
6985:William Lassell
6944:
6849:
6837:
6828:Small Dark Spot
6823:Great Dark Spot
6811:
6798:
6793:
6763:
6758:
6730:
6721:Neptune trojans
6705:
6674:
6643:
6599:
6550:
6540:
6535:
6505:
6500:
6475:
6450:
6427:Shensuo program
6422:Neptune Odyssey
6414:
6408:
6395:Voyager program
6372:
6351:
6347:William Lassell
6326:
6322:
6313:
6287:
6271:
6245:
6204:
6177:
6171:
6148:
6143:
6061:
6051:
6046:
6036:
6034:
6026:
6022:
6010:
6004:
6000:
5990:
5988:
5984:
5977:
5971:
5967:
5957:
5955:
5943:
5939:
5929:
5927:
5920:
5916:
5906:
5904:
5892:
5888:
5878:
5876:
5872:
5865:
5861:
5860:
5856:
5808:
5804:
5773:
5769:
5738:
5734:
5687:
5683:
5634:
5621:
5588:
5584:
5561:
5552:
5542:
5540:
5528:
5522:
5518:
5508:
5506:
5469:
5463:
5456:
5433:
5426:
5386:
5382:
5372:
5370:
5355:
5351:
5297:
5288:
5283:Wayback Machine
5271:
5267:
5224:
5220:
5170:
5160:
5156:
5148:
5142:
5138:
5101:
5097:
5058:
5054:
5046:
5038:
5034:
5024:
5022:
5012:
5008:
4977:
4970:
4923:
4916:
4897:
4893:
4838:
4834:
4811:
4807:
4797:
4795:
4782:
4781:
4777:
4767:
4765:
4750:
4743:
4733:
4731:
4699:
4695:
4644:
4637:
4600:(5122): 751–4.
4590:
4586:
4539:
4532:
4525:
4508:
4504:
4453:
4446:
4407:
4403:
4393:
4391:
4381:
4377:
4338:
4334:
4294:
4288:
4281:
4266:
4257:
4220:
4216:
4208:
4167:
4161:
4157:
4110:
4106:
4096:
4094:
4085:
4084:
4080:
4075:. January 2010.
4071:
4070:
4066:
4057:
4056:
4052:
4042:
4040:
4039:on May 23, 2008
4025:
4021:
4011:
4009:
4005:
3974:
3968:
3964:
3954:
3952:
3939:
3938:
3931:
3898:
3897:
3893:
3824:
3820:
3810:
3808:
3793:
3789:
3733:
3728:
3724:
3687:
3683:
3673:
3671:
3662:
3661:
3654:
3639:
3601:
3594:
3566:
3559:
3554:Wayback Machine
3544:
3540:
3517:J. Geophys. Res
3512:
3506:
3502:
3492:
3490:
3477:
3476:
3472:
3457:
3434:
3430:
3420:
3418:
3413:. p. 591.
3402:
3398:
3388:
3386:
3378:
3377:
3370:
3331:
3324:
3301:(17): 307–308.
3287:
3267:(10): 167–168.
3253:
3216:
3212:
3173:
3166:
3156:
3154:
3145:
3144:
3137:
3127:
3125:
3117:
3116:
3112:
3102:
3100:
3096:
3060:(7090): 192–4.
3049:
3043:
3032:
3022:
3020:
3010:
3006:
2957:
2948:
2903:
2896:
2864:
2858:
2854:
2844:
2842:
2831:
2827:
2817:
2815:
2814:on July 9, 2011
2806:
2805:
2801:
2794:
2776:
2729:
2719:
2717:
2704:
2703:
2690:
2651:
2636:
2626:
2624:
2605:
2592:
2582:
2580:
2568:Overbye, Dennis
2565:
2558:
2548:
2546:
2535:
2526:
2518:
2514:
2510:
2505:
2504:
2493:
2489:
2485:
2477:
2469:
2461:
2453:
2445:
2437:
2429:
2421:
2413:
2405:
2397:
2391:
2387:
2380:
2376:
2374:
2370:
2352:irregular moons
2349:
2345:
2340:
2336:
2331:
2327:
2303:
2292:
2290:
2287:
2286:
2281:and the radius
2269:
2265:
2243:
2239:
2231:
2229:
2227:
2224:
2223:
2218:and the radius
2206:
2202:
2182:
2178:
2165:
2163:
2160:
2159:
2149:
2145:
2125:
2121:
2113:
2110:
2109:
2103:
2099:
2094:
2090:
2085:
2080:
2036:
2031:
2029:
2022:
2017:
2015:
2008:
2003:
2001:
1998:
1989:
1988:
1987:
1985:
1980:
1979:
1972:
1960:
1959:
1958:
1956:
1951:
1950:
1943:
1929:
1905:Neptune Odyssey
1897:under the name
1835:liquid nitrogen
1794:
1741:
1720:
1692:
1623:
1616:
1597:
1588:
1581:
1572:
1553:
1530:south polar cap
1526:geysers on Mars
1523:
1515:
1485:(named after a
1460:
1454:
1422:
1416:
1404:
1375:Interpretative
1369:
1363:
1306:
1304:
1250:
1242:Main articles:
1240:
1187:, into a solid
1146:carbon monoxide
1126:frozen nitrogen
1097:
1096:
1095:
1094:
1093:
1078:
1069:
1068:
1067:
1064:
1053:
1009:eccentric orbit
954:
867:irregular moons
839:
771:William Lassell
759:
712:William Lassell
697:carbon monoxide
677:frozen nitrogen
665:
638:2.061 g/cm
637:
574:is the largest
563:carbon monoxide
541:
539:
535:
533:
529:
525:
507:
492:
460:
448:
434:
424:1.455 km/s
423:
420:
418:Escape velocity
403:
396:
393:
391:Surface gravity
383:2.061 g/cm
382:
379:
366:
364:
359:
355:
353:
341:
329:
326:
316:
313:
305:
303:
300:
273:
271:
253:
238:
236:5.876854 d
235:
232:
221:
210:354,759 km
209:
206:
204:Semi-major axis
154:
150:
131:
101:
97:
86:
65:William Lassell
49:
24:
17:
12:
11:
5:
9375:
9365:
9364:
9359:
9354:
9349:
9344:
9339:
9324:
9323:
9311:
9299:
9287:
9275:
9252:
9251:
9249:
9248:
9237:
9234:
9233:
9230:
9229:
9227:
9226:
9213:
9211:
9205:
9204:
9202:
9201:
9196:
9191:
9186:
9181:
9176:
9171:
9166:
9161:
9156:
9151:
9146:
9140:
9138:
9132:
9131:
9129:
9128:
9116:
9104:
9092:
9080:
9068:
9056:
9044:
9039:
9034:
9022:
9017:
9012:
9007:
9002:
8997:
8992:
8987:
8982:
8975:
8963:
8958:
8953:
8948:
8943:
8931:
8926:
8921:
8909:
8904:
8899:
8894:
8889:
8884:
8879:
8874:
8869:
8864:
8859:
8854:
8849:
8844:
8839:
8834:
8832:Gǃkúnǁʼhòmdímà
8828:
8826:
8824:Scattered disc
8820:
8819:
8817:
8816:
8811:
8806:
8801:
8796:
8791:
8786:
8781:
8776:
8771:
8766:
8754:
8749:
8744:
8739:
8734:
8729:
8724:
8719:
8714:
8709:
8704:
8699:
8693:
8691:
8687:
8686:
8684:
8683:
8671:
8666:
8661:
8656:
8651:
8646:
8641:
8636:
8631:
8626:
8621:
8616:
8611:
8606:
8601:
8596:
8591:
8586:
8581:
8576:
8571:
8566:
8561:
8549:
8544:
8539:
8534:
8529:
8524:
8519:
8514:
8508:
8506:
8500:
8499:
8497:
8496:
8491:
8485:
8483:
8477:
8476:
8474:
8473:
8461:
8456:
8451:
8446:
8441:
8436:
8431:
8426:
8421:
8416:
8411:
8406:
8401:
8396:
8391:
8386:
8380:
8378:
8372:
8371:
8369:
8368:
8363:
8358:
8353:
8348:
8343:
8338:
8333:
8328:
8322:
8320:
8314:
8313:
8311:
8310:
8305:
8299:
8297:
8288:
8284:
8283:
8270:
8268:
8266:
8265:
8258:
8257:
8256:
8244:
8243:
8242:
8230:
8229:
8228:
8223:
8211:
8210:
8209:
8197:
8196:
8195:
8190:
8178:
8177:
8176:
8171:
8166:
8154:
8153:
8152:
8140:
8139:
8138:
8133:
8120:
8118:
8114:
8113:
8111:
8110:
8105:
8100:
8099:
8098:
8093:
8088:
8083:
8075:
8069:
8066:
8065:
8058:
8057:
8050:
8043:
8035:
8026:
8025:
8023:
8022:
8017:
8012:
8007:
8002:
7997:
7992:
7987:
7982:
7976:
7973:
7972:
7970:
7969:
7966:
7961:
7956:
7951:
7946:
7941:
7936:
7931:
7926:
7921:
7916:
7911:
7906:
7901:
7896:
7891:
7886:
7881:
7876:
7871:
7866:
7861:
7856:
7851:
7846:
7841:
7836:
7831:
7830:
7829:
7815:
7813:
7807:
7806:
7804:
7803:
7798:
7793:
7792:
7791:
7782:Gǃkúnǁʼhòmdímà
7779:
7778:
7777:
7765:
7764:
7763:
7751:
7746:
7741:
7736:
7735:
7734:
7727:
7715:
7711:
7710:
7709:
7708:
7696:
7695:
7694:
7682:
7681:
7680:
7668:
7664:
7663:
7657:
7652:
7647:
7646:
7645:
7633:
7632:
7631:
7619:
7618:
7617:
7612:
7602:
7597:
7592:
7591:
7590:
7585:
7575:
7574:
7573:
7566:
7554:
7553:
7552:
7540:
7539:
7538:
7528:
7523:
7522:
7521:
7509:
7505:
7504:
7499:
7494:
7487:
7486:
7485:
7473:
7472:
7471:
7459:
7454:
7450:
7448:
7440:
7439:
7437:
7436:
7431:
7426:
7421:
7416:
7411:
7406:
7400:
7398:
7389:
7388:
7369:
7367:
7365:
7364:
7359:
7354:
7349:
7344:
7339:
7333:
7331:
7322:
7321:
7310:
7309:
7302:
7295:
7287:
7278:
7277:
7275:
7274:
7264:
7253:
7250:
7249:
7247:
7246:
7241:
7235:
7233:
7229:
7228:
7225:
7224:
7222:
7221:
7218:New Horizons 2
7214:
7209:
7201:
7199:
7195:
7194:
7192:
7191:
7184:
7177:
7172:
7167:
7159:
7157:
7153:
7152:
7150:
7149:
7138:
7136:
7129:
7123:
7122:
7119:
7118:
7116:
7115:
7103:
7091:
7079:
7067:
7055:
7043:
7031:
7026:
7020:
7018:
7012:
7011:
7009:
7008:
7003:
6997:
6995:
6991:
6990:
6988:
6987:
6982:
6977:
6972:
6967:
6961:
6959:
6950:
6946:
6945:
6943:
6942:
6937:
6932:
6927:
6922:
6917:
6912:
6907:
6902:
6895:
6890:
6885:
6880:
6875:
6870:
6865:
6859:
6857:
6851:
6850:
6840:
6838:
6836:
6835:
6830:
6825:
6819:
6817:
6813:
6812:
6810:
6809:
6803:
6800:
6799:
6792:
6791:
6784:
6777:
6769:
6760:
6759:
6757:
6756:
6746:
6735:
6732:
6731:
6729:
6728:
6723:
6717:
6715:
6711:
6710:
6707:
6706:
6704:
6703:
6698:
6693:
6688:
6682:
6680:
6676:
6675:
6673:
6672:
6667:
6662:
6657:
6651:
6649:
6645:
6644:
6642:
6641:
6640:
6639:
6634:
6629:
6616:
6614:
6607:
6601:
6600:
6598:
6597:
6592:
6587:
6582:
6577:
6572:
6567:
6561:
6559:
6552:
6551:
6545:
6542:
6541:
6534:
6533:
6526:
6519:
6511:
6502:
6501:
6499:
6498:
6493:
6487:
6485:
6481:
6480:
6477:
6476:
6474:
6473:
6470:New Horizons 2
6466:
6458:
6456:
6452:
6451:
6449:
6448:
6441:
6434:
6433:
6432:
6424:
6418:
6416:
6410:
6409:
6407:
6406:
6405:
6404:
6391:
6389:
6382:
6378:
6377:
6374:
6373:
6371:
6370:
6365:
6359:
6357:
6353:
6352:
6350:
6349:
6343:
6341:
6332:
6328:
6327:
6320:
6318:
6315:
6314:
6312:
6311:
6306:
6301:
6295:
6293:
6289:
6288:
6286:
6285:
6279:
6277:
6273:
6272:
6270:
6269:
6264:
6259:
6253:
6251:
6247:
6246:
6244:
6243:
6238:
6236:Ruach Planitia
6233:
6228:
6223:
6218:
6216:Cipango Planum
6212:
6210:
6206:
6205:
6203:
6202:
6199:
6196:
6192:
6190:
6183:
6173:
6172:
6170:
6169:
6164:
6159:
6153:
6150:
6149:
6142:
6141:
6134:
6127:
6119:
6113:
6112:
6106:
6100:
6094:
6081:
6072:
6058:
6055:Triton profile
6050:
6049:External links
6047:
6045:
6044:
6020:
5998:
5965:
5937:
5914:
5886:
5854:
5802:
5783:(1): 104–114.
5767:
5732:
5681:
5619:
5600:(4): 299–302.
5582:
5550:
5516:
5482:(14): L14202.
5454:
5424:
5380:
5349:
5286:
5265:
5218:
5154:
5136:
5109:Remote Sensing
5095:
5052:
5032:
5020:Universe Today
5006:
4968:
4914:
4891:
4832:
4805:
4775:
4741:
4715:(7): 669–672.
4693:
4635:
4584:
4530:
4523:
4502:
4457:Dessler, A. J.
4444:
4401:
4375:
4332:
4279:
4255:
4236:(1): 258–273.
4214:
4194:10.1086/342933
4155:
4104:
4078:
4064:
4050:
4029:"Lunar Albedo"
4019:
3985:(2): 436–439.
3962:
3929:
3891:
3818:
3787:
3766:10.1086/383558
3731:
3722:
3681:
3652:
3637:
3592:
3557:
3538:
3500:
3470:
3455:
3439:(April 1996).
3437:Moore, Patrick
3428:
3396:
3368:
3322:
3210:
3164:
3151:Jason Dekarske
3135:
3110:
3030:
3018:New York Times
3004:
2946:
2894:
2875:(2): 425–428.
2852:
2825:
2799:
2792:
2727:
2688:
2634:
2590:
2577:New York Times
2556:
2524:
2511:
2509:
2506:
2503:
2502:
2385:
2368:
2343:
2334:
2325:
2310:
2306:
2302:
2299:
2296:
2263:
2246:
2242:
2237:
2234:
2200:
2185:
2181:
2177:
2172:
2169:
2143:
2128:
2124:
2120:
2117:
2097:
2087:
2086:
2084:
2081:
2079:
2078:
2072:
2067:
2059:
2054:
2049:
2043:
2042:
2041:
2027:
2013:
1997:
1994:
1991:
1990:
1982:
1981:
1973:
1966:
1965:
1964:
1963:
1961:
1953:
1952:
1944:
1937:
1936:
1935:
1934:
1928:
1925:
1793:
1790:
1757:impact craters
1740:
1739:Impact craters
1737:
1691:
1688:
1665:Europan lineae
1622:
1619:
1618:
1617:
1598:
1591:
1589:
1582:
1575:
1573:
1569:Ruach Planitia
1554:
1547:
1521:
1483:Mahilani plume
1456:Main article:
1453:
1450:
1415:
1412:
1402:
1393:impact craters
1365:Main article:
1362:
1359:
1239:
1236:
1134:carbon dioxide
1079:
1072:
1071:
1070:
1065:
1058:
1057:
1056:
1055:
1054:
1052:
1049:
1027:interactions.
953:
950:
898:tidally locked
838:
835:
758:
755:
708:Neptunian moon
681:impact craters
567:
566:
552:
546:
545:
526:
520:
517:
516:
512:
511:
508:
500:
497:
496:
493:
488:
485:
484:
481:
475:
474:
471:
465:
464:
461:
456:
453:
452:
449:
444:
441:
440:
435:
430:
427:
426:
421:
416:
413:
412:
411:) (0.48 Moons)
394:
389:
386:
385:
380:
374:
371:
370:
351:
345:
344:
339:
333:
332:
327:
322:
319:
318:
314:
311:
301:
296:
293:
292:
288:
287:
282:
276:
275:
264:
258:
257:
254:
248:
245:
244:
233:
228:
225:
224:
219:
213:
212:
207:
202:
199:
198:
192:
191:
147:
141:
140:
132:
129:
126:
125:
95:
91:
90:
87:
84:
81:
80:
76:
75:
72:
68:
67:
62:
56:
55:
51:
50:
39:
15:
9:
6:
4:
3:
2:
9374:
9363:
9360:
9358:
9355:
9353:
9350:
9348:
9345:
9343:
9340:
9338:
9337:Triton (moon)
9335:
9334:
9332:
9322:
9312:
9310:
9300:
9298:
9288:
9286:
9281:
9276:
9274:
9264:
9263:
9260:
9247:
9239:
9238:
9235:
9224:
9215:
9214:
9212:
9210:
9206:
9199:
9192:
9189:
9182:
9179:
9172:
9169:
9162:
9159:
9152:
9149:
9142:
9141:
9139:
9137:
9133:
9126:
9117:
9114:
9105:
9102:
9093:
9090:
9081:
9078:
9069:
9066:
9057:
9054:
9045:
9042:
9035:
9032:
9023:
9020:
9013:
9010:
9003:
9000:
8993:
8990:
8983:
8980:
8976:
8973:
8964:
8961:
8954:
8951:
8944:
8941:
8932:
8929:
8922:
8919:
8910:
8907:
8900:
8897:
8890:
8887:
8880:
8877:
8870:
8867:
8860:
8857:
8850:
8847:
8840:
8838:
8835:
8833:
8830:
8829:
8827:
8825:
8821:
8814:
8807:
8804:
8797:
8794:
8787:
8784:
8777:
8774:
8767:
8764:
8755:
8752:
8745:
8742:
8735:
8732:
8725:
8722:
8715:
8712:
8705:
8702:
8695:
8694:
8692:
8688:
8681:
8672:
8669:
8662:
8659:
8652:
8649:
8642:
8639:
8632:
8629:
8622:
8619:
8612:
8609:
8602:
8599:
8592:
8589:
8582:
8579:
8572:
8569:
8562:
8559:
8550:
8547:
8540:
8537:
8530:
8528:
8525:
8523:
8520:
8518:
8515:
8513:
8510:
8509:
8507:
8505:
8501:
8494:
8487:
8486:
8484:
8482:
8478:
8471:
8462:
8459:
8452:
8449:
8442:
8439:
8432:
8429:
8422:
8419:
8412:
8409:
8402:
8399:
8392:
8390:
8387:
8385:
8382:
8381:
8379:
8377:
8373:
8366:
8359:
8356:
8349:
8346:
8339:
8337:
8334:
8332:
8329:
8327:
8324:
8323:
8321:
8319:
8315:
8309:
8306:
8304:
8301:
8300:
8298:
8296:
8295:Asteroid belt
8292:
8289:
8285:
8280:
8274:
8264:
8263:
8259:
8255:
8252:
8251:
8250:
8249:
8245:
8241:
8238:
8237:
8236:
8235:
8231:
8227:
8224:
8222:
8219:
8218:
8217:
8216:
8212:
8208:
8205:
8204:
8203:
8202:
8198:
8194:
8191:
8189:
8186:
8185:
8184:
8183:
8179:
8175:
8172:
8170:
8167:
8165:
8162:
8161:
8160:
8159:
8155:
8151:
8148:
8147:
8146:
8145:
8141:
8137:
8134:
8132:
8129:
8128:
8127:
8126:
8122:
8121:
8119:
8115:
8109:
8106:
8104:
8101:
8097:
8094:
8092:
8089:
8087:
8084:
8082:
8079:
8078:
8076:
8074:
8071:
8070:
8067:
8063:
8062:Dwarf planets
8056:
8051:
8049:
8044:
8042:
8037:
8036:
8033:
8021:
8018:
8016:
8015:Regular moons
8013:
8011:
8008:
8006:
8003:
8001:
7998:
7996:
7993:
7991:
7988:
7986:
7983:
7981:
7978:
7977:
7974:
7967:
7965:
7962:
7960:
7957:
7955:
7952:
7950:
7947:
7945:
7942:
7940:
7937:
7935:
7932:
7930:
7927:
7925:
7922:
7920:
7917:
7915:
7912:
7910:
7907:
7905:
7902:
7900:
7897:
7895:
7892:
7890:
7887:
7885:
7882:
7880:
7877:
7875:
7872:
7870:
7867:
7865:
7862:
7860:
7857:
7855:
7852:
7850:
7847:
7845:
7842:
7840:
7837:
7835:
7832:
7826:
7822:
7821:
7820:
7817:
7816:
7814:
7808:
7801:
7794:
7789:
7785:
7784:
7783:
7780:
7775:
7771:
7770:
7769:
7766:
7761:
7757:
7756:
7755:
7752:
7750:
7747:
7744:
7737:
7732:
7728:
7725:
7721:
7720:
7719:
7716:
7713:
7712:
7706:
7702:
7701:
7700:
7697:
7692:
7688:
7687:
7686:
7683:
7678:
7674:
7673:
7672:
7669:
7666:
7665:
7661:
7658:
7656:
7653:
7651:
7648:
7643:
7639:
7638:
7637:
7634:
7629:
7625:
7624:
7623:
7620:
7613:
7608:
7607:
7606:
7603:
7601:
7598:
7596:
7593:
7586:
7581:
7580:
7579:
7576:
7571:
7567:
7564:
7560:
7559:
7558:
7555:
7550:
7546:
7545:
7544:
7541:
7534:
7533:
7532:
7529:
7527:
7524:
7519:
7515:
7514:
7513:
7510:
7507:
7506:
7502:
7495:
7492:
7488:
7483:
7479:
7478:
7477:
7474:
7469:
7465:
7464:
7463:
7460:
7458:
7455:
7452:
7451:
7449:
7447:
7441:
7435:
7432:
7430:
7427:
7425:
7422:
7420:
7417:
7415:
7412:
7410:
7407:
7405:
7402:
7401:
7399:
7396:
7390:
7385:
7379:
7373:
7363:
7360:
7358:
7355:
7353:
7350:
7348:
7345:
7343:
7340:
7338:
7335:
7334:
7332:
7329:
7323:
7319:
7315:
7308:
7303:
7301:
7296:
7294:
7289:
7288:
7285:
7273:
7269:
7265:
7263:
7255:
7254:
7251:
7245:
7242:
7240:
7237:
7236:
7234:
7230:
7220:
7219:
7215:
7213:
7210:
7208:
7207:
7203:
7202:
7200:
7196:
7190:
7189:
7185:
7183:
7182:
7181:Triton Hopper
7178:
7176:
7173:
7171:
7168:
7166:
7165:
7161:
7160:
7158:
7154:
7145:
7144:
7140:
7139:
7137:
7133:
7130:
7128:
7124:
7113:
7104:
7101:
7092:
7089:
7080:
7077:
7068:
7065:
7056:
7053:
7044:
7041:
7032:
7030:
7027:
7025:
7024:385571 Otrera
7022:
7021:
7019:
7017:
7013:
7007:
7004:
7002:
6999:
6998:
6996:
6992:
6986:
6983:
6981:
6978:
6976:
6973:
6971:
6968:
6966:
6963:
6962:
6960:
6958:
6954:
6951:
6947:
6941:
6938:
6936:
6933:
6931:
6928:
6926:
6923:
6921:
6918:
6916:
6913:
6911:
6908:
6906:
6903:
6901:
6900:
6896:
6894:
6891:
6889:
6886:
6884:
6881:
6879:
6876:
6874:
6871:
6869:
6866:
6864:
6861:
6860:
6858:
6856:
6852:
6844:
6834:
6831:
6829:
6826:
6824:
6821:
6820:
6818:
6814:
6808:
6805:
6804:
6801:
6797:
6790:
6785:
6783:
6778:
6776:
6771:
6770:
6767:
6755:
6751:
6747:
6745:
6737:
6736:
6733:
6727:
6724:
6722:
6719:
6718:
6716:
6712:
6702:
6699:
6697:
6694:
6692:
6689:
6687:
6684:
6683:
6681:
6677:
6671:
6668:
6666:
6663:
6661:
6658:
6656:
6653:
6652:
6650:
6646:
6638:
6635:
6633:
6630:
6628:
6625:
6624:
6623:
6622:
6618:
6617:
6615:
6611:
6608:
6606:
6602:
6596:
6593:
6591:
6588:
6586:
6583:
6581:
6578:
6576:
6573:
6571:
6568:
6566:
6563:
6562:
6560:
6557:
6553:
6549:
6543:
6539:
6532:
6527:
6525:
6520:
6518:
6513:
6512:
6509:
6497:
6494:
6492:
6489:
6488:
6486:
6482:
6472:
6471:
6467:
6465:
6464:
6460:
6459:
6457:
6453:
6447:
6446:
6445:Triton Hopper
6442:
6440:
6439:
6435:
6430:
6429:
6428:
6425:
6423:
6420:
6419:
6417:
6411:
6403:
6402:
6398:
6397:
6396:
6393:
6392:
6390:
6386:
6383:
6379:
6369:
6366:
6364:
6361:
6360:
6358:
6354:
6348:
6345:
6344:
6342:
6340:
6336:
6333:
6329:
6310:
6307:
6305:
6302:
6300:
6297:
6296:
6294:
6290:
6284:
6281:
6280:
6278:
6274:
6268:
6265:
6263:
6260:
6258:
6257:Kraken Catena
6255:
6254:
6252:
6248:
6242:
6239:
6237:
6234:
6232:
6229:
6227:
6224:
6222:
6221:Dilolo Patera
6219:
6217:
6214:
6213:
6211:
6209:Cryovolcanism
6207:
6201:Uhlanga Regio
6200:
6197:
6195:Bubembe Regio
6194:
6193:
6191:
6187:
6184:
6181:
6174:
6168:
6165:
6163:
6160:
6158:
6155:
6154:
6151:
6147:
6140:
6135:
6133:
6128:
6126:
6121:
6120:
6117:
6110:
6107:
6104:
6103:Triton images
6101:
6098:
6095:
6093:
6089:
6085:
6082:
6080:
6076:
6073:
6071:
6067:
6064:
6059:
6056:
6053:
6052:
6032:
6024:
6016:
6009:
6002:
5983:
5976:
5969:
5954:
5953:
5948:
5941:
5925:
5918:
5903:
5902:
5897:
5890:
5871:
5864:
5858:
5849:
5845:
5841:
5837:
5833:
5829:
5825:
5821:
5817:
5813:
5806:
5798:
5794:
5790:
5786:
5782:
5778:
5771:
5763:
5759:
5755:
5751:
5748:(1): 221–34.
5747:
5743:
5736:
5728:
5724:
5720:
5716:
5712:
5708:
5704:
5700:
5696:
5692:
5685:
5677:
5673:
5669:
5665:
5661:
5657:
5653:
5649:
5645:
5641:
5640:
5632:
5630:
5628:
5626:
5624:
5615:
5611:
5607:
5603:
5599:
5595:
5594:
5586:
5578:
5574:
5570:
5566:
5559:
5557:
5555:
5538:
5534:
5527:
5520:
5505:
5501:
5497:
5493:
5489:
5485:
5481:
5477:
5476:
5468:
5461:
5459:
5450:
5446:
5442:
5438:
5431:
5429:
5420:
5416:
5412:
5411:10.1038/31651
5408:
5404:
5400:
5396:
5392:
5384:
5368:
5364:
5360:
5353:
5345:
5341:
5337:
5333:
5329:
5325:
5320:
5315:
5311:
5307:
5303:
5295:
5293:
5291:
5284:
5280:
5276:
5275:
5269:
5261:
5257:
5253:
5249:
5245:
5241:
5237:
5233:
5229:
5222:
5214:
5210:
5206:
5202:
5198:
5194:
5190:
5186:
5182:
5178:
5177:
5169:
5165:
5158:
5147:
5140:
5131:
5126:
5122:
5118:
5114:
5110:
5106:
5099:
5091:
5087:
5083:
5079:
5075:
5071:
5067:
5063:
5056:
5045:
5044:
5036:
5025:September 26,
5021:
5017:
5010:
5002:
4998:
4994:
4990:
4987:(1): 135–49.
4986:
4982:
4975:
4973:
4964:
4960:
4955:
4950:
4945:
4940:
4936:
4932:
4928:
4921:
4919:
4910:
4906:
4902:
4895:
4887:
4883:
4879:
4875:
4870:
4869:10.1038/16615
4865:
4861:
4857:
4853:
4849:
4848:
4843:
4836:
4828:
4824:
4820:
4816:
4809:
4793:
4789:
4785:
4779:
4763:
4759:
4755:
4748:
4746:
4730:
4726:
4722:
4718:
4714:
4710:
4709:
4704:
4697:
4689:
4685:
4681:
4677:
4673:
4669:
4665:
4661:
4657:
4653:
4649:
4642:
4640:
4631:
4627:
4623:
4619:
4615:
4611:
4607:
4603:
4599:
4595:
4588:
4580:
4576:
4572:
4568:
4564:
4560:
4556:
4552:
4548:
4544:
4537:
4535:
4526:
4520:
4516:
4512:
4506:
4498:
4494:
4490:
4486:
4482:
4478:
4474:
4470:
4466:
4462:
4458:
4451:
4449:
4440:
4436:
4432:
4428:
4424:
4420:
4416:
4412:
4405:
4394:September 18,
4390:
4386:
4379:
4371:
4367:
4363:
4359:
4355:
4351:
4348:(2): 143–60.
4347:
4343:
4336:
4328:
4324:
4320:
4316:
4312:
4308:
4304:
4300:
4293:
4286:
4284:
4275:
4271:
4264:
4262:
4260:
4251:
4247:
4243:
4239:
4235:
4231:
4230:
4225:
4218:
4207:
4203:
4199:
4195:
4191:
4187:
4183:
4179:
4175:
4174:
4166:
4159:
4151:
4147:
4143:
4139:
4135:
4131:
4127:
4123:
4119:
4115:
4108:
4092:
4088:
4082:
4074:
4068:
4060:
4054:
4038:
4034:
4030:
4023:
4004:
4000:
3996:
3992:
3988:
3984:
3980:
3973:
3966:
3950:
3946:
3942:
3936:
3934:
3925:
3921:
3917:
3913:
3909:
3905:
3904:New Scientist
3901:
3895:
3887:
3883:
3878:
3873:
3868:
3863:
3859:
3855:
3850:
3845:
3841:
3837:
3833:
3829:
3822:
3806:
3802:
3798:
3791:
3783:
3779:
3775:
3771:
3767:
3763:
3759:
3755:
3750:
3745:
3741:
3737:
3726:
3717:
3712:
3708:
3704:
3700:
3696:
3692:
3685:
3669:
3665:
3659:
3657:
3648:
3644:
3640:
3634:
3630:
3626:
3622:
3618:
3614:
3610:
3606:
3599:
3597:
3588:
3584:
3580:
3576:
3575:
3570:
3564:
3562:
3555:
3551:
3547:
3542:
3534:
3530:
3526:
3522:
3518:
3511:
3504:
3488:
3484:
3480:
3474:
3466:
3462:
3458:
3452:
3448:
3444:
3443:
3438:
3432:
3416:
3412:
3411:
3406:
3400:
3385:
3381:
3375:
3373:
3364:
3360:
3356:
3352:
3348:
3344:
3340:
3336:
3329:
3327:
3317:
3312:
3308:
3304:
3300:
3296:
3292:
3283:
3278:
3274:
3270:
3266:
3262:
3258:
3249:
3244:
3240:
3236:
3232:
3228:
3224:
3220:
3214:
3205:
3200:
3196:
3192:
3188:
3184:
3183:
3178:
3171:
3169:
3152:
3148:
3142:
3140:
3124:
3120:
3114:
3095:
3091:
3087:
3083:
3079:
3075:
3071:
3067:
3063:
3059:
3055:
3048:
3041:
3039:
3037:
3035:
3019:
3015:
3008:
3000:
2996:
2992:
2988:
2984:
2980:
2975:
2970:
2966:
2962:
2955:
2953:
2951:
2942:
2938:
2934:
2930:
2925:
2920:
2916:
2912:
2908:
2901:
2899:
2890:
2886:
2882:
2878:
2874:
2870:
2863:
2856:
2840:
2836:
2829:
2818:September 28,
2813:
2809:
2803:
2795:
2789:
2785:
2781:
2774:
2772:
2770:
2768:
2766:
2764:
2762:
2760:
2758:
2756:
2754:
2752:
2750:
2748:
2746:
2744:
2742:
2740:
2738:
2736:
2734:
2732:
2715:
2711:
2707:
2701:
2699:
2697:
2695:
2693:
2683:
2678:
2674:
2670:
2666:
2662:
2661:
2656:
2649:
2647:
2645:
2643:
2641:
2639:
2622:
2618:
2614:
2610:
2603:
2601:
2599:
2597:
2595:
2579:
2578:
2573:
2569:
2563:
2561:
2544:
2540:
2533:
2531:
2529:
2522:
2516:
2512:
2499:
2483:
2475:
2467:
2459:
2451:
2443:
2435:
2427:
2419:
2411:
2403:
2395:
2389:
2372:
2366:(140 km)
2365:
2361:
2357:
2353:
2347:
2338:
2329:
2308:
2304:
2300:
2297:
2294:
2284:
2280:
2277:
2273:
2267:
2244:
2240:
2235:
2232:
2221:
2217:
2214:
2210:
2204:
2183:
2179:
2175:
2170:
2167:
2157:
2153:
2147:
2126:
2122:
2118:
2115:
2107:
2101:
2092:
2088:
2076:
2073:
2071:
2068:
2065:
2064:
2063:Triton Hopper
2060:
2058:
2055:
2053:
2050:
2048:
2045:
2044:
2039:
2028:
2025:
2014:
2011:
2000:
1984:
1977:
1970:
1962:
1955:
1948:
1941:
1933:
1932:
1924:
1922:
1918:
1914:
1910:
1906:
1902:
1901:
1896:
1892:
1891:
1890:Triton Hopper
1885:
1881:
1879:
1874:
1870:
1866:
1864:
1859:
1854:
1852:
1847:
1846:Gerard Kuiper
1842:
1840:
1836:
1832:
1828:
1823:
1821:
1820:
1811:
1806:
1798:
1789:
1786:
1780:
1778:
1774:
1770:
1766:
1762:
1758:
1750:
1745:
1736:
1734:
1733:cryovolcanism
1730:
1726:
1721:30–40 km
1717:
1715:
1707:
1703:
1702:
1696:
1687:
1685:
1681:
1677:
1673:
1671:
1666:
1662:
1657:
1655:
1654:
1647:
1645:
1639:
1637:
1627:
1614:
1610:
1606:
1602:
1595:
1590:
1586:
1579:
1574:
1570:
1566:
1562:
1561:Kraken Catena
1558:
1551:
1546:
1545:
1544:
1542:
1537:
1533:
1531:
1527:
1524:
1514:
1510:
1506:
1502:
1497:
1495:
1491:
1488:
1484:
1480:
1475:
1471:
1467:
1466:
1459:
1449:
1447:
1443:
1439:
1435:
1431:
1427:
1421:
1414:Cryovolcanism
1411:
1409:
1405:
1398:
1394:
1390:
1386:
1379:map of Triton
1378:
1373:
1368:
1358:
1356:
1352:
1348:
1344:
1339:
1338:
1333:
1329:
1324:
1322:
1318:
1314:
1313:magnetosphere
1302:
1298:
1294:
1286:
1281:
1277:
1275:
1271:
1267:
1263:
1254:
1249:
1245:
1235:
1233:
1229:
1225:
1222:
1218:
1214:
1210:
1206:
1202:
1198:
1194:
1190:
1186:
1181:
1179:
1175:
1171:
1167:
1163:
1159:
1155:
1151:
1147:
1143:
1139:
1135:
1131:
1127:
1124:
1119:
1117:
1113:
1109:
1106:
1105:dwarf planets
1102:
1091:
1088:) and Earth (
1087:
1083:
1076:
1062:
1048:
1044:
1042:
1036:
1033:
1032:tidal heating
1028:
1026:
1025:gravitational
1022:
1018:
1017:giant planets
1014:
1010:
1005:
1001:
997:
995:
991:
987:
983:
979:
975:
971:
963:
958:
949:
947:
943:
939:
935:
931:
927:
923:
919:
918:circularizing
915:
911:
906:
904:
903:orbital plane
899:
894:
891:
886:
884:
880:
876:
872:
868:
864:
856:
852:
848:
843:
834:
832:
828:
827:John Herschel
824:
820:
816:
812:
808:
804:
800:
795:
793:
789:
785:
780:
779:John Herschel
776:
772:
763:
754:
752:
748:
744:
743:New Frontiers
740:
739:
734:
730:
726:
723:
722:
717:
713:
709:
704:
702:
698:
694:
690:
686:
682:
678:
673:
671:
670:tidal heating
663:
659:
655:
651:
647:
643:
635:
631:
630:dwarf planets
627:
623:
618:
616:
612:
608:
604:
600:
596:
592:
588:
584:
581:
577:
573:
564:
560:
556:
553:
551:
547:
527:
524:
518:
513:
509:
506:
505:
498:
494:
491:
486:
482:
480:
476:
472:
470:
466:
462:
459:
454:
450:
447:
442:
439:
436:
433:
428:
422:
419:
414:
409:
408:
400:
395:
392:
387:
381:
378:
372:
352:
350:
346:
340:
338:
334:
328:
325:
320:
310:(0.2122
302:
299:
294:
289:
286:
283:
281:
277:
269:
265:
263:
259:
255:
252:
251:orbital speed
246:
242:
234:
231:
226:
220:
218:
214:
208:
205:
200:
197:
193:
187:
148:
146:
142:
139:
136:
133:
127:
122:
96:
94:Pronunciation
92:
88:
82:
77:
73:
69:
66:
63:
61:
57:
52:
47:
43:
37:
32:
26:
22:
9321:Solar System
8260:
8246:
8232:
8213:
8199:
8180:
8156:
8142:
8123:
8085:
8020:Trojan moons
8010:Subsatellite
7858:
7824:
7549:Petit-Prince
7444:Minor-planet
7393:Dwarf planet
7318:Solar System
7216:
7204:
7198:Not selected
7186:
7179:
7162:
7147:(1989 flyby)
7141:
7029:385695 Clete
6898:
6897:
6620:
6619:
6496:In mythology
6468:
6461:
6443:
6436:
6399:
6145:
6091:
6078:
6062:
6035:. Retrieved
6023:
6014:
6001:
5989:. Retrieved
5982:the original
5968:
5956:. Retrieved
5950:
5940:
5930:February 11,
5928:. Retrieved
5917:
5905:. Retrieved
5899:
5889:
5877:. Retrieved
5870:the original
5857:
5815:
5811:
5805:
5780:
5776:
5770:
5745:
5741:
5735:
5694:
5690:
5684:
5643:
5637:
5597:
5591:
5585:
5568:
5564:
5541:. Retrieved
5536:
5532:
5519:
5507:. Retrieved
5479:
5473:
5440:
5436:
5394:
5390:
5383:
5371:. Retrieved
5352:
5309:
5305:
5273:
5268:
5235:
5231:
5221:
5180:
5174:
5157:
5139:
5115:(17): 3476.
5112:
5108:
5098:
5065:
5061:
5055:
5042:
5035:
5023:. Retrieved
5019:
5009:
4984:
4980:
4934:
4930:
4900:
4894:
4851:
4845:
4835:
4818:
4814:
4808:
4798:December 31,
4796:. Retrieved
4778:
4768:December 31,
4766:. Retrieved
4757:
4732:. Retrieved
4712:
4706:
4696:
4655:
4651:
4597:
4593:
4587:
4546:
4542:
4514:
4505:
4464:
4460:
4414:
4410:
4404:
4392:. Retrieved
4388:
4378:
4345:
4342:Astrobiology
4341:
4335:
4302:
4298:
4273:
4233:
4227:
4217:
4206:the original
4177:
4171:
4158:
4117:
4113:
4107:
4095:. Retrieved
4091:the original
4081:
4067:
4053:
4041:. Retrieved
4037:the original
4032:
4022:
4010:. Retrieved
4003:the original
3982:
3978:
3965:
3953:. Retrieved
3907:
3903:
3894:
3839:
3835:
3821:
3809:. Retrieved
3800:
3790:
3739:
3735:
3725:
3698:
3694:
3684:
3672:. Retrieved
3667:
3612:
3608:
3578:
3572:
3569:Chyba, C. F.
3541:
3516:
3503:
3491:. Retrieved
3487:the original
3482:
3473:
3441:
3431:
3419:. Retrieved
3409:
3399:
3389:November 28,
3387:. Retrieved
3383:
3341:(42): 1–17.
3338:
3334:
3298:
3294:
3264:
3260:
3230:
3226:
3213:
3186:
3180:
3155:. Retrieved
3150:
3126:. Retrieved
3122:
3113:
3101:. Retrieved
3094:the original
3057:
3053:
3021:. Retrieved
3017:
3007:
2964:
2960:
2914:
2910:
2872:
2868:
2855:
2843:. Retrieved
2839:the original
2828:
2816:. Retrieved
2812:the original
2802:
2783:
2718:. Retrieved
2664:
2658:
2625:. Retrieved
2621:the original
2612:
2581:. Retrieved
2575:
2547:. Retrieved
2543:the original
2520:
2515:
2388:
2371:
2346:
2337:
2328:
2282:
2278:
2271:
2266:
2219:
2215:
2208:
2203:
2155:
2151:
2146:
2105:
2100:
2091:
2070:Triton's sky
2061:
1920:
1916:
1898:
1888:
1877:
1867:
1862:
1855:
1850:
1843:
1830:
1824:
1817:
1814:
1809:
1784:
1781:
1773:surface area
1760:
1754:
1749:cryovolcanic
1724:
1718:
1711:
1699:
1668:
1658:
1651:
1648:
1640:
1635:
1632:
1540:
1538:
1534:
1512:
1498:
1490:water sprite
1463:
1461:
1426:cryovolcanic
1423:
1388:
1384:
1382:
1354:
1351:Solar System
1335:
1325:
1317:hydrocarbons
1301:thermosphere
1297:stratosphere
1290:
1284:
1259:
1182:
1120:
1098:
1089:
1085:
1081:
1045:
1037:
1029:
1006:
1002:
998:
970:solar nebula
967:
914:Viscoelastic
910:eccentricity
907:
895:
887:
860:
814:
796:
768:
750:
746:
737:
719:
705:
685:cryovolcanic
674:
619:
603:dwarf planet
599:Solar System
589:and hosts a
571:
570:
503:
406:
404:0.0794
324:Surface area
217:Eccentricity
137:
79:Designations
41:
25:
21:Titan (moon)
9309:Outer space
9297:Spaceflight
7985:Inner moons
7691:Skamandrios
7127:Exploration
7001:Kuiper belt
6413:Planned and
6381:Exploration
6363:Kuiper belt
6267:Slidr Sulci
6226:Kibu Patera
6198:Monad Regio
6086:(including
6084:Triton page
6075:Triton page
6037:January 11,
5879:October 10,
5543:January 25,
4937:: 836–842.
4511:Miller, Ron
4043:February 4,
3955:December 9,
3828:Robin Canup
3493:January 13,
3157:January 25,
3128:January 16,
3023:October 21,
2720:October 26,
2627:October 26,
2583:November 5,
2549:January 18,
2354:: Saturn's
1858:occultation
1825:Before the
1609:Kraken Mare
1501:translucent
1420:Cryovolcano
1347:Bond albedo
1293:troposphere
1180:radiation.
1178:ultraviolet
1158:lithosphere
1092:), to scale
974:Kuiper belt
962:Kuiper belt
938:Roche limit
851:tilted −23°
714:. The 1989
632:. The mean
607:Kuiper belt
479:Temperature
438:synchronous
397:0.779
308:0.9 km
298:Mean radius
262:Inclination
149:Tritonian (
130:Named after
85:Designation
9331:Categories
8690:Other KBOs
8308:Interamnia
8169:Atmosphere
8136:Atmosphere
8103:Mesoplanet
7749:Sila–Nunam
7615:Cleoselene
7610:Alexhelios
7588:Gorgoneion
7526:Euphrosyne
7453:Near-Earth
7395:satellites
7328:satellites
6940:S/2021 N 1
6920:S/2002 N 5
6701:S/2021 N 1
6679:Retrograde
6665:S/2002 N 5
6627:atmosphere
6491:In fiction
6304:Polar caps
6262:Set Catena
6157:Atmosphere
6097:Triton map
5571:: 165–66.
5509:October 9,
5373:August 29,
5319:2112.04627
5312:: 114835.
4944:1904.08073
4758:Hubblesite
4734:October 8,
4097:January 7,
3849:1711.01581
3842:(5): 208.
3233:(9): 157.
3103:August 28,
2924:2402.02476
2508:References
1714:cantaloupe
1676:Yasu Sulci
1599:Two large
1565:Set Catena
1479:Hili plume
1238:Atmosphere
1144:and 0.05%
1086:upper left
1082:lower left
784:have rings
725:spacecraft
515:Atmosphere
458:Axial tilt
362:10 kg
241:retrograde
145:Adjectives
9273:Astronomy
8837:Dziewanna
8504:Cubewanos
8287:Candidate
8117:Consensus
7914:Enceladus
7788:Gǃòʼé ǃHú
7699:Eurybates
7677:Menoetius
7671:Patroclus
7660:Dinkinesh
7605:Kleopatra
7508:Main belt
7468:Dimorphos
7326:Planetary
7244:Mythology
7156:Proposals
7143:Voyager 2
6957:Discovery
6949:Astronomy
6925:Laomedeia
6888:Hippocamp
6816:Geography
6670:Laomedeia
6605:Irregular
6590:Hippocamp
6455:Cancelled
6401:Voyager 2
6339:Discovery
6331:Astronomy
6176:Geography
5991:April 18,
5958:March 20,
5907:March 20,
5344:0019-1035
5090:125508759
5068:: 19–25.
4963:118682572
4886:204990689
4389:Space.com
3782:119486610
3774:0004-6256
3647:189794324
3421:April 10,
3363:116314854
2974:1003.2866
2496:10. (See
2466:Enceladus
2176:π
2119:π
1863:Voyager 2
1851:Voyager 2
1831:Voyager 2
1819:Voyager 2
1810:Voyager 2
1785:Voyager 2
1761:Voyager 2
1729:diapirism
1701:Voyager 2
1636:Voyager 2
1541:Voyager 2
1513:Voyager 2
1509:sublimate
1474:entrained
1465:Voyager 2
1401:frozen CO
1389:Voyager 2
1385:Voyager 2
1355:Voyager 2
1337:Voyager 2
1285:Voyager 2
1232:habitable
1221:obliquity
1162:water ice
1154:dihydrate
1021:disrupted
890:obliquity
733:Discovery
721:Voyager 2
642:water ice
605:from the
256:4.39 km/s
89:Neptune I
54:Discovery
42:Voyager 2
9246:Category
9209:Sednoids
8481:Twotinos
8376:Plutinos
8326:Chariklo
8318:Centaurs
8248:Gonggong
8201:Makemake
7959:Hyperion
7909:Dysnomia
7839:Callisto
7819:Ganymede
7642:Olympias
7512:Kalliope
7482:Squannit
7457:Florence
7429:Gonggong
7424:Makemake
7262:Category
6930:Psamathe
6910:Halimede
6868:Thalassa
6744:Category
6714:See also
6691:Psamathe
6686:Halimede
6648:Prograde
6570:Thalassa
6415:proposed
6180:features
5840:17755996
5727:24279680
5719:17793022
5676:38689872
5668:17793023
5419:40865426
5367:Archived
5279:Archived
5260:54843498
5205:17793016
4792:Archived
4762:Archived
4688:45403579
4680:17755997
4630:25093997
4622:17757214
4579:19761107
4571:17757213
4497:21809358
4489:17756000
4370:12467118
4327:40342189
4305:: 2–10.
4202:59040182
4150:20022185
4142:17793020
4012:June 25,
3949:Archived
3886:31019331
3811:June 24,
3805:Archived
3674:June 27,
3550:Archived
3465:33103787
3415:Archived
3407:(1880).
3189:(1): 8.
3082:16688170
2999:58889896
2780:"Triton"
2714:Archived
2350:Largest
1996:See also
1921:Nautilus
1767:'s moon
1684:Lo Sulci
1680:Ho Sulci
1674:such as
1601:cryolava
1587:geysers.
1585:nitrogen
1438:Ganymede
1321:nitriles
1309:5 K
1262:nitrogen
1205:volatile
1123:annealed
1080:Triton (
990:plutinos
926:prograde
922:gas drag
823:Hyperion
803:Poseidon
788:aperture
751:Nautilus
689:tectonic
666:0.000016
611:captured
555:nitrogen
523:pressure
521:Surface
268:ecliptic
249:Average
222:0.000016
9259:Portals
9218:2012 VP
9195:2008 ST
9185:2007 JJ
9175:2005 TB
9165:2004 XR
9155:2003 QX
9145:2003 FY
9120:2021 LL
9108:2021 DR
9096:2018 VG
9084:2018 AG
9072:2017 FO
9060:2015 RR
9048:2015 KH
9038:2014 WK
9026:2014 UZ
9016:2014 EZ
9006:2014 AN
8996:2013 FY
8986:2010 VZ
8979:2010 TJ
8967:2010 JO
8957:2010 RF
8947:2010 RE
8935:2010 KZ
8925:2008 OG
8913:2006 QH
8903:2005 RM
8893:2005 QU
8883:2004 XA
8873:2002 TC
8863:2001 UR
8853:1996 TL
8843:1996 GQ
8810:2015 RR
8800:2015 AM
8790:2014 UM
8780:2013 FZ
8770:2011 GM
8758:2011 FW
8748:2010 VK
8738:2010 JO
8728:2002 XW
8718:2000 YW
8708:1999 DE
8698:1999 CD
8675:2010 FX
8665:2005 UQ
8655:2005 RN
8645:2004 UX
8635:2004 TY
8625:2004 PF
8615:2004 NT
8605:2004 GV
8595:2003 QW
8585:2002 UX
8575:2002 MS
8565:2002 KX
8553:2002 CY
8543:2002 AW
8533:1998 SN
8517:Salacia
8490:2002 WC
8465:2017 OF
8455:2007 JH
8445:2003 VS
8435:2003 UZ
8425:2003 AZ
8415:2002 XV
8405:2002 VR
8395:2001 QF
8362:2014 NW
8352:2013 TC
8342:1999 OX
8164:Geology
8131:Geology
8108:Planemo
7949:Hiʻiaka
7929:Proteus
7919:Miranda
7889:Umbriel
7879:Iapetus
7864:Titania
7825:largest
7812:by size
7797:2013 FY
7754:Salacia
7740:2002 UX
7662:(Selam)
7650:Pulcova
7600:Elektra
7595:Camilla
7578:Minerva
7563:Romulus
7543:Eugenia
7536:Peneius
7498:2001 SN
7491:1994 CC
7462:Didymos
7362:Neptune
7347:Jupiter
7316:of the
7239:Fiction
7232:Related
7188:Trident
7164:Shensuo
7107:2011 HM
7095:2008 LC
7083:2007 VL
7071:2006 RJ
7059:2005 TN
7047:2004 KV
7035:2001 QR
7016:Trojans
6994:General
6893:Proteus
6883:Larissa
6878:Galatea
6873:Despina
6796:Neptune
6637:geology
6632:climate
6595:Proteus
6585:Larissa
6580:Galatea
6575:Despina
6558:(inner)
6556:Regular
6548:Neptune
6484:Related
6438:Trident
6356:General
6276:Craters
6189:Regions
6167:Geology
6162:Climate
6070:YouTube
5848:9367553
5820:Bibcode
5812:Science
5785:Bibcode
5750:Bibcode
5699:Bibcode
5691:Science
5648:Bibcode
5639:Science
5602:Bibcode
5593:Geology
5573:Bibcode
5504:8623816
5484:Bibcode
5445:Bibcode
5399:Bibcode
5324:Bibcode
5300:2022).
5240:Bibcode
5213:1948948
5185:Bibcode
5176:Science
5117:Bibcode
5070:Bibcode
4989:Bibcode
4903:: 108.
4878:9930696
4856:Bibcode
4823:Bibcode
4717:Bibcode
4660:Bibcode
4652:Science
4602:Bibcode
4594:Science
4551:Bibcode
4543:Science
4469:Bibcode
4461:Science
4439:4250378
4419:Bibcode
4350:Bibcode
4307:Bibcode
4238:Bibcode
4182:Bibcode
4122:Bibcode
4114:Science
3987:Bibcode
3912:Bibcode
3877:6476549
3854:Bibcode
3754:Bibcode
3703:Bibcode
3617:Bibcode
3583:Bibcode
3548:(2010)
3521:Bibcode
3343:Bibcode
3303:Bibcode
3269:Bibcode
3235:Bibcode
3191:Bibcode
3090:4420518
3062:Bibcode
2979:Bibcode
2929:Bibcode
2877:Bibcode
2845:July 1,
2669:Bibcode
2474:Miranda
2442:Umbriel
2418:Iapetus
2394:Titania
2364:Himalia
2360:Sycorax
2150:Volume
2075:Shensuo
1900:Trident
1878:Huygens
1777:Mazomba
1769:Miranda
1653:maculae
1408:tholins
1174:tholins
1156:in the
1150:ammonia
1142:methane
1138:dry ice
952:Capture
924:from a
871:Jupiter
807:Neptune
777:. When
745:-class
738:Trident
735:-class
693:methane
634:density
615:gravity
583:Neptune
578:of the
559:methane
377:density
358:0.0028)
354:(2.1389
304:1,353.4
285:Neptune
8527:Varuna
8336:Pholus
8331:Chiron
8303:Hygiea
8215:Quaoar
8182:Haumea
8096:Pallas
8086:Triton
8081:Phoebe
8005:Naming
7964:Phoebe
7954:Actaea
7944:Nereid
7939:Ilmarë
7904:Tethys
7884:Charon
7874:Oberon
7859:Triton
7854:Europa
7810:Ranked
7774:Ilmarë
7760:Actaea
7685:Hektor
7636:Roxane
7628:Dactyl
7557:Sylvia
7531:Daphne
7476:Moshup
7419:Quaoar
7414:Haumea
7357:Uranus
7352:Saturn
7272:Portal
7175:ODINUS
6905:Nereid
6899:Triton
6754:Portal
6655:Nereid
6621:Triton
6613:Triton
6309:Plumes
6283:Amarum
6250:Faults
6146:Triton
6065:(1989)
5846:
5838:
5777:Icarus
5742:Icarus
5725:
5717:
5674:
5666:
5502:
5417:
5391:Nature
5342:
5306:Icarus
5258:
5211:
5203:
5088:
4981:Icarus
4961:
4884:
4876:
4847:Nature
4686:
4678:
4628:
4620:
4577:
4569:
4521:
4495:
4487:
4437:
4411:Nature
4368:
4325:
4299:Icarus
4229:Icarus
4200:
4148:
4140:
3979:Icarus
3884:
3874:
3780:
3772:
3645:
3635:
3463:
3453:
3361:
3088:
3080:
3054:Nature
2997:
2967:: L8.
2869:Icarus
2790:
2458:Tethys
2426:Charon
2402:Oberon
2356:Phoebe
2274:, the
2211:, the
1765:Uranus
1706:Europa
1682:, and
1494:Tongan
1492:and a
1470:geyser
1452:Plumes
1444:, and
1442:Charon
1343:albedo
1217:Europa
1195:and a
1193:mantle
1170:albedo
1013:Nereid
982:comets
946:Saturn
883:Phoebe
879:Uranus
875:Saturn
831:Saturn
819:Nereid
799:Triton
580:planet
572:Triton
565:traces
469:Albedo
337:Volume
138:Trītōn
135:Τρίτων
29:Triton
9285:Stars
8522:Varda
8512:Chaos
8389:Ixion
8262:Sedna
8226:Rings
8188:Moons
8174:Moons
8158:Pluto
8144:Orcus
8125:Ceres
8091:Vesta
7934:Mimas
7924:Vanth
7899:Dione
7894:Ariel
7834:Titan
7768:Varda
7724:Hiisi
7718:Lempo
7705:Queta
7655:Balam
7583:Aegis
7570:Remus
7518:Linus
7446:moons
7409:Pluto
7404:Orcus
7337:Earth
6863:Naiad
6855:Moons
6833:Rings
6565:Naiad
6431:IHP-2
6292:Other
6090:) at
6033:. AGU
6011:(PDF)
5985:(PDF)
5978:(PDF)
5873:(PDF)
5866:(PDF)
5844:S2CID
5723:S2CID
5672:S2CID
5529:(PDF)
5500:S2CID
5470:(PDF)
5415:S2CID
5314:arXiv
5256:S2CID
5209:S2CID
5171:(PDF)
5149:(PDF)
5086:S2CID
5047:(PDF)
4959:S2CID
4939:arXiv
4882:S2CID
4684:S2CID
4626:S2CID
4575:S2CID
4493:S2CID
4435:S2CID
4323:S2CID
4295:(PDF)
4209:(PDF)
4198:S2CID
4168:(PDF)
4146:S2CID
4006:(PDF)
3975:(PDF)
3844:arXiv
3778:S2CID
3744:arXiv
3643:S2CID
3513:(PDF)
3359:S2CID
3097:(PDF)
3086:S2CID
3050:(PDF)
2995:S2CID
2969:arXiv
2919:arXiv
2917:: 8.
2865:(PDF)
2484:—0.04
2482:Mimas
2476:—0.06
2468:—0.11
2450:Dione
2434:Ariel
2083:Notes
1884:Titan
1880:probe
1827:flyby
1670:sulci
1613:Titan
1516:'
1446:Titan
1434:Ariel
1328:Earth
1266:Pluto
1224:tides
1201:Water
1197:crust
1185:Earth
1166:Earth
1130:Water
1116:Pluto
1108:Pluto
1090:right
986:Pluto
729:probe
716:flyby
650:crust
495:13.47
375:Mean
8384:Huya
8254:Moon
8240:Moon
8234:Eris
8221:Moon
8207:Moon
8193:Ring
8150:Moon
7995:List
7869:Rhea
7849:Moon
7731:Paha
7714:TNOs
7434:Eris
7342:Mars
7206:Argo
7135:Past
6935:Neso
6696:Neso
6463:Argo
6388:Past
6039:2024
6015:NASA
5993:2021
5960:2019
5932:2017
5909:2019
5881:2013
5836:PMID
5715:PMID
5664:PMID
5545:2008
5511:2011
5375:2009
5340:ISSN
5201:PMID
5027:2017
4874:PMID
4800:2007
4770:2007
4736:2011
4676:PMID
4618:PMID
4567:PMID
4519:ISBN
4485:PMID
4396:2015
4366:PMID
4138:PMID
4099:2024
4045:2008
4014:2019
3957:2007
3945:NASA
3882:PMID
3813:2007
3770:ISSN
3732:G298
3676:2024
3633:ISBN
3495:2008
3461:OCLC
3451:ISBN
3423:2007
3391:2019
3159:2024
3130:2023
3105:2015
3078:PMID
3025:2014
2847:2008
2820:2007
2788:ISBN
2722:2011
2629:2011
2585:2014
2551:2008
2480:10,
2472:10,
2464:10,
2460:—0.6
2456:10,
2452:—1.1
2448:10,
2444:—1.3
2440:10,
2436:—1.2
2432:10,
2428:—1.6
2424:10,
2420:—1.8
2416:10,
2412:—2.3
2410:Rhea
2408:10,
2404:—3.1
2400:10,
2396:—3.5
1927:Maps
1882:for
1873:NASA
1725:cavi
1650:the
1563:and
1487:Zulu
1481:and
1462:The
1319:and
1274:mbar
1246:and
1191:, a
1189:core
1112:Eris
1110:and
960:The
942:ring
934:Moon
873:and
855:moon
849:and
749:and
741:and
701:haze
695:and
687:and
658:core
646:mass
626:Moon
561:and
510:−1.2
473:0.76
349:Mass
9221:113
9197:291
9177:190
9167:190
9157:113
9147:128
9075:161
9063:245
9051:162
9040:509
9029:224
8970:179
8916:181
8895:182
8885:192
8875:302
8865:163
8812:245
8802:281
8750:201
8740:179
8720:134
8700:158
8667:513
8637:364
8627:115
8556:248
8545:197
8535:165
8437:413
8407:128
8397:298
8354:146
7968:...
7622:Ida
7500:263
7110:102
7086:305
7074:103
7038:322
6915:Sao
6660:Sao
6077:at
6068:on
5828:doi
5816:246
5793:doi
5758:doi
5746:100
5707:doi
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