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Neptune is the farthest out of the major planets. Much like Uranus in appearance, it too is mostly hydrogen with some helium. High winds periodically produce storms that appear as dark spots. Voyager 2 found 5 new, small satellites. But, the real interest resulting from the Voyager passage is the very large (2400 km) satellite Triton, which seem an agglomerate of rock and frozen hydrogen and methane, with subordinate, perhaps trivial, amounts of water. Its southern polar cap has a melange of light and dark deposits of different compositions (and origins?). Pluto is farther out and appears to be a small planet. In 2004, discovery of Sedna, a planet or planet-like body much farther away brings the total of significant planetary objects to 10.`


Neptune has eight satellites, all but one irregular in shape and mostly rock. One, Triton, that is farthest out and much larger (2,700 km [1,678 mi] in diameter) than the others, is one of the most intriguing bodies - planets or satellites - in the Solar System. Triton moves in a retrograde circular orbit, i.e., it moves in a clockwise direction (looking down from north) compared to the counterclockwise rotation of Neptune and its other satellites. Triton's axis of rotation tilts 157° relative to its parent's axis. We cite these unusual conditions as evidence, either of its capture or of its assembly after a collision, possibly influenced by interactions with Pluto as that small body periodically orbits inside Neptune's orbit.

The full view (left) of Triton reveals it is very different from most of the giant planets' satellites. This satellite has a brownish pink color, has a polar cap (right), and a structured surface. The color may be due to frozen nitrogen and/or the effects of methane.

Full view image of Triton, taken from Voyager 2, showing its pinkish color.

The polar cap of nitrogen and methane sublimates in the southern hemisphere of Triton.


Triton's density (2.06 gm/cc) indicates it is a mix of rock (predominant) and frozen gases. But its surface shows not only rocky features but evidence of water ice (?), and (perhaps prevalent) frozen methane and nitrogen; both would be solid at a surface temperature of -235° C (35° K) which is the coldest surface yet found in the Solar System. Deposits of frozen nitrogen have built a polar ice cap, covering much of its southern hemisphere. Triton also has a very thin atmosphere (0.014 millibars) extending to 800 km (497 mi). The south polar ice cap appears mottled, with dark areas, perhaps showing rocks exposed along wind streaks where gases have sublimated:

19-71: Compare the atmospheric properties of Triton with those of Titan. ANSWER

The south polar ice cap appears mottled, with dark areas perhaps showing rocks exposed along wind streaks where gases have sublimed:

Voyager image of the south polar ice cap on Triton showing rocks exposed along wind streaks where gases have sublimed.

What has been interpreted as erupting nitrogen gas from structures or fissures made of frozen nitrogen and rock has been called "ice volcanoes" in which liquid nitrogen and/or methane vaporizes in plumes or geyser-like jets at the surface, carrying along particulates that form deposits on the ice cap. Ice "lavas" composed of water ice and some ammonia and methane produce flow features on the surface as well. Here is an area which contains this phenomenon - again the first of its kind in the Solar System. :

Color version of part of the south polar ice field, in which some so-called <i>ice volcanoes</i> (hard to see) made of nitrogen gas escaping and then freezing.

Triton's surface contains ridges, fault valleys, and occasional impact craters. This image shows a broad circular feature, with somewhat scalloped edges, that may be some strange volcanic caldera or a distorted impact crater (or one of each).

Voyager 2 view of the surface of Triton, showing a circular and an elliptical flat-bottomed depression and ridges and knobs.

This computer-generated perspective view helps to visualize this terrain:

Perspective view of the terrain on Triton.

Major fracture systems occur over much of Triton, especially in the equatorial regions. Some of the grabens are hundreds of kilometers long.

 Grabens cutting across the tritonian surface; Voyager 2

Terrains on Triton involving fracturing can take on a peculiar "texture" similar to the surface of a cantaloupe (top) or appearing as a series of oval features controlled by ridges (bottom):

Voyager image of the surface of Triton showing a series of oval features controlled by ridges.

Ovoid features on Triton's surface.

While filled grabens (fracture-bounded depressions) are a factor in canteloupe terrains, their specific origin remains unsettled. The oval features are even more mysterious.

19-72: Many of the individual roundish features making up the canteloupe texture look like distorted impact craters. What argues against this possible identity? ANSWER

Nereid, an irregular shaped satellite (maximum dimension = 340 km [220 miles] that is the outermost of the group, had been observed by telescope from Earth (discovered by Gerald Kuiper in 1941). Voyager 2 also got pictures but since Nereid was far away at the time, these are fuzzy:

Voyager 2 view of Nereid, the outermost larger neptunian satellite.

Largest (418 km; 261 miles) of the six satellites discovered by Voyager is the nearly round Proteus (below). Although bigger than Nereid, it remained undetected until Voyager because it was too close to the planet's surface and was masked by neptunian light.

Proteus, the innermost neptunian large satellite, discovered and imaged by Voyager 2.

The remaining smaller moons are Larissa, Galatea, Despina, Thalassa, and Naiad.

The last planet in our solar system, Pluto, is not much different in diameter (about 2,340 km [1,454 mi]) than Triton. No space probe has visited it yet, although NASA has proposed one (Pluto Express) for early in the 21st Century (but on hold, since Congress has not authorized funding). First discovered (though its existence had been predicted) in 1930, by Dr. Clyde Tombaugh, through the large telescope at the Lowell Observatory in Flagstaff, AZ, the best pictures (from HST) today show it is a mix of very dark (organic?) and light zones of unknown nature. Its density suggests mostly rock with some ices (nitrogen, methane, and water), from which an extremely tenuous atmosphere has evaporated.

 

Hubble Telescope images of Pluto.

Pluto's orbit is so eccentric that at times its path lies inside Neptune's. Its orbital period is 1.5 times that of Neptune, with which it locks in a 3:2 resonance. Pluto has a relatively large satellite, Charon, whose diameter (603 +/- 5 km [783 mi]) makes it just a fourth the size of its parent (one opinion considers the two to be a double planet system), with which it is in synchronous rotation. This diameter was determined from an occultation measurement during a 3 day exposure from the European Southern Observatory telescope, yielding this image:

Pluto and its moon Charon, seen here by their light reflection cumulating over 3 days.

There is a growing school of thought that holds Pluto to be a large asteroid that has escaped from the Kuiper belt beyond. However, its spherical shape supports the planet argument. More weight to that idea was the October 2005 announcement that, in addition to Charon, two more small moons have been detected by the Hubble Space Telescope:

Discovery of two more small moons that orbit about Pluto; evidence is the shift in positions on two different dates.

After 74 years, what is being hailed as the first new solar planet-like body (called a planetoid) since Pluto has been publicly announced in March, 2004. Astronomers from led by Michael E. Brown of Caltech and several universities using the 48-inch Palomar telescope found a large object within the solar system orbiting well beyond Pluto's orbit. Being very elliptical, this orbit extends out from about 8 billion miles 13 billion kilometers) at perisol to around 88 billion miles at apisol. The discovery image is this:

The arrows point to an object which moves definitively in a short time span; this is the new 'planet' Sedna.

This illustration shows an artist's conception of Sedna, with it and the asteroid Ouaoar, the Moon and Pluto shown in relative sizes to the Earth:

Sedna - a rendition based on limited observational data - with its size compared to other bodies.

These four panels give more information about Sedna, its orbit, and its relation to other named planets and fragmental bodies in the Solar System:

Sedna's location in the Solar System; read text below for explanation.

The upper left panel shows the inner Solar System out to beyond the Asteroid Belt (next page); the upper right shows Sedna in relation to the outer Solar System, including the Kuiper Belt of asteroids; the lower left shows the Solar System relative to the Oort Cloud (from which Sedna may have been ejected); the lower right depicts the highly elliptical orbit of Sedna.

This next image is purported to be one showing the Oort Cloud objects. The writer has greatly stretched the image to bring out the details:

The Oort Cloud.

Sedna has raised again questions about what constitutes a planet. Is it size, shape, orbit? One favored criterion is that a planet must be approximately spherical, which means it is big enough to have melted or otherwise reorganized its material into a shape with gravitational equilibrium favoring a globe. Sedna and Pluto meet this criterion but several Kuiper Belt Objects (KBO) approach that defining shape. A good summary of Sedna and similar objects is found at this CalTechsite.

The debate has been further complicated by the announcement of still another canditate as a possible 10th planet, so far designated only as 2003UB313, has been found among the KBOs. First examined in January 2005, its description was "leaked" on July 29, 2005. It is the circled object shown below:

2003UB313.

It is about 3 times further than Pluto from the Sun at apihelion (at 97 A.U.) but its highly elliptical orbit (perihelion at 36 A.U.), inclined about 45° from the ecliptic, removes it from the mainstream of solar planets. It takes about 560 years to fully orbit the Sun. Its size is still only approximated. Some observers think it smaller than Pluto but its discovers, the same group associated with Caltech that found Sedna, claim it is somewhat larger. It is definitely spherical, seems to have a solid surface, has methane in its atmosphere, and has its own tiny Moon. For the moment, its classification is "up in the air". Here is a time lapse trio of images that show the planet and its smaller moon:

Palomar telescope views of 2003UB313 and its moon.

Before turning to asteroids and comets, we summarize the information on the larger bodies in the Solar System with this diagram (Sedna and the newest "planet" not included):

Diagram showing the location and distance from the Sun of the planets, the Asteroid and Kuiper Belts, and the Oort Cloud; the planets are not to scale, either in size and in location, being shown at one size merely to indicate their relative positions.

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Primary Author: Nicholas M. Short, Sr. email: nmshort@ptd.net