solar system: Definition from Answers.com

This article is about the Sun and its planetary system. For other systems, see planetary system and star system. For a list of physical and orbital statistics for the Solar System's largest bodies, see List of gravitationally rounded objects of the Solar System.

Planets and dwarf planets of the Solar System. Sizes are to scale. Distances from the Sun are not to scale

Objects in the Solar System
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The Solar System^[a] consists of the Sun and the astronomical objects gravitationally bound in orbit around it, all of which formed from the collapse of a giant molecular cloud approximately 4.6 billion years ago. The vast majority of the system's mass is in the Sun. Of the many objects that orbit the Sun, most of the mass is contained within eight relatively solitary planets^[e] whose orbits are almost circular and lie within a nearly flat disc called the ecliptic plane. The four smaller inner planets, Mercury, Venus, Earth and Mars, also called the terrestrial planets, are primarily composed of rock and metal. The four outer planets, the gas giants, are substantially more massive than the terrestrials. The two largest, Jupiter and Saturn, are composed mainly of hydrogen and helium; the two outermost planets, Uranus and Neptune, are composed largely of ices, such as water, ammonia and methane, and are often referred to separately as "ice giants".

The Solar System is also home to a number of regions populated by smaller objects. The asteroid belt, which lies between Mars and Jupiter, is similar to the terrestrial planets as it is composed mainly of rock and metal. Beyond Neptune's orbit lie the Kuiper belt and scattered disc; linked populations of trans-Neptunian objects composed mostly of ices such as water, ammonia and methane. Within these populations, five individual objects, Ceres, Pluto, Haumea, Makemake and Eris, are recognized to be large enough to have been rounded by their own gravity, and are thus termed dwarf planets.^[e] In addition to thousands of small bodies^[e] in those two regions, several dozen of which are considered dwarf-planet candidates, various other small body populations including comets, centaurs and interplanetary dust freely travel between regions. Six of the planets and three of the dwarf planets are orbited by natural satellites,^[b] usually termed "moons" after Earth's Moon. Each of the outer planets is encircled by planetary rings of dust and other particles.

The solar wind, a flow of plasma from the Sun, creates a bubble in the interstellar medium known as the heliosphere, which extends out to the edge of the scattered disc. The Oort cloud, which is believed to be the source for long-period comets, may also exist at a distance roughly a thousand times further than the heliosphere. The heliopause is the point at which pressure from the solar wind is equal to the opposing pressure of interstellar wind. The Solar System is located within one of the outer arms of Milky Way galaxy, which contains about 200 billion stars.

Discovery and exploration

Main article: Discovery and exploration of the Solar System

For many thousands of years, humanity, with a few notable exceptions, did not recognize the existence of the Solar System. People believed the Earth to be stationary at the centre of the universe and categorically different from the divine or ethereal objects that moved through the sky. Although the Greek philosopher Aristarchus of Samos had speculated on a heliocentric reordering of the cosmos,^[1] Nicolaus Copernicus was the first to develop a mathematically predictive heliocentric system.^[2] His 17th-century successors, Galileo Galilei, Johannes Kepler and Isaac Newton, developed an understanding of physics that led to the gradual acceptance of the idea that the Earth moves around the Sun and that the planets are governed by the same physical laws that governed the Earth. Additionally, the invention of the telescope led to the discovery of further planets and moons. In more recent times, improvements in the telescope and the use of unmanned spacecraft have enabled the investigation of geological phenomena such as mountains and craters, and seasonal meteorological phenomena such as clouds, dust storms and ice caps on the other planets.

Structure

The orbits of the bodies in the Solar System to scale (clockwise from top left)

Solar System showing the plane of the Earth's orbit around the Sun in 3D. Mercury, Venus, Earth, and Mars are shown in both panels; the right panel also shows Jupiter making one full revolution with Saturn and Uranus making less than one full revolution.

The principal component of the Solar System is the Sun, a main-sequence G2 star that contains 99.86 percent of the system's known mass and dominates it gravitationally.^[3] The Sun's four largest orbiting bodies, the gas giants, account for 99 percent of the remaining mass, with Jupiter and Saturn together comprising more than 90 percent.^[c]

Most large objects in orbit around the Sun lie near the plane of Earth's orbit, known as the ecliptic. The planets are very close to the ecliptic while comets and Kuiper belt objects are frequently at significantly greater angles to it.^[4]^[5] All the planets and most other objects orbit the Sun in the same direction that the Sun is rotating (counter-clockwise, as viewed from above the Sun's north pole).^[6] There are exceptions, such as Halley's Comet.

The overall structure of the charted regions of the Solar System consists of the Sun, four relatively small inner planets surrounded by a belt of rocky asteroids, and four gas giants surrounded by the Kuiper belt of icy objects. Astronomers sometimes informally divide this structure into separate regions. The inner Solar System includes the four terrestrial planets and the asteroid belt. The outer Solar System is beyond the asteroids, including the four gas giants.^[7] Since the discovery of the Kuiper belt, the outermost parts of the Solar System are considered a distinct region consisting of the objects beyond Neptune.^[8]

Most of the planets in the Solar System possess secondary systems of their own, being orbited by planetary objects called natural satellites, or moons (two of which are larger than the planet Mercury), or, in the case of the four gas giants, by planetary rings; thin bands of tiny particles that orbit them in unison. Most of the largest natural satellites are in synchronous rotation, with one face permanently turned toward their parent.

Kepler's laws of planetary motion describe the orbits of objects about the Sun. Following Kepler's laws, each object travels along an ellipse with the Sun at one focus. Objects closer to the Sun (with smaller semi-major axes) travel more quickly, as they are more affected by the Sun's gravity. On an elliptical orbit, a body's distance from the Sun varies over the course of its year. A body's closest approach to the Sun is called its perihelion, while its most distant point from the Sun is called its aphelion. The orbits of the planets are nearly circular, but many comets, asteroids and Kuiper belt objects follow highly elliptical orbits. The positions of the bodies in the Solar System can be predicted using numerical models.

Due to the vast distances involved, many representations of the Solar System show orbits the same distance apart. In reality, with a few exceptions, the farther a planet or belt is from the Sun, the larger the distance between it and the previous orbit. For example, Venus is approximately 0.33 astronomical units (AU)^[d] farther out from the Sun than Mercury, while Saturn is 4.3 AU out from Jupiter, and Neptune lies 10.5 AU out from Uranus. Attempts have been made to determine a relationship between these orbital distances (for example, the Titius–Bode law),^[9] but no such theory has been accepted.

A number of Solar System models on Earth attempt to convey the relative scales involved in the Solar System on human terms. Some models are mechanical — called orreries — while others extend across cities or regional areas.^[10] The largest such scale model, the Sweden Solar System, uses the 110-metre Ericsson Globe in Stockholm as its substitute Sun, and, following the scale, Jupiter is a 7.5 metre sphere at Arlanda International Airport, 40 km away, while the farthest current object, Sedna, is a 10-cm sphere in Luleå, 912 km away.^[11]^[12]

Range of selected bodies of the Solar System from the middle of the Sun. The left and right edges of each bar correspond to the perihelion and aphelion of the body, respectively. Long bars denote high orbital eccentricity.

Composition

The Sun, which comprises nearly all the matter in the Solar System, is composed of roughly 98% hydrogen and helium.^[13] Jupiter and Saturn, which comprise nearly all the remaining matter, possess atmospheres composed of roughly 99% of those same elements.^[14]^[15] A composition gradient exists in the Solar System, created by heat and light pressure from the Sun; those objects closer to the Sun, which are more affected by heat and light pressure, are composed of elements with high melting points. Objects farther from the Sun are composed largely of materials with lower melting points.^[16] The boundary in the Solar System beyond which those volatile substances could condense is known as the frost line, and it lies at roughly 4 AU from the Sun.^[17]

The objects of the inner Solar System are composed mostly of rock,^[18] the collective name for compounds with high melting points, such as silicates, iron or nickel, that remained solid under almost all conditions in the protoplanetary nebula.^[19] Jupiter and Saturn are composed mainly of gases, the astronomical term for materials with extremely low melting points and high vapor pressure such as molecular hydrogen, helium, and neon, which were always in the gaseous phase in the nebula.^[19] Ices, like water, methane, ammonia, hydrogen sulfide and carbon dioxide,^[18] have melting points up to a few hundred kelvins, while their phase depends on the ambient pressure and temperature.^[19] They can be found as ices, liquids, or gases in various places in the Solar System, while in the nebula they were either in the solid or gaseous phase.^[19] Icy substances comprise the majority of the satellites of the giant planets, as well as most of Uranus and Neptune (the so-called "ice giants") and the numerous small objects that lie beyond Neptune's orbit.^[18]^[20] Together, gases and ices are referred to as volatiles.^[21]

Sun

Main article: Sun

A transit of Venus

The Sun is the Solar System's star, and by far its chief component. Its large mass (332,900 Earth masses)^[22] produces temperatures and densities in its core great enough to sustain nuclear fusion,^[23] which releases enormous amounts of energy, mostly radiated into space as electromagnetic radiation, peaking in the 400–700 nm band of visible light.^[24]

The Sun is classified as a type G2 yellow dwarf, but this name is misleading as, compared to the majority of stars in our galaxy, the Sun is rather large and bright.^[25] Stars are classified by the Hertzsprung–Russell diagram, a graph that plots the brightness of stars with their surface temperatures. Generally, hotter stars are brighter. Stars following this pattern are said to be on the main sequence, and the Sun lies right in the middle of it. However, stars brighter and hotter than the Sun are rare, while substantially dimmer and cooler stars, known as red dwarfs, are common, making up 85 percent of the stars in the galaxy.^[25]^[26]

Evidence suggests that the Sun's position on the main sequence puts it in the "prime of life" for a star, in that it has not yet exhausted its store of hydrogen for nuclear fusion. The Sun is growing brighter; early in its history it was 70 percent as bright as it is today.^[27]

The Sun is a population I star; it was born in the later stages of the universe's evolution, and thus contains more elements heavier than hydrogen and helium ("metals" in astronomical parlance) than older population II stars.^[28] Elements heavier than hydrogen and helium were formed in the cores of ancient and exploding stars, so the first generation of stars had to die before the universe could be enriched with these atoms. The oldest stars contain few metals, while stars born later have more. This high metallicity is thought to have been crucial to the Sun's developing a planetary system, because planets form from accretion of "metals".^[29]

The heliospheric current sheet

Interplanetary medium

Main articles: Interplanetary medium and Heliosphere

Along with light, the Sun radiates a continuous stream of charged particles (a plasma) known as the solar wind. This stream of particles spreads outwards at roughly 1.5 million kilometres per hour,^[30] creating a tenuous atmosphere (the heliosphere) that permeates the Solar System out to at least 100 AU (see heliopause).^[31] This is known as the interplanetary medium. Activity on the Sun's surface, such as solar flares and coronal mass ejections, disturb the heliosphere, creating space weather and causing geomagnetic storms.^[32] The largest structure within the heliosphere is the heliospheric current sheet, a spiral form created by the actions of the Sun's rotating magnetic field on the interplanetary medium.^[33]^[34]

Earth's magnetic field stops its atmosphere from being stripped away by the solar wind. Venus and Mars do not have magnetic fields, and as a result, the solar wind causes their atmospheres to gradually bleed away into space.^[35] Coronal mass ejections and similar events blow a magnetic field and huge quantities of material from the surface of the Sun. The interaction of this magnetic field and material with Earth's magnetic field funnels charged particles into the Earth's upper atmosphere, where its interactions create aurorae seen near the magnetic poles.

Cosmic rays originate outside the Solar System. The heliosphere partially shields the Solar System, and planetary magnetic fields (for those planets that have them) also provide some protection. The density of cosmic rays in the interstellar medium and the strength of the Sun's magnetic field change on very long timescales, so the level of cosmic radiation in the Solar System varies, though by how much is unknown.^[36]

The interplanetary medium is home to at least two disc-like regions of cosmic dust. The first, the zodiacal dust cloud, lies in the inner Solar System and causes zodiacal light. It was likely formed by collisions within the asteroid belt brought on by interactions with the planets.^[37] The second extends from about 10 AU to about 40 AU, and was probably created by similar collisions within the Kuiper belt.^[38]^[39]

Inner Solar System

The inner Solar System is the traditional name for the region comprising the terrestrial planets and asteroids.^[40] Composed mainly of silicates and metals, the objects of the inner Solar System are relatively close to the Sun; the radius of this entire region is shorter than the distance between Jupiter and Saturn.

Inner planets

Main article: Terrestrial planet

The inner planets. From left to right: Mercury, Venus, Earth, and Mars (sizes to scale, interplanetary distances not)

The four inner or terrestrial planets have dense, rocky compositions, few or no moons, and no ring systems. They are composed largely of refractory minerals, such as the silicates, which form their crusts and mantles, and metals such as iron and nickel, which form their cores. Three of the four inner planets (Venus, Earth and Mars) have atmospheres substantial enough to generate weather; all have impact craters and tectonic surface features such as rift valleys and volcanoes. The term inner planet should not be confused with inferior planet, which designates those planets that are closer to the Sun than Earth is (i.e. Mercury and Venus).

Mercury

Mercury (0.4 AU from the Sun) is the closest planet to the Sun and the smallest planet in the Solar System (0.055 Earth masses). Mercury has no natural satellites, and its only known geological features besides impact craters are lobed ridges or rupes, probably produced by a period of contraction early in its history.^[41] Mercury's almost negligible atmosphere consists of atoms blasted off its surface by the solar wind.^[42] Its relatively large iron core and thin mantle have not yet been adequately explained. Hypotheses include that its outer layers were stripped off by a giant impact, and that it was prevented from fully accreting by the young Sun's energy.^[43]^[44]

Venus

Venus (0.7 AU from the Sun) is close in size to Earth (0.815 Earth masses), and, like Earth, has a thick silicate mantle around an iron core, a substantial atmosphere and evidence of internal geological activity. However, it is much drier than Earth and its atmosphere is ninety times as dense. Venus has no natural satellites. It is the hottest planet, with surface temperatures over 400 °C, most likely due to the amount of greenhouse gases in the atmosphere.^[45] No definitive evidence of current geological activity has been detected on Venus, but it has no magnetic field that would prevent depletion of its substantial atmosphere, which suggests that its atmosphere is regularly replenished by volcanic eruptions.^[46]

Earth

Earth (1 AU from the Sun) is the largest and densest of the inner planets, the only one known to have current geological activity, and is the only place in the Solar System where life is known to exist.^[47] Its liquid hydrosphere is unique among the terrestrial planets, and it is also the only planet where plate tectonics has been observed. Earth's atmosphere is radically different from those of the other planets, having been altered by the presence of life to contain 21% free oxygen.^[48] It has one natural satellite, the Moon, the only large satellite of a terrestrial planet in the Solar System.

Mars

Mars (1.5 AU from the Sun) is smaller than Earth and Venus (0.107 Earth masses). It possesses an atmosphere of mostly carbon dioxide with a surface pressure of 6.1 millibars (roughly 0.6 percent that of the Earth's).^[49] Its surface, peppered with vast volcanoes such as Olympus Mons and rift valleys such as Valles Marineris, shows geological activity that may have persisted until as recently as 2 million years ago.^[50] Its red colour comes from iron oxide (rust) in its soil.^[51] Mars has two tiny natural satellites (Deimos and Phobos) thought to be captured asteroids.^[52]

Asteroid belt

Main article: Asteroid belt

Image of the asteroid belt and the Trojan asteroids

Asteroids are small Solar System bodies^[e] composed mainly of refractory rocky and metallic minerals, with some ice.^[53]

The asteroid belt occupies the orbit between Mars and Jupiter, between 2.3 and 3.3 AU from the Sun. It is thought to be remnants from the Solar System's formation that failed to coalesce because of the gravitational interference of Jupiter.^[54]

Asteroids range in size from hundreds of kilometres across to microscopic. All asteroids except the largest, Ceres, are classified as small Solar System bodies, but some asteroids such as Vesta and Hygiea may be reclassed as dwarf planets if they are shown to have achieved hydrostatic equilibrium.^[55]

The asteroid belt contains tens of thousands, possibly millions, of objects over one kilometre in diameter.^[56] Despite this, the total mass of the asteroid belt is unlikely to be more than a thousandth of that of the Earth.^[57] The asteroid belt is very sparsely populated; spacecraft routinely pass through without incident. Asteroids with diameters between 10 and 10⁻⁴ m are called meteoroids.^[58]

Ceres

Ceres (2.77 AU) is the largest asteroid, a protoplanet, and a dwarf planet.^[e] It has a diameter of slightly under 1000 km, and a mass large enough for its own gravity to pull it into a spherical shape. Ceres was considered a planet when it was discovered in the 19th century, but was reclassified as an asteroid in the 1850s as further observations revealed additional asteroids.^[59] It was classified in 2006 as a dwarf planet.

Asteroid groups

Asteroids in the asteroid belt are divided into asteroid groups and families based on their orbital characteristics. Asteroid moons are asteroids that orbit larger asteroids. They are not as clearly distinguished as planetary moons, sometimes being almost as large as their partners. The asteroid belt also contains main-belt comets, which may have been the source of Earth's water.^[60]

Trojan asteroids are located in either of Jupiter's L₄ or L₅ points (gravitationally stable regions leading and trailing a planet in its orbit); the term "Trojan" is also used for small bodies in any other planetary or satellite Lagrange point. Hilda asteroids are in a 2:3 resonance with Jupiter; that is, they go around the Sun three times for every two Jupiter orbits.^[61]

The inner Solar System is also dusted with rogue asteroids, many of which cross the orbits of the inner planets.^[62]

Outer Solar System

The outer region of the Solar System is home to the gas giants and their large moons. Many short-period comets, including the centaurs, also orbit in this region. Due to their greater distance from the Sun, the solid objects in the outer Solar System contain a higher proportion of volatiles such as water, ammonia and methane, than the rocky denizens of the inner Solar System, as the colder temperatures allow these compounds to remain solid.

Outer planets

Main articles: Outer planets and Gas giant

From top to bottom: Neptune, Uranus, Saturn, and Jupiter (not to scale)

The four outer planets, or gas giants (sometimes called Jovian planets), collectively make up 99 percent of the mass known to orbit the Sun.^[c] Jupiter and Saturn are each many tens of times the mass of the Earth and consist overwhelmingly of hydrogen and helium; Uranus and Neptune are far less massive (<20 Earth masses) and possess more ices in their makeup. For these reasons, some astronomers suggest they belong in their own category, "ice giants".^[63] All four gas giants have rings, although only Saturn's ring system is easily observed from Earth. The term outer planet should not be confused with superior planet, which designates planets outside Earth's orbit and thus includes both the outer planets and Mars.

Jupiter

Jupiter (5.2 AU), at 318 Earth masses, is 2.5 times the mass of all the other planets put together. It is composed largely of hydrogen and helium. Jupiter's strong internal heat creates a number of semi-permanent features in its atmosphere, such as cloud bands and the Great Red Spot.

Jupiter has 66 known satellites. The four largest, Ganymede, Callisto, Io, and Europa, show similarities to the terrestrial planets, such as volcanism and internal heating.^[64] Ganymede, the largest satellite in the Solar System, is larger than Mercury.

Saturn

Saturn (9.5 AU), distinguished by its extensive ring system, has several similarities to Jupiter, such as its atmospheric composition and magnetosphere. Although Saturn has 60% of Jupiter's volume, it is less than a third as massive, at 95 Earth masses, making it the least dense planet in the Solar System. The rings of Saturn are made up of small ice and rock particles.

Saturn has 62 confirmed satellites; two of which, Titan and Enceladus, show signs of geological activity, though they are largely made of ice.^[65] Titan, the second-largest moon in the Solar System, is larger than Mercury and the only satellite in the Solar System with a substantial atmosphere.

Uranus

Uranus (19.6 AU), at 14 Earth masses, is the lightest of the outer planets. Uniquely among the planets, it orbits the Sun on its side; its axial tilt is over ninety degrees to the ecliptic. It has a much colder core than the other gas giants, and radiates very little heat into space.^[66]

Uranus has 27 known satellites, the largest ones being Titania, Oberon, Umbriel, Ariel and Miranda.

Neptune

Neptune (30 AU), though slightly smaller than Uranus, is more massive (equivalent to 17 Earths) and therefore more dense. It radiates more internal heat, but not as much as Jupiter or Saturn.^[67]

Neptune has 13 known satellites. The largest, Triton, is geologically active, with geysers of liquid nitrogen.^[68] Triton is the only large satellite with a retrograde orbit. Neptune is accompanied in its orbit by a number of minor planets, termed Neptune trojans, that are in 1:1 resonance with it.

Comets

Main article: Comet

Comet Hale–Bopp

Comets are small Solar System bodies,^[e] typically only a few kilometres across, composed largely of volatile ices. They have highly eccentric orbits, generally a perihelion within the orbits of the inner planets and an aphelion far beyond Pluto. When a comet enters the inner Solar System, its proximity to the Sun causes its icy surface to sublimate and ionise, creating a coma: a long tail of gas and dust often visible to the naked eye.

Short-period comets have orbits lasting less than two hundred years. Long-period comets have orbits lasting thousands of years. Short-period comets are believed to originate in the Kuiper belt, while long-period comets, such as Hale–Bopp, are believed to originate in the Oort cloud. Many comet groups, such as the Kreutz Sungrazers, formed from the breakup of a single parent.^[69] Some comets with hyperbolic orbits may originate outside the Solar System, but determining their precise orbits is difficult.^[70] Old comets that have had most of their volatiles driven out by solar warming are often categorised as asteroids.^[71]

Centaurs

Main article: Centaur (minor planet)

The centaurs are icy comet-like bodies with a semi-major axis greater than Jupiter's (5.5 AU) and less than Neptune's (30 AU). The largest known centaur, 10199 Chariklo, has a diameter of about 250 km.^[72] The first centaur discovered, 2060 Chiron, has also been classified as comet (95P) since it develops a coma just as comets do when they approach the Sun.^[73]

Trans-Neptunian region

The area beyond Neptune, or the "trans-Neptunian region", is still largely unexplored. It appears to consist overwhelmingly of small worlds (the largest having a diameter only a fifth that of the Earth and a mass far smaller than that of the Moon) composed mainly of rock and ice. This region is sometimes known as the "outer Solar System", though others use that term to mean the region beyond the asteroid belt.

Kuiper belt

Main article: Kuiper belt

Plot of all known Kuiper belt objects, set against the four outer planets

The Kuiper belt, the region's first formation, is a great ring of debris similar to the asteroid belt, but composed mainly of ice.^[74] It extends between 30 and 50 AU from the Sun. Though it contains at least three dwarf planets, it is composed mainly of small Solar System bodies. However, many of the largest Kuiper belt objects, such as Quaoar, Varuna, and Orcus, may be reclassified as dwarf planets. There are estimated to be over 100,000 Kuiper belt objects with a diameter greater than 50 km, but the total mass of the Kuiper belt is thought to be only a tenth or even a hundredth the mass of the Earth.^[75] Many Kuiper belt objects have multiple satellites,^[76] and most have orbits that take them outside the plane of the ecliptic.^[77]

The Kuiper belt can be roughly divided into the "classical" belt and the resonances.^[74] Resonances are orbits linked to that of Neptune (e.g. twice for every three Neptune orbits, or once for every two). The first resonance begins within the orbit of Neptune itself. The classical belt consists of objects having no resonance with Neptune, and extends from roughly 39.4 AU to 47.7 AU.^[78] Members of the classical Kuiper belt are classified as cubewanos, after the first of their kind to be discovered, (15760) 1992 QB₁, and are still in near primordial, low-eccentricity orbits.^[79]

Pluto and Charon

Artistic comparison of Eris, Pluto, Makemake, Haumea, Sedna, 2007 OR₁₀, Quaoar, Orcus, and Earth. These eight trans-Neptunian objects have the brightest absolute magnitudes; several other TNOs have been found to be physically larger than Orcus, and several more may yet be found to be that.

Pluto (39 AU average), a dwarf planet, is the largest known object in the Kuiper belt. When discovered in 1930, it was considered to be the ninth planet; this changed in 2006 with the adoption of a formal definition of planet. Pluto has a relatively eccentric orbit inclined 17 degrees to the ecliptic plane and ranging from 29.7 AU from the Sun at perihelion (within the orbit of Neptune) to 49.5 AU at aphelion.

Charon, Pluto's largest moon, is sometimes described as part of a binary system with Pluto, as the two bodies orbit a barycenter of gravity above their surfaces (i.e., they appear to "orbit each other"). Beyond Charon, three much smaller moons, Nix, P4 and Hydra, orbit within the system.

Pluto has a 3:2 resonance with Neptune, meaning that Pluto orbits twice round the Sun for every three Neptunian orbits. Kuiper belt objects whose orbits share this resonance are called plutinos.^[80]

Haumea and Makemake

Haumea (43.34 AU average), and Makemake (45.79 AU average), while smaller than Pluto, are the largest known objects in the classical Kuiper belt (that is, they are not in a confirmed resonance with Neptune). Haumea is an egg-shaped object with two moons. Makemake is the brightest object in the Kuiper belt after Pluto. Originally designated 2003 EL₆₁ and 2005 FY₉ respectively, they were given names and designated dwarf planets in 2008.^[81] Their orbits are far more inclined than Pluto's, at 28° and 29°.^[82]

Scattered disc

Main article: Scattered disc

The scattered disc, which overlaps the Kuiper belt but extends much further outwards, is thought to be the source of short-period comets. Scattered disc objects are believed to have been ejected into erratic orbits by the gravitational influence of Neptune's early outward migration. Most scattered disc objects (SDOs) have perihelia within the Kuiper belt but aphelia as far as 150 AU from the Sun. SDOs' orbits are also highly inclined to the ecliptic plane, and are often almost perpendicular to it. Some astronomers consider the scattered disc to be merely another region of the Kuiper belt, and describe scattered disc objects as "scattered Kuiper belt objects."^[83] Some astronomers also classify centaurs as inward-scattered Kuiper belt objects along with the outward-scattered residents of the scattered disc.^[84]

Eris

Eris (68 AU average) is the largest known scattered disc object, and caused a debate about what constitutes a planet, since it is 25% more massive than Pluto^[85] and about the same diameter. It is the most massive of the known dwarf planets. It has one moon, Dysnomia. Like Pluto, its orbit is highly eccentric, with a perihelion of 38.2 AU (roughly Pluto's distance from the Sun) and an aphelion of 97.6 AU, and steeply inclined to the ecliptic plane.

Farthest regions

The point at which the Solar System ends and interstellar space begins is not precisely defined, since its outer boundaries are shaped by two separate forces: the solar wind and the Sun's gravity. The outer limit of the solar wind's influence is roughly four times Pluto's distance from the Sun; this heliopause is considered the beginning of the interstellar medium.^[31] However, the Sun's Roche sphere, the effective range of its gravitational dominance, is believed to extend up to a thousand times farther.^[86]

Heliopause

Energetic neutral atoms map of heliosheath and heliopause by IBEX. Credit: NASA/Goddard Space Flight Center Scientific Visualization Studio.

The heliosphere is divided into two separate regions. The solar wind travels at roughly 400 km/s until it collides with the interstellar wind; the flow of plasma in the interstellar medium. The collision occurs at the termination shock, which is roughly 80–100 AU from the Sun upwind of the interstellar medium and roughly 200 AU from the Sun downwind.^[87] Here the wind slows dramatically, condenses and becomes more turbulent,^[87] forming a great oval structure known as the heliosheath. This structure is believed to look and behave very much like a comet's tail, extending outward for a further 40 AU on the upwind side but tailing many times that distance downwind; but evidence from the Cassini and Interstellar Boundary Explorer spacecraft has suggested that it is in fact forced into a bubble shape by the constraining action of the interstellar magnetic field.^[88] Both Voyager 1 and Voyager 2 are reported to have passed the termination shock and entered the heliosheath, at 94 and 84 AU from the Sun, respectively.^[89]^[90] The outer boundary of the heliosphere, the heliopause, is the point at which the solar wind finally terminates and is the beginning of interstellar space.^[31]

The shape and form of the outer edge of the heliosphere is likely affected by the fluid dynamics of interactions with the interstellar medium^[87] as well as solar magnetic fields prevailing to the south, e.g. it is bluntly shaped with the northern hemisphere extending 9 AU farther than the southern hemisphere. Beyond the heliopause, at around 230 AU, lies the bow shock, a plasma "wake" left by the Sun as it travels through the Milky Way.^[91]

No spacecraft have yet passed beyond the heliopause, so it is impossible to know for certain the conditions in local interstellar space. It is expected that NASA's Voyager spacecraft will pass the heliopause some time in the next decade and transmit valuable data on radiation levels and solar wind back to the Earth.^[92] How well the heliosphere shields the Solar System from cosmic rays is poorly understood. A NASA-funded team has developed a concept of a "Vision Mission" dedicated to sending a probe to the heliosphere.^[93]^[94]

Oort cloud

Main article: Oort cloud

An artist's rendering of the Oort Cloud, the Hills Cloud, and the Kuiper belt (inset)

The hypothetical Oort cloud is a spherical cloud of up to a trillion icy objects that is believed to be the source for all long-period comets and to surround the Solar System at roughly 50,000 AU (around 1 light-year (LY)), and possibly to as far as 100,000 AU (1.87 LY). It is believed to be composed of comets that were ejected from the inner Solar System by gravitational interactions with the outer planets. Oort cloud objects move very slowly, and can be perturbed by infrequent events such as collisions, the gravitational effects of a passing star, or the galactic tide, the tidal force exerted by the Milky Way.^[95]^[96]

Sedna

90377 Sedna (525.86 AU average) is a large, reddish probable dwarf planet with a gigantic, highly elliptical orbit that takes it from about 76 AU at perihelion to 928 AU at aphelion and takes 12,050 years to complete. Mike Brown, who discovered the object in 2003, asserts that it cannot be part of the scattered disc or the Kuiper belt as its perihelion is too distant to have been affected by Neptune's migration. He and other astronomers consider it to be the first in an entirely new population, which also may include the object 2000 CR₁₀₅, which has a perihelion of 45 AU, an aphelion of 415 AU, and an orbital period of 3,420 years.^[97] Brown terms this population the "Inner Oort cloud", as it may have formed through a similar process, although it is far closer to the Sun.^[98] Sedna is very likely a dwarf planet, though its shape has yet to be determined with certainty.

Boundaries

Much of the Solar System is still unknown. The Sun's gravitational field is estimated to dominate the gravitational forces of surrounding stars out to about two light years (125,000 AU). Lower estimates for the radius of the Oort cloud, by contrast, do not place it farther than 50,000 AU.^[99] Despite discoveries such as Sedna, the region between the Kuiper belt and the Oort cloud, an area tens of thousands of AU in radius, is still virtually unmapped. There are also ongoing studies of the region between Mercury and the Sun.^[100] Objects may yet be discovered in the Solar System's uncharted regions.

Galactic context

Location of the Solar System within our galaxy

The Solar System is located in the Milky Way galaxy, a barred spiral galaxy with a diameter of about 100,000 light-years containing about 200 billion stars.^[101] The Sun resides in one of the Milky Way's outer spiral arms, known as the Orion Arm or Local Spur.^[102] The Sun lies between 25,000 and 28,000 light years from the Galactic Centre,^[103] and its speed within the galaxy is about 220 kilometres per second, so that it completes one revolution every 225–250 million years. This revolution is known as the Solar System's galactic year.^[104] The solar apex, the direction of the Sun's path through interstellar space, is near the constellation of Hercules in the direction of the current location of the bright star Vega.^[105] The plane of the ecliptic lies at an angle of about 60° to the galactic plane.^[f]

The Solar System's location in the galaxy is a factor in the evolution of life on Earth. Its orbit is close to circular, and orbits near the Sun are at roughly the same speed as that of the spiral arms. Therefore, the Sun passes through arms only rarely. Since spiral arms are home to a far larger concentration of supernovae, gravitational instabilities, and radiation which could disrupt the Solar System, this has given Earth long periods of stability for life to evolve.^[106] The Solar System also lies well outside the star-crowded environs of the galactic centre. Near the centre, gravitational tugs from nearby stars could perturb bodies in the Oort Cloud and send many comets into the inner Solar System, producing collisions with potentially catastrophic implications for life on Earth. The intense radiation of the galactic centre could also interfere with the development of complex life.^[106] Even at the Solar System's current location, some scientists have hypothesised that recent supernovae may have adversely affected life in the last 35,000 years by flinging pieces of expelled stellar core towards the Sun as radioactive dust grains and larger, comet-like bodies.^[107]

Neighbourhood

The immediate galactic neighbourhood of the Solar System is known as the Local Interstellar Cloud or Local Fluff, an area of denser cloud in an otherwise sparse region known as the Local Bubble, an hourglass-shaped cavity in the interstellar medium roughly 300 light years across. The bubble is suffused with high-temperature plasma that suggests it is the product of several recent supernovae.^[108]

There are relatively few stars within ten light years (95 trillion km) of the Sun. The closest is the triple star system Alpha Centauri, which is about 4.4 light years away. Alpha Centauri A and B are a closely tied pair of Sun-like stars, while the small red dwarf Alpha Centauri C (also known as Proxima Centauri) orbits the pair at a distance of 0.2 light years. The stars next closest to the Sun are the red dwarfs Barnard's Star (at 5.9 light years), Wolf 359 (7.8 light years) and Lalande 21185 (8.3 light years). The largest star within ten light years is Sirius, a bright main-sequence star roughly twice the Sun's mass and orbited by a white dwarf called Sirius B. It lies 8.6 light years away. The remaining systems within ten light years are the binary red dwarf system Luyten 726-8 (8.7 light years) and the solitary red dwarf Ross 154 (9.7 light years).^[109] The Solar System's closest solitary sun-like star is Tau Ceti, which lies 11.9 light years away. It has roughly 80 percent the Sun's mass, but only 60 percent of its luminosity.^[110] The closest known extrasolar planet to the Sun lies around the star Epsilon Eridani, a star slightly dimmer and redder than the Sun, which lies 10.5 light years away. Its one confirmed planet, Epsilon Eridani b, is roughly 1.5 times Jupiter's mass and orbits its star every 6.9 years.^[111]

A diagram of our location in the observable Universe. (Click here for larger image.)

Formation and evolution

Main article: Formation and evolution of the Solar System

The Solar System formed from the gravitational collapse of a giant molecular cloud 4.568 billion years ago.^[112] This initial cloud was likely several light-years across and probably birthed several stars.^[113] As the region that would become the Solar System, known as the pre-solar nebula,^[114] collapsed, conservation of angular momentum made it rotate faster. The centre, where most of the mass collected, became increasingly hotter than the surrounding disc.^[113] As the contracting nebula rotated, it began to flatten into a spinning protoplanetary disc with a diameter of roughly 200 AU^[113] and a hot, dense protostar at the centre.^[115]^[116] The planets formed by accretion from this disk.^[117]

Within 50 million years, the pressure and density of hydrogen in the centre of the protostar became great enough for it to begin thermonuclear fusion.^[118] The temperature, reaction rate, pressure, and density increased until hydrostatic equilibrium was achieved: the thermal pressure equaled the force of gravity. At this point the Sun became a main-sequence star.^[119]

The Nice model explains many otherwise puzzling features of the history and structure of the Solar System. In this model, the four giant planets (Jupiter, Saturn, Uranus and Neptune) originally formed in orbits between ~5.5 and ~17 astronomical units (AU) from the Sun, (inside the current orbit of Uranus). A disk of planetesimals, of ~35 Earth masses, extended beyond this to ~35 AU. Gravitational interactions between these planets and the planetismal disc caused changes to the planets' orbits. Over a period of several hundred million years, Saturn, Uranus and Neptune migrated outwards, Neptune passing Uranus, while Jupiter migrated a small distance inwards.

The Solar System will remain roughly as we know it today until the hydrogen in the core of the Sun has been entirely converted to helium, which will occur roughly 5.4 billion years from now. This will mark the end of the Sun's main sequence life. At this time, the core of the Sun will collapse, and the energy output will be much greater than at present. The outer layers of the Sun will expand to roughly up to 260 times its current diameter; the Sun will become a red giant. Because of its vastly increased surface area, the surface of the Sun will be considerably cooler than it is on the main sequence (2600 K at the coolest).^[120] Eventually, the core will be hot enough for helium fusion to begin in the core; the Sun will burn helium for a fraction of the time it burned hydrogen in the core. The Sun is not massive enough to commence fusion of heavier elements, and nuclear reactions in the core will dwindle. Its outer layers will fall away into space, leaving a white dwarf, an extraordinarily dense object, half the original mass of the Sun but only the size of the Earth.^[121] The ejected outer layers will form what is known as a planetary nebula, returning some of the material that formed the Sun -- but now enriched with heavier elements like carbon -- to the interstellar medium.

Visual summary

A sampling of closely imaged Solar System bodies, selected for size and detail and sorted by volume. The Sun is approximately 10,000 times larger than, and 41 trillion times the volume of, the smallest object shown (Prometheus). Other lists include: List of Solar System objects by size, List of natural satellites, List of minor planets, and Lists of comets.

Solar System

Sun	Jupiter	Saturn	Uranus	Neptune	Earth	Venus

Mars	Ganymede	Titan	Mercury	Callisto	Io	Moon

Europa	Triton	Titania	Rhea	Oberon	Iapetus	Umbriel

Ariel	Dione	Tethys	Vesta	Enceladus	Miranda	Proteus

Mimas	Hyperion	Phoebe	Janus	Amalthea	Epimetheus	Prometheus

Notes

^{^} Capitalization of the name varies. The IAU, the authoritative body regarding astronomical nomenclature, specifies capitalizing the names of all individual astronomical objects (Solar System). However, the name is commonly rendered in lower case (solar system) – as, for example, in the Oxford English Dictionary and Merriam-Webster's 11th Collegiate Dictionary
^{^} See List of natural satellites for the full list of natural satellites of the eight planets and five dwarf planets.
^{^} The mass of the Solar System excluding the Sun, Jupiter and Saturn can be determined by adding together all the calculated masses for its largest objects and using rough calculations for the masses of the Oort cloud (estimated at roughly 3 Earth masses),^[122] the Kuiper belt (estimated at roughly 0.1 Earth mass)^[75] and the asteroid belt (estimated to be 0.0005 Earth mass)^[57] for a total, rounded upwards, of ~37 Earth masses, or 8.1 percent the mass in orbit around the Sun. With the combined masses of Uranus and Neptune (~31 Earth masses) subtracted, the remaining ~6 Earth masses of material comprise 1.3 percent of the total.
^{^} Astronomers measure distances within the Solar System in astronomical units (AU). One AU equals the average distance between the centers of Earth and the Sun, or 149,598,000 km. Pluto is about 38 AU from the Sun and Jupiter is about 5.2 AU from the Sun. One light-year is 63,240 AU.
^{^} According to current definitions, objects in orbit around the Sun are classed dynamically and physically into three categories: planets, dwarf planets and small Solar System bodies. A planet is any body in orbit around the Sun that has enough mass to form itself into a spherical shape and has cleared its immediate neighbourhood of all smaller objects. By this definition, the Solar System has eight known planets: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. Pluto does not fit this definition, as it has not cleared its orbit of surrounding Kuiper belt objects.^[123] A dwarf planet is a celestial body orbiting the Sun that is massive enough to be rounded by its own gravity but has not cleared its neighbouring region of planetesimals and is not a satellite.^[123] By this definition, the Solar System has five known dwarf planets: Ceres, Pluto, Haumea, Makemake, and Eris.^[81] Other objects may be classified in the future as dwarf planets, such as Sedna, Orcus, and Quaoar.^[124] Dwarf planets that orbit in the trans-Neptunian region are called "plutoids".^[125] The remainder of the objects in orbit around the Sun are small Solar System bodies.^[123]
^{^} If ψ is the angle between the north pole of the ecliptic and the north galactic pole then:

$\cos\psi=\cos(\beta_g)\cos(\beta_e)\cos(\alpha_g-\alpha_e)+\sin(\beta_g)\sin(\beta_e)$ ,

where $\beta_g=$ 27° 07′ 42.01″ and $\alpha_g=$ 12h 51m 26.282 are the declination and right ascension of the north galactic pole,^[126] while $\beta_e=$ 66° 33′ 38.6″ and $\alpha_e=$ 18h 0m 00 are those for the north pole of the ecliptic. (Both pairs of coordinates are for J2000 epoch.) The result of the calculation is 60.19°.

References

^ WC Rufus (1923). "The astronomical system of Copernicus". Popular Astronomy 31: 510. Bibcode 1923PA.....31..510R.
^ Weinert, Friedel (2009). Copernicus, Darwin, & Freud: revolutions in the history and philosophy of science. Wiley-Blackwell. p. 21. ISBN 978-1-4051-8183-9.
^ M Woolfson (2000). "The origin and evolution of the solar system". Astronomy & Geophysics 41 (1): 1.12. doi:10.1046/j.1468-4004.2000.00012.x.
^ Levison, H. F.; Morbidelli, A. (2003-11-27). "The formation of the Kuiper belt by the outward transport of bodies during Neptune's migration". Nature 426: 419-421. doi:10.1038/nature02120. PMID 14647375. http://www.nature.com/nature/journal/v426/n6965/abs/nature02120.html. Retrieved 2012-05-26.
^ Harold F. Levison, Martin J Duncan (1997). "From the Kuiper Belt to Jupiter-Family Comets: The Spatial Distribution of Ecliptic Comets". Icarus 127 (1): 13–32. Bibcode 1997Icar..127...13L. doi:10.1006/icar.1996.5637.
^ Grossman, Lisa (13 August 2009). "Planet found orbiting its star backwards for first time". NewScientist. http://www.newscientist.com/article/dn17603-planet-found-orbiting-its-star-backwards-for-first-time.html. Retrieved 10 October 2009.
^ nineplanets.org. "An Overview of the Solar System". http://www.nineplanets.org/overview.html. Retrieved 2007-02-15.
^ Amir Alexander (2006). "New Horizons Set to Launch on 9-Year Voyage to Pluto and the Kuiper Belt". The Planetary Society. http://www.planetary.org/news/2006/0116_New_Horizons_Set_to_Launch_on_9_Year.html. Retrieved 2006-11-08.
^ "Dawn: A Journey to the Beginning of the Solar System". Space Physics Center: UCLA. 2005. http://www-ssc.igpp.ucla.edu/dawn/background.html. Retrieved 2007-11-03.
^ Guy Ottewell (1989). "The Thousand-Yard Model". NOAO Educational Outreach Office. http://www.noao.edu/education/peppercorn/pcmain.html. Retrieved 2012-5-10.
^ "Tours of Model Solar Systems". University of Illinois. http://internal.psychology.illinois.edu/~wbrewer/solarmodel.html. Retrieved 2012-05-10.
^ "Luleå är Sedna. I alla fall om vår sol motsvaras av Globen i Stockholm.". Norrbotten Kuriren (in swedish). http://www.kuriren.nu/arkiv/2005/11/17/Lokalt/1510647/Lule%C3%A5-%C3%A4r-Sedna.aspx. Retrieved 2010-05-10.
^ "The Sun's Vital Statistics". Stanford Solar Center. http://solar-center.stanford.edu/vitalstats.html. Retrieved 2008-07-29. , citing Eddy, J. (1979). A New Sun: The Solar Results From Skylab. NASA. p. 37. NASA SP-402. http://history.nasa.gov/SP-402/contents.htm.
^ Williams, Dr. David R. (September 7, 2006). "Saturn Fact Sheet". NASA. http://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html. Retrieved 2007-07-31.
^ Williams, Dr. David R. (November 16, 2004). "Jupiter Fact Sheet". NASA. http://nssdc.gsfc.nasa.gov/planetary/factsheet/jupiterfact.html. Retrieved 2007-08-08.
^ Paul Robert Weissman, Torrence V. Johnson (2007). Encyclopedia of the solar system. Academic Press. p. 615. ISBN 0-12-088589-1.
^ "Planet Formation (in the Solar System)". University of Toronto. http://www.astro.utoronto.ca/~mhvk/AST221/L20/L20_4.pdf. Retrieved 2011-07-11.
^ ^a ^b ^c Podolak, M.; Weizman, A.; Marley, M. (December 1995). "Comparative models of Uranus and Neptune". Planetary and Space Science 43 (12): 1517–1522. Bibcode 1995P&SS...43.1517P. doi:10.1016/0032-0633(95)00061-5. edit
^ ^a ^b ^c ^d Podolak, M.; Podolak, J. I.; Marley, M. S. (February 2000). "Further investigations of random models of Uranus and Neptune". Planetary and Space Science 48 (2–3): 143–151. Bibcode 2000P&SS...48..143P. doi:10.1016/S0032-0633(99)00088-4. edit
^ Michael Zellik (2002). Astronomy: The Evolving Universe (9th ed.). Cambridge University Press. p. 240. ISBN 0-521-80090-0. OCLC 46685453 223304585 46685453.
^ Placxo, Kevin W.; Gross, Michael (2006). Astrobiology: a brief introduction. JHU Press. p. 66. ISBN 978-0-8018-8367-5. http://books.google.com/?id=2JuGDL144BEC&pg=PA66&dq=inventory+volatiles+hydrogen&q=inventory%20volatiles%20hydrogen.
^ "Sun: Facts & Figures". NASA. Archived from the original on 2008-01-02. http://web.archive.org/web/20080102034758/http://solarsystem.nasa.gov/planets/profile.cfm?Object=Sun&Display=Facts&System=Metric. Retrieved 2009-05-14.
^ Zirker, Jack B. (2002). Journey from the Center of the Sun. Princeton University Press. pp. 120–127. ISBN 978-0-691-05781-1.
^ "Why is visible light visible, but not other parts of the spectrum?". The Straight Dome. 2003. http://www.straightdope.com/columns/read/2085/why-is-visible-light-visible-but-not-other-parts-of-the-spectrum. Retrieved 2009-05-14.
^ ^a ^b Than, Ker (January 30, 2006). "Astronomers Had it Wrong: Most Stars are Single". SPACE.com. http://www.space.com/scienceastronomy/060130_mm_single_stars.html. Retrieved 2007-08-01.
^ Smart, R. L.; Carollo, D.; Lattanzi, M. G.; McLean, B.; Spagna, A. (2001). "The Second Guide Star Catalogue and Cool Stars". In Hugh R. A. Jones and Iain A. Steele. Ultracool Dwarfs: New Spectral Types L and T. Springer. pp. 119. Bibcode 2001udns.conf..119S.
^ Nir J. Shaviv (2003). "Towards a Solution to the Early Faint Sun Paradox: A Lower Cosmic Ray Flux from a Stronger Solar Wind". Journal of Geophysical Research 108 (A12): 1437. arXiv:astroph/0306477. Bibcode 2003JGRA..108.1437S. doi:10.1029/2003JA009997.
^ T. S. van Albada, Norman Baker (1973). "On the Two Oosterhoff Groups of Globular Clusters". Astrophysical Journal 185: 477–498. Bibcode 1973ApJ...185..477V. doi:10.1086/152434.
^ Charles H. Lineweaver (2001-03-09). "An Estimate of the Age Distribution of Terrestrial Planets in the Universe: Quantifying Metallicity as a Selection Effect". Icarus 151 (2): 307–313. Bibcode 2001Icar..151..307L. doi:10.1006/icar.2001.6607.
^ "Solar Physics: The Solar Wind". Marshall Space Flight Center. 2006-07-16. http://solarscience.msfc.nasa.gov/SolarWind.shtml. Retrieved 2006-10-03.
^ ^a ^b ^c "Voyager Enters Solar System's Final Frontier". NASA. http://www.nasa.gov/vision/universe/solarsystem/voyager_agu.html. Retrieved 2007-04-02.
^ Phillips, Tony (2001-02-15). "The Sun Does a Flip". Science@NASA. http://science.nasa.gov/headlines/y2001/ast15feb_1.htm. Retrieved 2007-02-04.
^ A Star with two North Poles, April 22, 2003, Science @ NASA
^ Riley, Pete (2002). "Modeling the heliospheric current sheet: Solar cycle variations". Journal of Geophysical Research 107. Bibcode 2002JGRA.107g.SSH8R. doi:10.1029/2001JA000299. http://ulysses.jpl.nasa.gov/science/monthly_highlights/2002-July-2001JA000299.pdf.
^ Lundin, Richard (2001-03-09). "Erosion by the Solar Wind". Science 291 (5510): 1909. doi:10.1126/science.1059763. PMID 11245195.
^ Langner, U. W.; M. S. Potgieter (2005). "Effects of the position of the solar wind termination shock and the heliopause on the heliospheric modulation of cosmic rays". Advances in Space Research 35 (12): 2084–2090. Bibcode 2005AdSpR..35.2084L. doi:10.1016/j.asr.2004.12.005.
^ "Long-term Evolution of the Zodiacal Cloud". 1998. http://astrobiology.arc.nasa.gov/workshops/1997/zodiac/backman/IIIc.html. Retrieved 2007-02-03.
^ "ESA scientist discovers a way to shortlist stars that might have planets". ESA Science and Technology. 2003. http://sci.esa.int/science-e/www/object/index.cfm?fobjectid=29471. Retrieved 2007-02-03.
^ Landgraf, M.; Liou, J.-C.; Zook, H. A.; Grün, E. (May 2002). "Origins of Solar System Dust beyond Jupiter". The Astronomical Journal 123 (5): 2857–2861. Bibcode 2002AJ....123.2857L. doi:10.1086/339704. http://astron.berkeley.edu/~kalas/disksite/library/ladgraf02.pdf. Retrieved 2007-02-09.
^ "Inner Solar System". NASA Science (Planets). http://nasascience.nasa.gov/planetary-science/exploring-the-inner-solar-system. Retrieved 2009-05-09.
^ Schenk P., Melosh H. J. (1994), Lobate Thrust Scarps and the Thickness of Mercury's Lithosphere, Abstracts of the 25th Lunar and Planetary Science Conference, 1994LPI....25.1203S
^ Bill Arnett (2006). "Mercury". The Nine Planets. http://www.nineplanets.org/mercury.html. Retrieved 2006-09-14.
^ Benz, W., Slattery, W. L., Cameron, A. G. W. (1988), Collisional stripping of Mercury's mantle, Icarus, v. 74, p. 516–528.
^ Cameron, A. G. W. (1985), The partial volatilization of Mercury, Icarus, v. 64, p. 285–294.
^ Mark Alan Bullock (1997) (PDF). The Stability of Climate on Venus. Southwest Research Institute. http://www.boulder.swri.edu/~bullock/Homedocs/PhDThesis.pdf. Retrieved 2006-12-26.
^ Paul Rincon (1999). "Climate Change as a Regulator of Tectonics on Venus" (PDF). Johnson Space Center Houston, TX, Institute of Meteoritics, University of New Mexico, Albuquerque, NM. http://www.boulder.swri.edu/~bullock/Homedocs/Science2_1999.pdf. Retrieved 2006-11-19.
^ "What are the characteristics of the Solar System that lead to the origins of life?". NASA Science (Big Questions). http://science.nasa.gov/planetary-science/big-questions/what-are-the-characteristics-of-the-solar-system-that-lead-to-the-origins-of-life-1/. Retrieved 2011-08-30.
^ Anne E. Egger, M.A./M.S.. "Earth's Atmosphere: Composition and Structure". VisionLearning.com. http://www.visionlearning.com/library/module_viewer.php?c3=&mid=107&l=. Retrieved 2006-12-26.
^ David C. Gatling, Conway Leovy (2007). "Mars Atmosphere: History and Surface Interactions". In Lucy-Ann McFadden et. al.. Encyclopaedia of the Solar System. pp. 301–314.
^ David Noever (2004). "Modern Martian Marvels: Volcanoes?". NASA Astrobiology Magazine. http://www.astrobio.net/news/modules.php?op=modload&name=News&file=article&sid=1360&mode=thread&order=0&thold=0. Retrieved 2006-07-23.
^ "Mars: A Kid's Eye View". NASA. http://solarsystem.nasa.gov/planets/profile.cfm?Object=Mars&Display=Kids. Retrieved 2009-05-14.
^ Scott S. Sheppard, David Jewitt, and Jan Kleyna (2004). "A Survey for Outer Satellites of Mars: Limits to Completeness". Astronomical Journal. http://www2.ess.ucla.edu/~jewitt/papers/2004/SJK2004.pdf. Retrieved 2006-12-26.
^ "Are Kuiper Belt Objects asteroids? Are large Kuiper Belt Objects planets?". Cornell University. http://curious.astro.cornell.edu/question.php?number=601. Retrieved 2009-03-01.
^ Petit, J.-M.; Morbidelli, A.; Chambers, J. (2001). "The Primordial Excitation and Clearing of the Asteroid Belt" (PDF). Icarus 153 (2): 338–347. Bibcode 2001Icar..153..338P. doi:10.1006/icar.2001.6702. http://www.gps.caltech.edu/classes/ge133/reading/asteroids.pdf. Retrieved 2007-03-22.
^ "IAU Planet Definition Committee". International Astronomical Union. 2006. http://www.iau.org/public_press/news/release/iau0601/newspaper/. Retrieved 2009-03-01.
^ "New study reveals twice as many asteroids as previously believed". ESA. 2002. http://www.esa.int/esaCP/ESAASPF18ZC_index_0.html. Retrieved 2006-06-23.
^ ^a ^b Krasinsky, G. A.; Pitjeva, E. V.; Vasilyev, M. V.; Yagudina, E. I. (July 2002). "Hidden Mass in the Asteroid Belt". Icarus 158 (1): 98–105. Bibcode 2002Icar..158...98K. doi:10.1006/icar.2002.6837.
^ Beech, M.; Steel; Duncan I. Steel (September 1995). "On the Definition of the Term Meteoroid". Quarterly Journal of the Royal Astronomical Society 36 (3): 281–284. Bibcode 1995QJRAS..36..281B.
^ "History and Discovery of Asteroids" (DOC). NASA. http://dawn.jpl.nasa.gov/DawnClassrooms/1_hist_dawn/history_discovery/Development/a_modeling_scale.doc. Retrieved 2006-08-29.
^ Phil Berardelli (2006). "Main-Belt Comets May Have Been Source Of Earths Water". SpaceDaily. http://www.spacedaily.com/reports/Main_Belt_Comets_May_Have_Been_Source_Of_Earths_Water.html. Retrieved 2006-06-23.
^ Barucci, M. A.; Kruikshank, D.P.; Mottola S.; Lazzarin M. (2002). "Physical Properties of Trojan and Centaur Asteroids". Asteroids III. Tucson, Arizona: University of Arizona Press. pp. 273–87.
^ A. Morbidelli, W. F. Bottke Jr., Ch. Froeschlé, P. Michel; Bottke; Froeschlé; Michel (January 2002). W. F. Bottke Jr., A. Cellino, P. Paolicchi, and R. P. Binzel. ed. "Origin and Evolution of Near-Earth Objects" (PDF). Asteroids III (University of Arizona Press): 409–422. Bibcode 2002aste.conf..409M. http://www.boulder.swri.edu/~bottke/Reprints/Morbidelli-etal_2002_AstIII_NEOs.pdf.
^ Jack J. Lissauer, David J. Stevenson (2006). "Formation of Giant Planets" (PDF). NASA Ames Research Center; California Institute of Technology. http://www.gps.caltech.edu/uploads/File/People/djs/lissauer&stevenson(PPV).pdf. Retrieved 2006-01-16.
^ Pappalardo, R T (1999). "Geology of the Icy Galilean Satellites: A Framework for Compositional Studies". Brown University. http://www.agu.org/cgi-bin/SFgate/SFgate?&listenv=table&multiple=1&range=1&directget=1&application=fm99&database=%2Fdata%2Fepubs%2Fwais%2Findexes%2Ffm99%2Ffm99&maxhits=200&=%22P11C-10%22. Retrieved 2006-01-16.
^ Kargel, J. S. (1994). "Cryovolcanism on the icy satellites". Earth, Moon, and Planets 67: 101–113. Bibcode 1995EM&P...67..101K. doi:10.1007/BF00613296.
^ Hawksett, David; Longstaff, Alan; Cooper, Keith; Clark, Stuart; Longstaff; Cooper; Clark (2005). "10 Mysteries of the Solar System". Astronomy Now 19: 65. Bibcode 2005AsNow..19h..65H.
^ Podolak, M.; Reynolds, R. T.; Young, R. (1990). "Post Voyager comparisons of the interiors of Uranus and Neptune". Geophysical Research Letters 17 (10): 1737. Bibcode 1990GeoRL..17.1737P. doi:10.1029/GL017i010p01737.
^ Duxbury, N. S., Brown, R. H. (1995). "The Plausibility of Boiling Geysers on Triton". Beacon eSpace. http://trs-new.jpl.nasa.gov/dspace/handle/2014/28034?mode=full. Retrieved 2006-01-16.
^ Sekanina, Zdeněk (2001). "Kreutz sungrazers: the ultimate case of cometary fragmentation and disintegration?". Publications of the Astronomical Institute of the Academy of Sciences of the Czech Republic 89: 78–93. Bibcode 2001PAICz..89...78S.
^ Królikowska, M. (2001). "A study of the original orbits of hyperbolic comets". Astronomy & Astrophysics 376 (1): 316–324. Bibcode 2001A&A...376..316K. doi:10.1051/0004-6361:20010945.
^ Whipple, Fred L. (1992). "The activities of comets related to their aging and origin". Celestial Mechanics and Dynamical Astronomy 54: 1–11. Bibcode 1992CeMDA..54....1W. doi:10.1007/BF00049540.
^ John Stansberry, Will Grundy, Mike Brown, Dale Cruikshank, John Spencer, David Trilling, Jean-Luc Margot (2007). "Physical Properties of Kuiper Belt and Centaur Objects: Constraints from Spitzer Space Telescope". The Solar System Beyond Neptune. pp. 161. arXiv:astro-ph/0702538. Bibcode 2008ssbn.book..161S.
^ Patrick Vanouplines (1995). "Chiron biography". Vrije Universitiet Brussel. http://www.vub.ac.be/STER/www.astro/chibio.htm. Retrieved 2006-06-23.
^ ^a ^b Stephen C. Tegler (2007). "Kuiper Belt Objects: Physical Studies". In Lucy-Ann McFadden et. al.. Encyclopedia of the Solar System. pp. 605–620.
^ ^a ^b Audrey Delsanti and David Jewitt (2006). "The Solar System Beyond The Planets" (PDF). Institute for Astronomy, University of Hawaii. Archived from the original on January 29, 2007. http://web.archive.org/web/20070129151907/http://www.ifa.hawaii.edu/faculty/jewitt/papers/2006/DJ06.pdf. Retrieved 2007-01-03.
^ Brown, M. E. et al (2006). "Satellites of the Largest Kuiper Belt Objects" (PDF). The Astrophysical Journal 639: L43. arXiv:astro-ph/0510029. Bibcode 2006ApJ...639L..43B. doi:10.1086/501524. http://web.gps.caltech.edu/~mbrown/papers/ps/gab.pdf. Retrieved 2011-10-19. edit
^ Chiang et al.; Jordan, A. B.; Millis, R. L.; Buie, M. W.; Wasserman, L. H.; Elliot, J. L.; Kern, S. D.; Trilling, D. E. et al (2003). "Resonance Occupation in the Kuiper Belt: Case Examples of the 5:2 and Trojan Resonances". The Astronomical Journal 126 (1): 430–443. Bibcode 2003AJ....126..430C. doi:10.1086/375207. http://www.boulder.swri.edu/~buie/biblio/pub047.pdf. Retrieved 2009-08-15.
^ M. W. Buie, R. L. Millis, L. H. Wasserman, J. L. Elliot, S. D. Kern, K. B. Clancy, E. I. Chiang, A. B. Jordan, K. J. Meech, R. M. Wagner, D. E. Trilling (2005). "Procedures, Resources and Selected Results of the Deep Ecliptic Survey". Earth, Moon, and Planets 92 (1): 113. arXiv:astro-ph/0309251. Bibcode 2003EM&P...92..113B. doi:10.1023/B:MOON.0000031930.13823.be.
^ E. Dotto1, M. A. Barucci2, and M. Fulchignoni (2006-08-24). "Beyond Neptune, the new frontier of the Solar System" (PDF). http://sait.oat.ts.astro.it/MSAIS/3/PDF/20.pdf. Retrieved 2006-12-26.
^ Fajans, J.; L. Frièdland (October 2001). "Autoresonant (nonstationary) excitation of pendulums, Plutinos, plasmas, and other nonlinear oscillators". American Journal of Physics 69 (10): 1096–1102. doi:10.1119/1.1389278. http://ist-socrates.berkeley.edu/~fajans/pub/pdffiles/AutoPendAJP.pdf. Retrieved 2006-12-26.
^ ^a ^b "Dwarf Planets and their Systems". Working Group for Planetary System Nomenclature (WGPSN). U.S. Geological Survey. 2008-11-07. http://planetarynames.wr.usgs.gov/append7.html#DwarfPlanets. Retrieved 2008-07-13.
^ Marc W. Buie (2008-04-05). "Orbit Fit and Astrometric record for 136472". SwRI (Space Science Department). http://www.boulder.swri.edu/~buie/kbo/astrom/136472.html. Retrieved 2008-07-13.
^ David Jewitt (2005). "The 1000 km Scale KBOs". University of Hawaii. http://www2.ess.ucla.edu/~jewitt/kb/big_kbo.html. Retrieved 2006-07-16.
^ "List Of Centaurs and Scattered-Disk Objects". IAU: Minor Planet Center. http://www.minorplanetcenter.org/iau/lists/Centaurs.html. Retrieved 2007-04-02.
^ Brown, M. E.; Schaller, E. L. (15 June 2007). "The Mass of Dwarf Planet Eris". Science 316 (5831): 1585. Bibcode 2007Sci...316.1585B. doi:10.1126/science.1139415. PMID 17569855. edit
^ Littmann, Mark (2004). Planets Beyond: Discovering the Outer Solar System. Courier Dover Publications. pp. 162–163. ISBN 978-0-486-43602-9.
^ ^a ^b ^c Fahr, H. J.; Kausch, T.; Scherer, H.; Kausch; Scherer (2000). "A 5-fluid hydrodynamic approach to model the Solar System-interstellar medium interaction" (PDF). Astronomy & Astrophysics 357: 268. Bibcode 2000A&A...357..268F. http://aa.springer.de/papers/0357001/2300268.pdf. See Figures 1 and 2.
^ NASA/JPL (2009). "Cassini's Big Sky: The View from the Center of Our Solar System". http://www.jpl.nasa.gov/news/features.cfm?feature=2370&msource=F20091119&tr=y&auid=5615216. Retrieved 2009-12-20.
^ Stone, E. C.; Cummings, A. C.; McDonald, F. B.; Heikkila, B. C.; Lal, N.; Webber, W. R. (September 2005). "Voyager 1 explores the termination shock region and the heliosheath beyond". Science 309 (5743): 2017–20. Bibcode 2005Sci...309.2017S. doi:10.1126/science.1117684. PMID 16179468.
^ Stone, E. C.; Cummings, A. C.; McDonald, F. B.; Heikkila, B. C.; Lal, N.; Webber, W. R. (July 2008). "An asymmetric solar wind termination shock". Nature 454 (7200): 71–4. doi:10.1038/nature07022. PMID 18596802.
^ P. C. Frisch (University of Chicago) (June 24, 2002). "The Sun's Heliosphere & Heliopause". Astronomy Picture of the Day. http://antwrp.gsfc.nasa.gov/apod/ap020624.html. Retrieved 2006-06-23.
^ "Voyager: Interstellar Mission". NASA Jet Propulsion Laboratory. 2007. http://voyager.jpl.nasa.gov/mission/interstellar.html. Retrieved 2008-05-08.
^ R. L. McNutt, Jr. et al. (2006). "Innovative Interstellar Explorer". Physics of the Inner Heliosheath: Voyager Observations, Theory, and Future Prospects. AIP Conference Proceedings. 858. pp. 341–347. Bibcode 2006AIPC..858..341M. doi:10.1063/1.2359348.
^ Anderson, Mark (2007-01-05). "Interstellar space, and step on it!". New Scientist. http://space.newscientist.com/article/mg19325850.900-interstellar-space-and-step-on-it.html. Retrieved 2007-02-05.
^ Stern SA, Weissman PR. (2001). "Rapid collisional evolution of comets during the formation of the Oort cloud.". Space Studies Department, Southwest Research Institute, Boulder, Colorado. http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?cmd=Retrieve&db=PubMed&list_uids=11214311&dopt=Citation. Retrieved 2006-11-19.
^ Bill Arnett (2006). "The Kuiper Belt and the Oort Cloud". nineplanets.org. http://www.nineplanets.org/kboc.html. Retrieved 2006-06-23.
^ David Jewitt (2004). "Sedna – 2003 VB₁₂". University of Hawaii. http://www2.ess.ucla.edu/~jewitt/kb/sedna.html. Retrieved 2006-06-23.
^ Mike Brown. "Sedna". CalTech. http://www.gps.caltech.edu/~mbrown/sedna/. Retrieved 2007-05-02.
^ T. Encrenaz, JP. Bibring, M. Blanc, MA. Barucci, F. Roques, PH. Zarka (2004). The Solar System: Third edition. Springer. p. 1.
^ Durda D. D.; Stern S. A.; Colwell W. B.; Parker J. W.; Levison H. F.; Hassler D. M. (2004). "A New Observational Search for Vulcanoids in SOHO/LASCO Coronagraph Images". Icarus 148: 312–315. Bibcode 2000Icar..148..312D. doi:10.1006/icar.2000.6520.
^ English, J. (2000). "Exposing the Stuff Between the Stars" (Press release). Hubble News Desk. http://www.ras.ucalgary.ca/CGPS/press/aas00/pr/pr_14012000/pr_14012000map1.html. Retrieved 2007-05-10.
^ R. Drimmel, D. N. Spergel (2001). "Three Dimensional Structure of the Milky Way Disk". Astrophysical Journal 556: 181–202. arXiv:astro-ph/0101259. Bibcode 2001ApJ...556..181D. doi:10.1086/321556.
^ Eisenhauer, F.; et al. (2003). "A Geometric Determination of the Distance to the Galactic Center". Astrophysical Journal 597 (2): L121–L124. Bibcode 2003ApJ...597L.121E. doi:10.1086/380188.
^ Leong, Stacy (2002). "Period of the Sun's Orbit around the Galaxy (Cosmic Year)". The Physics Factbook. http://hypertextbook.com/facts/2002/StacyLeong.shtml. Retrieved 2007-04-02.
^ C. Barbieri (2003). "Elementi di Astronomia e Astrofisica per il Corso di Ingegneria Aerospaziale V settimana". IdealStars.com. http://dipastro.pd.astro.it/planets/barbieri/Lezioni-AstroAstrofIng04_05-Prima-Settimana.ppt. Retrieved 2007-02-12.
^ ^a ^b Leslie Mullen (2001). "Galactic Habitable Zones". Astrobiology Magazine. http://www.astrobio.net/news/modules.php?op=modload&name=News&file=article&sid=139. Retrieved 2006-06-23.
^ "Supernova Explosion May Have Caused Mammoth Extinction". Physorg.com. 2005. http://www.physorg.com/news6734.html. Retrieved 2007-02-02.
^ "Near-Earth Supernovas". NASA. http://science.nasa.gov/headlines/y2003/06jan_bubble.htm. Retrieved 2006-07-23.
^ "Stars within 10 light years". SolStation. http://www.solstation.com/stars/s10ly.htm. Retrieved 2007-04-02.
^ "Tau Ceti". SolStation. http://www.solstation.com/stars/tau-ceti.htm. Retrieved 2007-04-02.
^ "HUBBLE ZEROES IN ON NEAREST KNOWN EXOPLANET". Hubblesite. 2006. http://hubblesite.org/newscenter/archive/releases/2006/32/text/. Retrieved 2008-01-13.
^ The date is based on the oldest inclusions found to date in meteorites, and is thought to be the date of the formation of the first solid material in the collapsing nebula.
A. Bouvier and M. Wadhwa. "The age of the solar system redefined by the oldest Pb-Pb age of a meteoritic inclusion." Nature Geoscience, in press, 2010. doi:10.1038/NGEO941
^ ^a ^b ^c "Lecture 13: The Nebular Theory of the origin of the Solar System". University of Arizona. http://atropos.as.arizona.edu/aiz/teaching/nats102/mario/solar_system.html. Retrieved 2006-12-27.
^ Irvine, W. M. (1983). "The chemical composition of the pre-solar nebula". Cometary exploration; Proceedings of the International Conference. 1. pp. 3. Bibcode 1983coex....1....3I.
^ Greaves, Jane S. (2005-01-07). "Disks Around Stars and the Growth of Planetary Systems". Science 307 (5706): 68–71. Bibcode 2005Sci...307...68G. doi:10.1126/science.1101979. PMID 15637266.
^ "Present Understanding of the Origin of Planetary Systems". National Academy of Sciences. 2000-04-05. http://www.nap.edu/openbook.php?record_id=1732&page=21. Retrieved 2007-01-19.
^ Boss, A. P.; Durisen, R. H. (2005). "Chondrule-forming Shock Fronts in the Solar Nebula: A Possible Unified Scenario for Planet and Chondrite Formation". The Astrophysical Journal 621 (2): L137. Bibcode 2005ApJ...621L.137B. doi:10.1086/429160.
^ Sukyoung Yi; Pierre Demarque; Yong-Cheol Kim; Young-Wook Lee; Chang H. Ree; Thibault Lejeune; Sydney Barnes (2001). "Toward Better Age Estimates for Stellar Populations: The $Y^{2}$ Isochrones for Solar Mixture". Astrophysical Journal Supplement 136: 417. arXiv:astro-ph/0104292. Bibcode 2001ApJS..136..417Y. doi:10.1086/321795.
^ A. Chrysostomou, P. W. Lucas (2005). "The Formation of Stars". Contemporary Physics 46 (1): 29. Bibcode 2005ConPh..46...29C. doi:10.1080/0010751042000275277.
^ K. P. Schroder, Robert Cannon Smith (2008). "Distant future of the Sun and Earth revisited". Monthly Notices of the Royal Astronomical Society 386 (1): 155–163. Bibcode 2008MNRAS.386..155S. doi:10.1111/j.1365-2966.2008.13022.x.
^ Pogge, Richard W. (1997). "The Once & Future Sun" (lecture notes). New Vistas in Astronomy. Archived from the original on May 27, 2005. http://web.archive.org/web/20050527094435/http://www-astronomy.mps.ohio-state.edu/Vistas/. Retrieved 2005-12-07.
^ Alessandro Morbidelli (2005). "Origin and dynamical evolution of comets and their reservoirs". arXiv:astro-ph/0512256.
^ ^a ^b ^c "The Final IAU Resolution on the definition of "planet" ready for voting". IAU. 2006-08-24. http://www.iau.org/iau0602.423.0.html. Retrieved 2007-03-02.
^ Ron Ekers. "IAU Planet Definition Committee". International Astronomical Union. http://www.iau.org/public_press/news/release/iau0601/newspaper/. Retrieved 2008-10-13.
^ "Plutoid chosen as name for Solar System objects like Pluto". International Astronomical Union. June 11, 2008, Paris. http://www.iau.org/public_press/news/release/iau0804. Retrieved 2008-06-11.
^ Reid, M.J.; Brunthaler, A. (2004 2004). "The Proper Motion of Sagittarius A*". The Astrophysical Journal 616 (2): 883. Bibcode 2004ApJ...616..872R. doi:10.1086/424960.

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The Solar System

Sun
•
Heliosphere

Planets	Mercury Venus Earth Moon Mars Moons of Mars Jupiter Moons of Jupiter Rings of Jupiter Saturn Moons of Saturn Rings of Saturn Uranus Moons of Uranus Rings of Uranus Neptune Moons of Neptune Rings of Neptune

Dwarf planets	Ceres Pluto Moons of Pluto Haumea Moons of Haumea Makemake Eris Dysnomia (moon)

Small
Solar
System
Bodies

Asteroids
(minor planets)

Groups and families	Vulcanoids Near-Earth asteroids Asteroid belt Jupiter Trojans Centaurs Neptune trojans Asteroid moons Meteoroids Pallas Juno Vesta Hygiea

See also: the list of asteroids and the meaning and pronunciation of asteroid names.

Trans-
Neptunians

Kuiper belt

Plutinos	Orcus Ixion

Cubewanos	2002 UX₂₅ Varuna 1992 QB₁ 2002 TX₃₀₀ Quaoar Huya 2002 AW₁₉₇

Scattered disc

Comets

Lists of periodic and non-periodic comets
Damocloids
Hills cloud
Oort cloud

See also: Geology of solar terrestrial planets, astronomical objects, the solar system's list of objects, sorted by radius or mass, and the Solar System Portal

Star systems within 0–5 light-years →

Star systems (including brown dwarf systems) within 0–5 light-years from Earth.

G V (Yellow)	Solar System (0 ly; 1 star, 8 planets) • Alpha Centauri (4.365 ± 0.007 ly; 3 stars: Alpha¹ Centauri • Alpha² Centauri • Proxima Centauri (4.242 ± 0.002 ly))

In left column are stellar classes of primary members of star systems. ‡Distance error margin extends out of declared distance interval. Bold are systems containing at least one component with absolute magnitude of +8.5 or brighter. Italic are systems possibly located within declared distance interval, but probably not.

Nearest star systems

Star systems (including brown dwarf systems) within 10 light-years from Earth.

0–5 ly →

G V (Yellow)	Solar System (0 ly; 1 star, 8 planets) • Alpha Centauri (4.365 ± 0.007 ly; 3 stars: Alpha¹ Centauri • Alpha² Centauri • Proxima Centauri (4.242 ± 0.002 ly))

← 5–10 ly →

A V (White)	Sirius (8.58 ± 0.03 ly; 2 stars)

M V (Red dwarf)	Barnard's Star (5.979 ± 0.003 ly; 1 star) • Wolf 359 (7.78 ± 0.04 ly; 1 star) • Lalande 21185 (8.29 ± 0.01 ly; 1 star) • BL/UV Ceti (8.73 ± 0.06 ly; 2 stars) • Ross 154 (9.67 ± 0.06 ly; 1 star)

Nearest bright star systems

Star systems within 30 light-years from Earth with brightest member's absolute magnitude of +8.5 or brighter.

0–10 ly →

A V (White)	Sirius (8.58 ± 0.03 ly; 2 stars)

G V (Yellow)	Solar System (0 ly; 1 star, 8 planets) • Alpha Centauri (4.365 ± 0.007 ly; 3 stars: Alpha¹ Centauri • Alpha² Centauri • Proxima Centauri (4.242 ± 0.002 ly))

← 10–20 ly →

A V (White)	Altair (16.69 ± 0.04 ly; 1 star)

F V (Yellow-white)	Procyon (11.44 ± 0.02 ly; 2 stars)

G V (Yellow)	Tau Ceti (11.905 ± 0.007 ly; 1 star) • Sigma Draconis «Alsafi» (18.77 ± 0.02 ly; 1 star) • Eta Cassiopeiae «Achird» (19.39 ± 0.05 ly; 2 stars) • e (82 G.) Eridani (19.71 ± 0.02 ly; 1 star, 3 planets: planet b • planet c • planet d) • Delta Pavonis (19.92 ± 0.02 ly; 1 star)

K V
(Orange)

Epsilon Eridani (10.480 ± 0.003 ly; 1 star, 2 planets: planet b • planet c) • 61 Cygni (11.40 ± 0.02 ly; 2 stars) • Epsilon Indi (11.81 ± 0.01 ly; 1 star, 2 brown dwarfs) • Groombridge 1618 (15.87 ± 0.04 ly; 1 star) • Omicron² (40) Eridani «Keid» (16.25 ± 0.02 ly; 3 stars) • 70 Ophiuchi (16.64 ± 0.07 ly; 2 stars) • 33 G. Librae (19.12 ± 0.08 ly; 3 stars, 1 brown dwarf) • 36 Ophiuchi (19.40 ± 0.05 ly; 3 stars) • Gliese 783 (19.62 ± 0.04 ly; 2 stars)

← 20–30 ly →

A V (White)	Fomalhaut (25.1 ± 0.2 ly; 1 star, 1 planet: planet b) • Vega (25.30 ± 0.11 ly; 1 star)

F V (Yellow-white)	Pi³ Orionis «Tabit» (26.2 ± 0.2 ly; 1 star) • Chi Draconis (26.22 ± 0.11 ly; 2 stars) • Zeta Tucanae (28.0 ± 0.2 ly; 1 star) • Gamma Leporis (29.3 ± 0.2 ly; 2 stars) • Gamma Pavonis (30.1* ± 0.2 ly; 1 star)‡*

G
(Yellow)

IV	Beta Hydri (24.4 ± 0.1 ly; 1 star) • Mu Herculis (27.4 ± 0.2 ly; 3 stars)

V	Xi Boötis (22.1 ± 0.2 ly; 2 stars) • Xi Ursae Majoris «Alula Australis» (27.25 ± 0.18 ly; 3 stars, 1 brown dwarf) • Beta Canum Venaticorum «Chara» (27.3 ± 0.2 ly; 1 star) • 61 Virginis (27.8 ± 0.2 ly; 1 star, 3 planets: planet b • planet c • planet d) • Chi¹ Orionis (28.3 ± 0.3 ly; 2 stars) • 41 G. Arae (28.7 ± 0.3 ly; 2 stars) • Beta Comae Berenices (29.9 ± 0.2 ly; 1 star)‡ • Kappa¹ Ceti (29.9 ± 0.2 ly; 1 star)‡ • HR 4523 (30.1* ± 0.2 ly; 2 stars, 1 planet: planet b)‡*

VI	Mu Cassiopeiae «Marfak-West» (24.6 ± 0.2 ly; 2 stars) • Groombridge 1830 (29.9 ± 0.2 ly; 1 star)‡

K
(Orange)

IV	Delta Eridani «Rana» (29.5 ± 0.3 ly; 1 star)

V	Gliese 892 (21.34 ± 0.04 ly; 1 star) • HR 753 (23.5 ± 0.2 ly; 3 stars) • Gliese 667 (23.6 ± 0.1 ly; 3 stars, 2 (3?) planets: planet Cb • planet Cc • planet Cd?) • Gliese 33 (24.3 ± 0.2 ly; 1 star) • 107 Piscium (24.4 ± 0.2 ly; 1 star) • TW Piscis Austrini (24.9 ± 0.2 ly; 1 star) • Gliese 673 (25.2 ± 0.2 ly; 1 star) • Gliese 884 (26.6 ± 0.3 ly; 1 star) • p Eridani (26.6 ± 0.3 ly; 2 stars) • Gliese 250 (28.4 ± 0.3 ly; 2 stars) • HR 1614 (28.8 ± 0.3 ly; 1 star) • HR 7722 (28.8 ± 0.3 ly; 1 star, 2 planets: planet b • planet c)

In left column are stellar classes of primary members of star systems. ‡Distance error margin extends out of declared distance interval. Italic are systems possibly located within declared distance interval, but likely not. Total about 50 (47–52) systems.

v t e Earth's location in the universe

Earth → Solar System → Local Interstellar Cloud → Local Bubble → Gould Belt → Orion–Cygnus Arm → Milky Way → Milky Way subgroup → Local Group → Virgo Supercluster → Pisces-Cetus Supercluster Complex → Observable universe → Universe

Each arrow should be read as "within" or "part of".

v t e Systems and systems science

Systems categories	Systems theory Systems science Systems scientists Conceptual Physical Social

Systems	Biological Complex Complex adaptive Conceptual Database management Dynamical Economical Ecosystem Formal Global Positioning System Human anatomy Information systems Legal systems of the world Systems of measurement Metric system Multi-agent system Nervous system Nonlinearity Operating system Physical system Political system Sensory system Social system Solar System Systems art

Theoretical fields	Chaos theory Complex systems Control theory Cybernetics Living systems Sociotechnical systems theory Systems biology System dynamics Systems ecology Systems engineering Systems neuroscience Systems psychology Systems science Systems theory World-systems theory

Systems scientists	Russell L. Ackoff William Ross Ashby Béla H. Bánáthy Gregory Bateson Richard E. Bellman Stafford Beer Ludwig von Bertalanffy Murray Bowen Kenneth E. Boulding C. West Churchman George Dantzig Heinz von Foerster Jay Wright Forrester Charles A S Hall George Klir Edward Lorenz Niklas Luhmann Humberto Maturana Margaret Mead Donella Meadows Mihajlo D. Mesarovic James Grier Miller Howard T. Odum Talcott Parsons Ilya Prigogine Anatol Rapoport Claude Shannon Qian Xuesen Francisco Varela Kevin Warwick Norbert Wiener Anthony Wilden

This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)

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Name	Orbits (Designation)	Distance 000 mi. / 000 km.	Radius mi. / km.	Rotate (days)	Period (days)	Discoverer	Date
Sun	—	—	431,520/696,000	25.4	—	Known in antiquity
Mercury	Sun (I)	36,000 / 57,910	1,600 / 2,440	58.7	87.97	Known in antiquity
Venus	Sun (II)	67,000 / 108,200	3,350 / 6,052	243*	224.70	Known in antiquity
Earth	Sun (III)	93,000 / 149,600	3,960 / 6,378	0.99	365.26	Known in antiquity
Mars	Sun (IV)	141,000 / 227,940	2,100 / 3,397	1.03	686.98	Known in antiquity
Jupiter	Sun (V)	483,000 / 778,570	44,320 / 71,492	0.41	4,331.59	Known in antiquity
Saturn	Sun (VI)	886,000 / 1,433,525	37,250 / 60,268	0.45	10,747	Known in antiquity
Uranus	Sun (VII)	1,782,000 / 2,872,450	16,000 / 25,559	0.72*	30,589	Herschel	1781
Neptune	Sun (VIII)	2,793,000 / 4,495,100	15,500 / 24,764	0.67	59,800	Adams, LeVerrier, Galle, and d’Arrest	1846
Pluto	Sun (IX)	3,670,000 / 5,869,660	750 / 1,195	6.39*	90,588	Tombaugh	1930

Planet (No. of Satellites)	Satellite Name	Distance 000 mi. / 000 km.	Radius mi. / km.	Period (days)	Discoverer	Date
Earth (1)	Moon	238 / 384	1,077 / 1,737	27.32	Known in antiquity
Mars (2)	Phobos	6 / 9	8x7x6 / 13x11x9	0.32	Hall	1877
	Deimos	14 / 23	5x4x3 / 8x6x5	1.26	Hall	1877
Jupiter (16)	Metis	79 / 128	12 / 20	0.29	Synnott**	1979
	Adrastea	80 / 129	8x6x5 / 13x10x8	0.30	Jewitt, Danielson	1979
	Amalthea	112 / 181	81x45x42 / 131x73x67	0.50	Barnard	1892
	Thebe	138 / 222	34x28 / 55x45	0.67	Synnott***	1979
	Io	262 / 422	1,129 / 1*821	1.77	Galileo	1610
	Europa	416 / 671	970 /1,565	3-55	Galileo	1610
	Ganymede	663 / 1,070	1,633/2,634	7.15	Galileo	1610
	Callista	1,167 / 1,883	1,490 / 2,403	16.69	Galileo	1610
	Leda	6,878 / 11,094	3/5	238.72	Kowal	1974
	Himalia	7,118 / 11,480	58/85	250.57	Perrine	1904
	Lysithea	7,266 / 11,720	7/12	259.22	Nicholson	1938
	Elara	7,277 / 11,737	25/40	259.65	Perrine	1905
	Ananke	13,144 / 21,200	6/10	631*	Nicholson	1951
	Carme	14,012 / 22,600	9/15	692*	Nicholson	1938
	Pasiphae	14,570/23,500	11/18	735*	Melotte	1908
	Sinope	14,694 / 23,700	9/14	758*	Nicholson	1914
Saturn (18)	Pan	83 / ^:34	6/10	0.58	Showaiter**	1990
	Atlas	86 / 138	12x11x9 / 19x17x14	0.60	Terrile***	1980
	Prometheus	86 / 139	46x31x21 / 74x50x34	0.61	Collins***	1980
	Pandora	88 / 142	34x27x19 / 55x44x31	0.63	Collins***	1980
	Epimetheus	94 / 151	43x34x34 / 69x55x55	0.69	Fountain, Larson, Reitsema, Smith***	1980
	Janus	94 / 151	60x59x48 / 97x95x77	0.69	Dollfus	1966
	Mimas	115 / 186	130x122x118 / 209x196x191	0.94	Herschel	1789
	Enceladus	148 / 238	159x153x152 / 256x247x245	1.37	Herschel	1789
	Tethys	183 / 295	332x327x326 / 536x528x526	1.89	Cassini	1684
	Telesto	183 / 295	9x8x5 / 15x13x8	1.89	Fountain, Larson, Reitsema, Smith***	1980
	Calypso	183 / 295	9x5x5 / 15x8x8	1.89	Pascu, Seidelman, Baum, Currie	1980
	Dione	234 / 377	347 / 560	2.74	Cassini	1684
	Helene	234 / 377	11x10x9 / 18x16x15	2.74	Laques, Lecacheux	1980
	Rhea	327 / 527	474 / 764	4.52	Cassini	1672
	Titan	758 / 1,222	1-597/2,575	15.95	Huygens	1655
	Hyperion	918 / 1,481	115x87x70 / 185x140x113	21.28	Bond, Lassell	1848
	Iapetus	2,208 / 3,561	445 / 718	79.33	Cassini	1671
	Phoebe	8,030 / 12,952	71x68x65 / 115x110x105	550.48*	Pickering	1898
Uranus (17)	Cordelia	31/50	8/13	0.34	Terrile**	1986
	Ophelia	33/54	9/15	0.38	Terrile**	1986
	Bianca	37/59	13/21	0.43	Voyager 2 photos	1986
	Cressida	38/62	19/31	0.46	Synnott**	1986
	Desdemons	39/63	17/27	0.47	Synnott**	1986
	Juliet	40 / 64	26 / 42	0.49	Synnott**	1986
	Portia	41 / 66	33/54	0.51	Synnott**	1986
	Rosalind	43/70	17/27	0.56	Synnott**	1986
	Belinda	47/75	20/33	0.62	Synnott**	1986
	Puck	53/86	48/77	0.76	Synnott**	1985
	Miranda	80 / 129	149x145x144/240x234x233	1.41	Kuiper	1948
	Ariel	118 / 191	360x358x358 / 581x578x578	2.52	Lassell	1851
	Umbriel	165/266	363/585		4.14	Lassell	1851
	Titania	270 / 436	489/789	8.71	Herschel	1787
	Oberon	362 / 584	472 / 761	13.46	Herschel	1787
	Caliban	4,445/7,169	19/30	579.38*	Gladman, Nicholson, Burns, Kavelaars	1997
	Sycorax	7,549 / 12,175	37/60	1289*	Gladman, Nicholson, Burns, Kavelaars	1997
Neptune (8)	Naiad	30/48	18/29	0.29	Terrile**	1989
	Thalassa	31/50	25/40	0.31	Terrile**	1989
	Despina	33/53	46/74	0.33	Synnott**	1989
	Galatea	38/62	49/79	0.43	Synnott**	1989
	Larissa	46/74	65x55x56 /104x89x90	0.55	Reitsema, Tholen, Hubbard, Lebofsky**	1989
	Proteus	73 /118	135x129x125 / 218x208x201	1.12	Synnott**	1989
	Triton	220 / 355	839 /1.353	5.88*	Lassell	1846
	Nereid	3.418 / 5,513	105 / 170	360.14	Kuiper	1949
Pluto (i)	Charon	12/20	368/593	6.39	Christy	1978

		American Heritage Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2009. Published by Houghton Mifflin Company. All rights reserved. Read more
		Wiley Book of Astronomy. Copyright © 2004 by Wiley-Blackwell. Wiley and the Wiley logo are registered trademarks of John Wiley & Sons, Inc. and/or its affiliates in the United States and other countries. Used here by license. Read more
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		McGraw-Hill Science & Technology Encyclopedia. McGraw-Hill Encyclopedia of Science and Technology. Copyright © 2005 by The McGraw-Hill Companies, Inc. All rights reserved. Read more
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		Gale Encyclopedia of Occultism & Parapsychology. Encyclopedia of Occultism and Parapsychology. Copyright © 2001 by The Gale Group, Inc. All rights reserved. Read more
		Cosmic Lexicon. Copyright 1996 Planetary Science Research Discoveries. Read more
		Dictionary of Cultural Literacy: Science. The New Dictionary of Cultural Literacy, Third Edition Edited by E.D. Hirsch, Jr., Joseph F. Kett, and James Trefil. Copyright © 2002 by Houghton Mifflin Company. Published by Houghton Mifflin. All rights reserved. Read more
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		Wikipedia on Answers.com. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article Solar System. Read more
		Oxford Essential Desk Reference. The Essenial Desk Reference Dictionary. Copyright © 2002 by Oxford University Press, Inc.. All rights reserved. Read more

	Book: Solar System
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Solar System

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Astronomy: The Solar System