Solar System

Page semi-protected
Listen to this article
Source: Wikipedia, the free encyclopedia.

Solar System
Orion–Cygnus Arm
  • Milky Way[2]
  • Nearest star
    Population
    StarsSun
    Planets
    Known dwarf planets
    Known
    million years[10]

    The Solar System

    fusion of hydrogen into helium inside the Sun's core releases energy, which is primarily emitted through its outer photosphere. This creates a decreasing temperature gradient
    across the system. Over 99.86% of the Solar System's mass is located within the Sun.

    The most massive objects that orbit the Sun are the eight planets. Closest to the Sun in order of increasing distance are the four terrestrial planetsMercury, Venus, Earth and Mars. Only the Earth and Mars orbit within the Sun's habitable zone, where liquid water can exist on the surface. Beyond the frost line at about five astronomical units (AU),[e] are two gas giantsJupiter and Saturn – and two ice giantsUranus and Neptune. Jupiter and Saturn possess nearly 90% of the non-stellar mass of the Solar System.

    There are a vast number of less massive objects. There is a strong consensus among astronomers that the Solar System has at least nine

    centaurs, meteoroids, and interplanetary dust clouds. Some of these bodies are in the asteroid belt (between Mars's and Jupiter's orbit) and the Kuiper belt (just outside Neptune's orbit).[g]

    Between the bodies of the Solar System is an

    Local Cloud. The closest star to the Solar System, Proxima Centauri, is 4.25 light-years (269,000 AU) away. Both are within the Local Bubble, a relatively small 1,000 light-years wide region of the Milky Way
    .

    Definition

    The Solar System includes the Sun and all objects that are bound to it by gravity and orbit it.[14][15][16]

    The International Astronomical Union describes the Solar System as all objects that are bound by the gravity of the Sun, the Sun itself, its eight planets, and the other celestial bodies which orbit it.[11] NASA describes the Solar System as a planetary system, including the Sun and all objects that orbit it.[12]

    When not used as a proper noun and written without capitalization, "solar system" may refer to either the Solar System itself or any system reminiscent of the Solar System.[14]

    Formation and evolution

    Past

    Diagram of the early Solar System's protoplanetary disk, out of which Earth and other Solar System bodies formed

    The Solar System formed at least 4.568 billion years ago from the gravitational collapse of a region within a large molecular cloud.[b] This initial cloud was likely several light-years across and probably birthed several stars.[18] As is typical of molecular clouds, this one consisted mostly of hydrogen, with some helium, and small amounts of heavier elements fused by previous generations of stars.[19]

    As the

    protoplanetary disc with a diameter of roughly 200 AU[18][20] and a hot, dense protostar at the center.[21][22] The planets formed by accretion from this disc,[23] in which dust and gas gravitationally attracted each other, coalescing to form ever larger bodies. Hundreds of protoplanets may have existed in the early Solar System, but they either merged or were destroyed or ejected, leaving the planets, dwarf planets, and leftover minor bodies.[24][25]

    Due to their higher boiling points, only metals and silicates could exist in solid form in the warm inner Solar System close to the Sun (within the frost line). They eventually formed the rocky planets of Mercury, Venus, Earth, and Mars. Because these refractory materials only comprised a small fraction of the solar nebula, the terrestrial planets could not grow very large.[24]

    The giant planets (Jupiter, Saturn, Uranus, and Neptune) formed further out, beyond the frost line, the point between the orbits of Mars and Jupiter where material is cool enough for volatile icy compounds to remain solid. The ices that formed these planets were more plentiful than the metals and silicates that formed the terrestrial inner planets, allowing them to grow massive enough to capture large atmospheres of hydrogen and helium, the lightest and most abundant elements.[24] Leftover debris that never became planets congregated in regions such as the asteroid belt, Kuiper belt, and Oort cloud.[24]

    Within 50 million years, the pressure and density of hydrogen in the center of the protostar became great enough for it to begin

    reaction rate, pressure, and density increased until hydrostatic equilibrium was achieved: the thermal pressure counterbalancing the force of gravity. At this point, the Sun became a main-sequence star.[29] Solar wind from the Sun created the heliosphere and swept away the remaining gas and dust from the protoplanetary disc into interstellar space.[27]

    Following the dissipation of the protoplanetary disk, the Nice model proposes that gravitational encounters between planetisimals and the gas giants caused each to migrate into different orbits. This led to dynamical instability of the entire system, which scattered the planetisimals and ultimately placed the gas giants in their current positions. During this period, the grand tack hypothesis suggests that a final inward migration of Jupiter dispersed much of the asteroid belt, leading to the Late Heavy Bombardment of the inner planets.[30][31]

    Present and future

    The Solar System remains in a relatively stable, slowly evolving state by following isolated,

    chaotic, and may eventually be disrupted. There is a small chance that another star will pass through the Solar System in the next few billion years. Although this could destabilize the system and eventually lead millions of years later to expulsion of planets, collisions of planets, or planets hitting the Sun, it would most likely leave the Solar System much as it is today.[33]

    The current Sun compared to its peak size in the red-giant phase

    The Sun's main-sequence phase, from beginning to end, will last about 10 billion years for the Sun compared to around two billion years for all other subsequent phases of the Sun's pre-

    remnant life combined.[34] The Solar System will remain roughly as it is known today until the hydrogen in the core of the Sun has been entirely converted to helium, which will occur roughly 5 billion years from now. This will mark the end of the Sun's main-sequence life. At that time, the core of the Sun will contract with hydrogen fusion occurring along a shell surrounding the inert helium, and the energy output will be greater than at present. The outer layers of the Sun will expand to roughly 260 times its current diameter, and the Sun will become a red giant. Because of its increased surface area, the surface of the Sun will be cooler (2,600 K (4,220 °F) at its coolest) than it is on the main sequence.[34]

    The expanding Sun is expected to vaporize Mercury as well as Venus, and render Earth and Mars uninhabitable (possibly destroying Earth as well).[35][36] Eventually, the core will be hot enough for helium fusion; 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 the fusion of heavier elements, and nuclear reactions in the core will dwindle. Its outer layers will be ejected into space, leaving behind a dense white dwarf, half the original mass of the Sun but only the size of Earth.[34] The ejected outer layers may form a planetary nebula, returning some of the material that formed the Sun – but now enriched with heavier elements like carbon – to the interstellar medium.[37][38]

    General characteristics

    Astronomers sometimes divide the Solar System structure into separate regions. The

    outer Solar System includes Jupiter, Saturn, Uranus, Neptune, and the bodies in the Kuiper belt.[39] 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.[40]

    Composition

    The principal component of the Solar System is the Sun, a G-type main-sequence star that contains 99.86% of the system's known mass and dominates it gravitationally.[41] The Sun's four largest orbiting bodies, the giant planets, account for 99% of the remaining mass, with Jupiter and Saturn together comprising more than 90%. The remaining objects of the Solar System (including the four terrestrial planets, the dwarf planets, moons, asteroids, and comets) together comprise less than 0.002% of the Solar System's total mass.[h]

    The Sun is composed of roughly 98% hydrogen and helium,

    light pressure from the early 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.[48] The boundary in the Solar System beyond which those volatile substances could coalesce is known as the frost line, and it lies at roughly five times the Earth's distance from the Sun.[5]

    Orbits

    inner planets
    orbiting. Each frame represents 2 days of motion.
    outer planets
    orbiting. This animation is 100 times faster than the inner planet animation.

    The planets and other large objects in orbit around the Sun lie near the

    synchronous rotation, with one face permanently turned toward their parent. The four giant planets have planetary rings, thin discs of tiny particles that orbit them in unison.[52]

    As a result of the formation of the Solar System, planets and most other objects orbit the Sun in the same direction that the Sun is rotating. That is, counter-clockwise, as viewed from above Earth's north pole.[53] There are exceptions, such as Halley's Comet.[54] Most of the larger moons orbit their planets in prograde direction, matching the direction of planetary rotation; Neptune's moon Triton is the largest to orbit in the opposite, retrograde manner.[55] Most larger objects rotate around their own axes in the prograde direction relative to their orbit, though the rotation of Venus is retrograde.[56]

    To a good first approximation,

    aphelion.[58]: 9-6  With the exception of Mercury, the orbits of the planets are nearly circular, but many comets, asteroids, and Kuiper belt objects follow highly elliptical orbits. Kepler's laws only account for the influence of the Sun's gravity upon an orbiting body, not the gravitational pulls of different bodies upon each other. On a human time scale, these perturbations can be accounted for using numerical models,[58]: 9-6  but the planetary system can change chaotically over billions of years.[59]

    The

    rotational momentum possessed by all its moving components.[60] Although the Sun dominates the system by mass, it accounts for only about 2% of the angular momentum.[61][62] The planets, dominated by Jupiter, account for most of the rest of the angular momentum due to the combination of their mass, orbit, and distance from the Sun, with a possibly significant contribution from comets.[61]

    Distances and scales

    Relative orbital distances in the Solar System visualized as a condensed rectangle

    The radius of the Sun is 0.0047 AU (700,000 km; 400,000 mi).[63] Thus, the Sun occupies 0.00001% (1 part in 107) of the volume of a sphere with a radius the size of Earth's orbit, whereas Earth's volume is roughly 1 millionth (10−6) that of the Sun. Jupiter, the largest planet, is 5.2 AU from the Sun and has a radius of 71,000 km (0.00047 AU; 44,000 mi), whereas the most distant planet, Neptune, is 30 AU from the Sun.[47][64]

    With a few exceptions, the farther a planet or belt is from the Sun, the larger the distance between its orbit and the orbit of the next nearest object to the Sun. For example, Venus is approximately 0.33 AU farther out from the Sun than Mercury, whereas 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, like the Titius–Bode law[65] and Johannes Kepler's model based on the Platonic solids,[66] but ongoing discoveries have invalidated these hypotheses.[67]

    Some

    Sedna, is a 10 cm (4 in) sphere in Luleå, 912 km (567 mi) away.[69][70]
    At that scale, the distance to Proxima Centauri would be roughly 8 times further than the Moon is from Earth.

    If the Sun–Neptune distance is scaled to 100 metres (330 ft), then the Sun would be about 3 cm (1.2 in) in diameter (roughly two-thirds the diameter of a golf ball), the giant planets would be all smaller than about 3 mm (0.12 in), and

    Earth's diameter along with that of the other terrestrial planets would be smaller than a flea (0.3 mm or 0.012 in) at this scale.[71]

    Comparison of the distances between planets, with the white bar showing orbital variations. The size of the planets is not to scale.

    Habitability

    orange dwarf (K-type main-sequence star), a typical red dwarf, and an ultra-cool dwarf
    .

    Besides solar energy, the primary characteristic of the Solar System enabling the presence of life is the heliosphere and planetary magnetic fields (for those planets that have them). These magnetic fields partially shield the Solar System from high-energy interstellar particles called cosmic rays. 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-ray penetration in the Solar System varies, though by how much is unknown.[72]

    The

    subsurface oceans of various outer Solar System moons.[74]

    Comparison with extrasolar systems

    Compared to many extrasolar systems, the Solar System stands out in lacking planets interior to the orbit of Mercury.[75][76] The known Solar System lacks super-Earths, planets between one and ten times as massive as the Earth,[75] although the hypothetical Planet Nine, if it does exist, could be a super-Earth orbiting in the edge of the Solar System.[77]

    Uncommonly, it has only small terrestrial and large gas giants; elsewhere planets of intermediate size are typical – both rocky and gas – so there is no "gap" as seen between the size of Earth and of Neptune (with a radius 3.8 times as large). As many of these super-Earths are closer to their respective stars than Mercury is to the Sun, a hypothesis has arisen that all planetary systems start with many close-in planets, and that typically a sequence of their collisions causes consolidation of mass into few larger planets, but in case of the Solar System the collisions caused their destruction and ejection.[75][78]

    The orbits of Solar System planets are nearly circular. Compared to many other systems, they have smaller orbital eccentricity.[75] Although there are attempts to explain it partly with a bias in the radial-velocity detection method and partly with long interactions of a quite high number of planets, the exact causes remain undetermined.[75][79]

    Sun

    White ball of plasma
    The Sun in true white color

    The Sun is the Solar System's star and by far its most massive component. Its large mass (332,900

    visible light.[83][84]

    Because the Sun fuses hydrogen at its core, it is a main-sequence star. More specifically, it is a G2-type main-sequence star, where the type designation refers to its effective temperature. Hotter main-sequence stars are more luminous but shorter lived. The Sun's temperature is intermediate between that of the hottest stars and that of the coolest stars. Stars brighter and hotter than the Sun are rare, whereas substantially dimmer and cooler stars, known as red dwarfs, make up about 75% of the fusor stars in the Milky Way.[85]

    The Sun is a

    population I star, having formed in the spiral arms of the Milky Way galaxy. It has a higher abundance of elements heavier than hydrogen and helium ("metals" in astronomical parlance) than the older population II stars in the galactic bulge and halo.[86] 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, whereas stars born later have more. This higher metallicity is thought to have been crucial to the Sun's development of a planetary system because the planets formed from the accretion of "metals".[87]

    The region of space dominated by the Solar magnetosphere is the heliosphere, which spans much of the Solar System. Along with light, the Sun radiates a continuous stream of charged particles (a plasma) called the solar wind. This stream spreads outwards at speeds from 900,000 kilometres per hour (560,000 mph) to 2,880,000 kilometres per hour (1,790,000 mph),[88] filling the vacuum between the bodies of the Solar System. The result is a thin, dusty atmosphere, called the interplanetary medium, which extends to at least 100 AU.[89]

    Activity on the Sun's surface, such as

    aurorae seen near the magnetic poles.[91] The largest stable 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.[92][93]

    Inner Solar System

    The inner Solar System is the region comprising the terrestrial planets and the asteroids.[94] Composed mainly of silicates and metals,[95] the objects of the inner Solar System are relatively close to the Sun; the radius of this entire region is less than the distance between the orbits of Jupiter and Saturn. This region is within the frost line, which is a little less than 5 AU from the Sun.[50]

    Inner planets

    Venus and Earth about the same size, Mars is about 0.55 times as big and Mercury is about 0.4 times as big
    The four terrestrial planets Mercury, Venus, Earth and Mars

    The four terrestrial or inner planets have dense, rocky compositions, few or no

    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.[96]

    Asteroids

    asteroid groups and families based on their orbital characteristics. Some asteroids have natural satellites that orbit them, that is, asteroids that orbit larger asteroids.[135]

    • perihelia within the orbit of Mercury. At least 362 are known to date, and include the closest objects to the Sun known in the Solar System.[136] No vulcanoids, asteroids between the orbit of Mercury and the Sun, have been discovered.[137][138] As of 2024, one asteroid has been discovered to orbit completely within Venus's orbit, 594913 ꞌAylóꞌchaxnim.[139]
    • Venus-crossing asteroids are those that cross the orbit of Venus. There are 2,809 as of 2015.[140]
    • Near-Earth asteroids have orbits that approach relatively close to Earth's orbit,[141] and some of them are potentially hazardous objects because they might collide with Earth in the future.[142][143] There are over 37,000 known as of 2024.[144] A number of solar-orbiting meteoroids were large enough to be tracked in space before striking Earth. It is now widely accepted that collisions in the past have had a significant role in shaping the geological and biological history of Earth.[145]
    • Mars-crossing asteroids are those with perhihelia above 1.3 AU which cross the orbit of Mars.[146] As of 2024, NASA lists 26,182 confirmed Mars-crossing asteroids.[140]

    Asteroid belt

    The asteroid belt occupies a torus-shaped region between 2.3 and 3.3 AU from the Sun, which lies between the orbits of Mars and Jupiter. It is thought to be remnants from the Solar System's formation that failed to coalesce because of the gravitational interference of Jupiter.[147] The asteroid belt contains tens of thousands, possibly millions, of objects over one kilometer in diameter.[148] Despite this, the total mass of the asteroid belt is unlikely to be more than a thousandth of that of Earth.[44] The asteroid belt is very sparsely populated; spacecraft routinely pass through without incident.[149]

    The four largest asteroids: Ceres, Vesta, Pallas, Hygiea. Only Ceres and Vesta have been visited by a spacecraft and thus have a detailed picture.

    Below are the descriptions of the three largest bodies in the asteroid belt. They are all considered to be relatively intact protoplanets, a precursor stage before becoming a fully-formed planet (see List of exceptional asteroids):[150][151][152]

    Hilda asteroids are in a 3:2 resonance with Jupiter; that is, they go around the Sun three times for every two Jovian orbits.[166] They lie in three linked clusters between Jupiter and the main asteroid belt.

    Lagrange points: L4, 60° ahead in its orbit, or L5, 60° behind in its orbit.[167] Every planet except Mercury and Saturn is known to possess at least 1 trojan.[168][169][170] The Jupiter trojan population is roughly equal to that of the asteroid belt.[171] After Jupiter, Neptune possesses the most confirmed trojans, at 28.[172]

    Outer Solar System

    The outer region of the Solar System is home to the

    short-period comets 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 planets of the inner Solar System because their lower temperatures allow these compounds to remain solid, without significant sublimation.[24]

    Outer planets

    Jupiter and Saturn is about 2 times bigger than Uranus and Neptune, 10 times bigger than Venus and Earth, 20 times bigger than Mars and 25 times bigger than Mercury
    The outer planets Jupiter, Saturn, Uranus and Neptune, compared to the inner planets Earth, Venus, Mars, and Mercury at the bottom right

    The four outer planets, called giant planets or Jovian planets, collectively make up 99% of the mass orbiting the Sun.

    ice giants,[175] meaning they are largely composed of 'ice' in the astronomical sense (chemical compounds with melting points of up to a few hundred kelvins[173] such as water, methane, ammonia, hydrogen sulfide, and carbon dioxide.[176]) Icy substances comprise the majority of the satellites of the giant planets and small objects that lie beyond Neptune's orbit.[176][177]

    Centaurs

    The centaurs are icy, comet-like bodies whose semi-major axes are longer than Jupiter's and shorter than Neptune's (between 5.5 and 30 AU). These are former Kuiper belt and scattered disc objects (SDOs) that were gravitationally perturbed closer to the Sun by the outer planets, and are expected to become comets or be ejected out of the Solar System.[43] While most centaurs are inactive and asteroid-like, some exhibit cometary activity, such as the first centaur discovered, 2060 Chiron, which has been classified as a comet (95P) because it develops a coma just as comets do when they approach the Sun.[198] The largest known centaur, 10199 Chariklo, has a diameter of about 250 km (160 mi) and is one of the few minor planets possessing a ring system.[199][200]

    Trans-Neptunian region

    Beyond the orbit of Neptune lies the area of the "trans-Neptunian region", with the doughnut-shaped Kuiper belt, home of Pluto and several other dwarf planets, and an overlapping disc of scattered objects, which is tilted toward the plane of the Solar System and reaches much further out than the Kuiper belt. The entire region is still largely unexplored. It appears to consist overwhelmingly of many thousands of small worlds – the largest having a diameter only a fifth that of Earth and a mass far smaller than that of the Moon – composed mainly of rock and ice. This region is sometimes described as the "third zone of the Solar System", enclosing the inner and the outer Solar System.[201]

    Kuiper belt

    Plot of objects around the Kuiper belt and other asteroid populations. J, S, U and N denotes Jupiter, Saturn, Uranus and Neptune.
    Orbit classification of Kuiper belt objects. Some clusters that is subjected to orbital resonance are marked.

    The Kuiper belt is a great ring of debris similar to the asteroid belt, but consisting mainly of objects composed primarily of ice.[202] It extends between 30 and 50 AU from the Sun. It is composed mainly of small Solar System bodies, although the largest few are probably large enough to be dwarf planets.[203] There are estimated to be over 100,000 Kuiper belt objects with a diameter greater than 50 km (30 mi), but the total mass of the Kuiper belt is thought to be only a tenth or even a hundredth the mass of Earth.[43] Many Kuiper belt objects have satellites,[204] and most have orbits that are substantially inclined (~10°) to the plane of the ecliptic.[205]

    The Kuiper belt can be roughly divided into the "classical" belt and the resonant trans-Neptunian objects.[202] The latter have orbits whose periods are in a simple ratio to that of Neptune: for example, going around the Sun twice for every three times that Neptune does, or once for every two. The classical belt consists of objects having no resonance with Neptune, and extends from roughly 39.4 to 47.7 AU.[206] Members of the classical Kuiper belt are sometimes called "cubewanos", after the first of their kind to be discovered, originally designated 1992 QB1, (and has since been named Albion); they are still in near primordial, low-eccentricity orbits.[207]

    There is strong consensus among astronomers that five members of the Kuiper belt are dwarf planets.[203][208] Many dwarf planet candidates are being considered, pending further data for verification.[209]

    • ecliptic plane. Pluto has a 2:3 resonance with Neptune, meaning that Pluto orbits twice around the Sun for every three Neptunian orbits. Kuiper belt objects whose orbits share this resonance are called plutinos.[210] Pluto has five moons: Charon, Styx, Nix, Kerberos, and Hydra.[211]
      • barycenter
        of gravity above their surfaces (i.e. they appear to "orbit each other").
    • Orcus (30.3–48.1 AU), is in the same 2:3 orbital resonance with Neptune as Pluto, and is the largest such object after Pluto itself.[212] Its eccentricity and inclination are similar to Pluto's, but its perihelion lies about 120° from that of Pluto. Thus, the phase of Orcus's orbit is opposite to Pluto's: Orcus is at aphelion (most recently in 2019) around when Pluto is at perihelion (most recently in 1989) and vice versa.[213] For this reason, it has been called the anti-Pluto.[214][215] It has one known moon, Vanth.[216]
    • Haumea (34.6–51.6 AU) was discovered in 2005.[217] It is in a temporary 7:12 orbital resonance with Neptune.[212] Haumea possesses a ring system, two known moons named Hiʻiaka and Namaka, and rotates so quickly (once every 3.9 hours) that it is stretched into an ellipsoid. It is part of a collisional family of Kuiper belt objects that share similar orbits, which suggests a giant impact on Haumea ejected fragments into space billions of years ago.[218]
    • Makemake (38.1–52.8 AU), although smaller than Pluto, is the largest known object in the classical Kuiper belt (that is, a Kuiper belt object not in a confirmed resonance with Neptune). Makemake is the brightest object in the Kuiper belt after Pluto. Discovered in 2005, it was officially named in 2009.[219] Its orbit is far more inclined than Pluto's, at 29°.[220] It has one known moon, S/2015 (136472) 1.[221]
    • Weywot.[222]

    Scattered disc

    The orbital eccentricities and inclinations of the scattered disc population compared to the classical and resonant Kuiper belt objects

    The scattered disc, which overlaps the Kuiper belt but extends out to near 500 AU, is thought to be the source of short-period comets. Scattered-disc objects are believed to have been perturbed into erratic orbits by the gravitational influence of Neptune's early outward migration. Most scattered disc objects have perihelia within the Kuiper belt but aphelia far beyond it (some more than 150 AU from the Sun). SDOs' orbits can be inclined up to 46.8° from the ecliptic plane.[223] 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".[224] Some astronomers classify centaurs as inward-scattered Kuiper belt objects along with the outward-scattered residents of the scattered disc.[225]

    Currently, there is strong consensus among astronomers that two of the bodies in the scattered disc are dwarf planets:

    • Eris (38.3–97.5 AU) is the largest known scattered disc object and the most massive known dwarf planet. Eris's discovery contributed to a debate about the definition of a planet because it is 25% more massive than Pluto[226] and about the same diameter. It has one known 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 at an angle of 44°.[227]
    • Gonggong (33.8–101.2 AU) is a dwarf planet in a comparable orbit to Eris, except that it is in a 3:10 resonance with Neptune.[D 10] It has one known moon, Xiangliu.[228]

    Extreme trans-Neptunian objects

    distant objects (red, brown and cyan) along with the predicted orbit of the hypothetical Planet Nine
    (dark blue)

    Some objects in the Solar System have a very large orbit, and therefore are much less affected by the known giant planets than other minor planet populations. These bodies are called extreme trans-Neptunian objects, or ETNOs for short.

    semi-major axes are at least 150–250 AU wide.[229][230] For example, 541132 Leleākūhonua orbits the Sun once every ~32,000 years, with a distance of 65–2000 AU from the Sun.[D 11]

    This population is divided into three subgroups by astronomers. The

    inner Oort cloud objects, with perihelia beyond 50–60 AU, are too far from Neptune to be strongly influenced by it.[229]

    Currently, there is one ETNO that is classified as a dwarf planet:

    • Sedna (76.2–937 AU) was the first extreme trans-Neptunian object to be discovered. It is a large, reddish object, and takes ~11,400 years to complete one orbit. Mike Brown, who discovered the object in 2003, asserts that it cannot be part of the scattered disc or the Kuiper belt because its perihelion is too distant to have been affected by Neptune's migration.[231] The sednoid population is named after Sedna.[229]

    Edge of the heliosphere

    Diagram of the Sun's magnetosphere and helioshealth

    The Sun's

    heliosheath.[232]

    The heliosheath has been theorized 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 to possibly several thousands of AU.

    Cassini and Interstellar Boundary Explorer spacecraft has suggested that it is forced into a bubble shape by the constraining action of the interstellar magnetic field,[236][237] but the actual shape remains unknown.[238]

    The shape and form of the outer edge of the heliosphere is likely affected by the

    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.[232] The heliopause is considered the beginning of the interstellar medium.[89] 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.[239] Large objects outside the heliopause remain gravitationally bound to the Sun, but the flow of matter in the interstellar medium homogenizes the distribution of micro-scale objects.[89]

    Miscellaneous populations

    Comets

    At lower left, a white coma stands out against a black background. Nebulous material streams away to the top and left, slowly fading with distance.
    The sparse plasma (blue) and dust (white) in the tail of comet Hale–Bopp are being shaped by pressure from solar radiation and the solar wind, respectively.

    Comets are

    coma: a long tail of gas and dust often visible to the naked eye.[240]

    Short-period comets have orbits lasting less than two hundred years. Long-period comets have orbits lasting thousands of years. Short-period comets are thought to originate in the Kuiper belt, whereas long-period comets, such as Hale–Bopp, are thought to originate in the Oort cloud. Many comet groups, such as the Kreutz sungrazers, formed from the breakup of a single parent.[241] Some comets with hyperbolic orbits may originate outside the Solar System, but determining their precise orbits is difficult.[242] Old comets whose volatiles have mostly been driven out by solar warming are often categorized as asteroids.[243]

    Meteoroids, meteors and dust

    The planets, zodiacal light and meteor shower (top left of image)

    Solid objects smaller than one meter are usually called meteoroids and micrometeoroids (grain-sized), with the exact division between the two categories being debated over the years.[244] By 2017, the IAU designated any solid object having a diameter between ~30 micrometers and 1 meter as meteoroids, and depreciated the micrometeoroid categorization, instead terms smaller particles simply as 'dust particles'.[245]

    Some meteoroids formed via disintegration of comets and asteroids, while a few formed via impact debris ejected from planetary bodies. Most meteoroids are made of silicates and heavier metals like nickel and iron.[246] When passing through the Solar System, comets produce a trail of meteoroids; it is hypothesized that this is caused either by vaporization of the comet's material or by simple breakup of dormant comets. When crossing an atmosphere, these meteoroids will produce bright streaks in the sky due to atmospheric entry, called meteors. If a stream of meteoroids enter the atmosphere on parallel trajectories, the meteors will seemingly 'radiate' from a point in the sky, hence the phenomenon's name: meteor shower.[247]

    The inner Solar System is home to the zodiacal dust cloud, which is visible as the hazy zodiacal light in dark, unpolluted skies. It may be generated by collisions within the asteroid belt brought on by gravitational interactions with the planets; a more recent proposed origin is materials from planet Mars.[248] The outer Solar System hosts a cosmic dust cloud. It extends from about 10 AU to about 40 AU, and was probably created by collisions within the Kuiper belt.[249][250]

    Boundary region and uncertainties

    An artist's impression of the Oort cloud, a region still well within the sphere of influence of the Solar System, including a depiction of the much further inside Kuiper belt (inset); the sizes of objects are over-scaled for visibility.

    Much of the outer Solar System is still unknown. The region beyond 100 AU away is virtually unexplored and learning about this region of space is difficult. Study of this region depends upon inferences from those few objects whose orbits happen to be perturbed such that they fall closer to the Sun, and even then, detecting these objects has often been possible only when they happened to become bright enough to register as comets.[251] Many objects are yet to be discovered in the Solar System's outer region.[252]

    The Oort cloud is a theorized spherical shell of up to a trillion icy objects that is thought to be the source for all long-period comets.[253][254] No direct observation of the Oort cloud is possible with present imaging technology.[255] It is theorized to surround the Solar System at roughly 50,000 AU (~0.9 ly) from the Sun and possibly to as far as 100,000 AU (~1.8 ly). The Oort cloud is thought 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.[253][254]

    As of the 2020s, a few astronomers have hypothesized that Planet Nine (a planet beyond Neptune) might exist, based on statistical variance in the orbit of extreme trans-Neptunian objects.[256] Their closest approaches to the Sun are mostly clustered around one sector and their orbits are similarly tilted, suggesting that a large planet might be influencing their orbit over millions of years.[257][258][259] However, some astronomers said that this observation might be credited to observational biases or just sheer coincidence.[260] An alternative hypothesis has a close flyby of another star disrupting the outer Solar System.[261]

    The Sun's gravitational field is estimated to

    Comet West, have aphelia around 70,000 AU from the Sun.[264] The Sun's Hill sphere with respect to the galactic nucleus, the effective range of its gravitational influence, is thought to extend up to a thousand times farther and encompasses the hypothetical Oort cloud.[265] It was calculated by G. A. Chebotarev to be 230,000 AU.[7]

    The Solar System (left) within the interstellar medium, with the different regions and their distances on a logarithmic scale

    Celestial neighborhood

    Diagram of the Local Interstellar Cloud, the G-Cloud and surrounding stars. As of 2022, the exact position of the Solar System within the interstellar clouds remains an unresolved question in astronomy.[266]

    Within 10 light-years of the Sun there are relatively few stars, the closest being the triple star system Alpha Centauri, which is about 4.4 light-years away and may be in the Local Bubble's G-Cloud.[267] Alpha Centauri A and B are a closely tied pair of Sun-like stars, whereas the closest star to the Sun, the small red dwarf Proxima Centauri, orbits the pair at a distance of 0.2 light-years. In 2016, a potentially habitable exoplanet was found to be orbiting Proxima Centauri, called Proxima Centauri b, the closest confirmed exoplanet to the Sun.[268]

    The Solar System is surrounded by the Local Interstellar Cloud, although it is not clear if it is embedded in the Local Interstellar Cloud or if it lies just outside the cloud's edge.[269] Multiple other interstellar clouds exist in the region within 300 light-years of the Sun, known as the Local Bubble.[269] The latter feature is an hourglass-shaped cavity or superbubble in the interstellar medium roughly 300 light-years across. The bubble is suffused with high-temperature plasma, suggesting that it may be the product of several recent supernovae.[270]

    The Local Bubble is a small superbubble compared to the neighboring wider

    Radcliffe Wave and Split linear structures (formerly Gould Belt), each of which are some thousands of light-years in length.[271] All these structures are part of the Orion Arm, which contains most of the stars in the Milky Way that are visible to the unaided eye.[272]

    Groups of stars form together in

    Corona Australis Molecular Cloud, the Rho Ophiuchi cloud complex and the Taurus molecular cloud; the latter lies just beyond the Local Bubble and is part of the Radcliffe wave.[273]

    Stellar flybys that pass within 0.8 light-years of the Sun occur roughly once every 100,000 years. The closest well-measured approach was Scholz's Star, which approached to ~50,000 AU of the Sun some ~70 thousands years ago, likely passing through the outer Oort cloud.[274] There is a 1% chance every billion years that a star will pass within 100 AU of the Sun, potentially disrupting the Solar System.[275]

    Galactic position

    Diagram of the Milky Way, with galactic features and the relative position of the Solar System labeled.

    The Solar System is located in the

    Orion–Cygnus Arm or Local Spur.[277][278] It is a member of the thin disk population of stars orbiting close to the galactic plane.[279]

    Its speed around the center of the Milky Way is about 220 km/s, so that it completes one revolution every 240 million years.[276] This revolution is known as the Solar System's galactic year.[280] The solar apex, the direction of the Sun's path through interstellar space, is near the constellation Hercules in the direction of the current location of the bright star Vega.[281] The plane of the ecliptic lies at an angle of about 60° to the galactic plane.[c]

    The Sun follows a nearly circular orbit around the Galactic Center (where the supermassive black hole Sagittarius A* resides) at a distance of 26,660 light-years,[283] orbiting at roughly the same speed as that of the spiral arms.[284] If it orbited close to the center, 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. In this scenario, the intense radiation of the Galactic Center could interfere with the development of complex life.[284]

    The Solar System's location in the Milky Way is a factor in the

    extinction events on Earth.[285][286]

    Discovery and exploration

    The motion of 'lights' moving across the sky is the basis of the classical definition of planets: wandering stars.

    Humanity's knowledge of the Solar System has grown incrementally over the centuries. Up to the

    heliocentric reordering of the cosmos, Nicolaus Copernicus was the first person known to have developed a mathematically predictive heliocentric system.[288][289]

    Heliocentrism did not triumph immediately over geocentrism, but the work of Copernicus had its champions, notably Johannes Kepler. Using a heliocentric model that improved upon Copernicus by allowing orbits to be elliptical, and the precise observational data of Tycho Brahe, Kepler produced the Rudolphine Tables, which enabled accurate computations of the positions of the then-known planets. Pierre Gassendi used them to predict a transit of Mercury in 1631, and Jeremiah Horrocks did the same for a transit of Venus in 1639. This provided a strong vindication of heliocentrism and Kepler's elliptical orbits.[290][291]

    In the 17th century,

    solar parallax of a planet (more ideally using the transit of Venus) could be used to trigonometrically determine the distances between Earth, Venus, and the Sun.[294] Halley's friend Isaac Newton, in his magisterial Principia Mathematica of 1687, demonstrated that celestial bodies are not quintessentially different from Earthly ones: the same laws of motion and of gravity apply on Earth and in the skies.[57]
    : 142 

    Solar system diagram by Emanuel Bowen in 1747, when neither Uranus, Neptune, nor the asteroid belts had yet been discovered. Orbits of planets are to scale, but the orbits of moons and the sizes of bodies are not.

    The term "Solar System" entered the English language by 1704, when John Locke used it to refer to the Sun, planets, and comets.[295] In 1705, Halley realized that repeated sightings of a comet were of the same object, returning regularly once every 75–76 years. This was the first evidence that anything other than the planets repeatedly orbited the Sun,[296] though Seneca had theorized this about comets in the 1st century.[297] Careful observations of the 1769 transit of Venus allowed astronomers to calculate the average Earth–Sun distance as 93,726,900 miles (150,838,800 km), only 0.8% greater than the modern value.[298]

    Mercury's orbital anomaly observations led to searches for Vulcan, a planet interior of Mercury, but these attempts were quashed with Albert Einstein's theory of general relativity in 1915.[302]

    In the 20th century, humans began their space exploration around the Solar System, starting with placing

    Sun's corona[307] and visited two dwarf planets (Pluto and Ceres).[308][309] To save on fuel, some space missions make use of gravity assist maneuvers, such as the two Voyager probes accelerating when flying by planets in the outer Solar System[310] and the Parker Solar Probe decelerating closer towards the Sun after its flyby of Venus.[311]

    Humans have landed on the Moon during the Apollo program in the 1960s and 1970s[312] and will return to the Moon in the 2020s with the Artemis program.[313] Discoveries in the 20th and 21st century has prompted the redefinition of the term planet in 2006, hence the demotion of Pluto to a dwarf planet,[314] and further interest in trans-Neptunian objects.[315]

    See also

    Notes

    1. Scattered Disc
      are not added because the individual asteroids are too small to be shown on the diagram.
    2. ^ a b The date is based on the oldest inclusions found to date in meteorites, 4568.2+0.2
      −0.4
      million years, and is thought to be the date of the formation of the first solid material in the collapsing nebula.[17]
    3. ^ a b If is the angle between the
      galactic pole
      then:

      where = 27° 07′ 42.01″ and = 12h 51m 26.282s are the declination and right ascension of the north galactic pole,[282] whereas = 66° 33′ 38.6″ and = 18h 0m 00s 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°.
    4. astronomical nomenclature, specifies capitalizing the names of all individual astronomical objects but uses mixed "Solar System" and "solar system" structures in their naming guidelines document Archived 25 July 2021 at the Wayback Machine. 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 Archived 27 January 2008 at the Wayback Machine
      .
    5. ^ The scale of the Solar System is sufficiently large that astronomers use a custom unit to express distances. The astronomical unit, abbreviated AU, is equal to 150,000,000 km; 93,000,000 mi. This is what the distance from the Earth to the Sun would be if the planet's orbit were perfectly circular.[13]
    6. ^ The International Astronomical Union's Minor Planet Center has yet to officially list Orcus, Quaoar, Gonggong, and Sedna as dwarf planets as of 2024.
    7. ^ For more classifications of Solar System objects, see List of minor-planet groups and Comet § Classification.
    8. ^ a b 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),[42] the Kuiper belt (estimated at 0.1 Earth mass)[43] and the asteroid belt (estimated to be 0.0005 Earth mass)[44] for a total, rounded upwards, of ~37 Earth masses, or 8.1% of 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% of the total orbiting mass.

    References

    Data sources

    1. S2CID 118492541
      .
    2. ^ "The One Hundred Nearest Star Systems". astro.gsu.edu. Research Consortium On Nearby Stars, Georgia State University. 7 September 2007. Archived from the original on 12 November 2007. Retrieved 2 December 2014.
    3. ^ "Solar System Objects". NASA/JPL Solar System Dynamics. Archived from the original on 7 July 2021. Retrieved 14 August 2023.
    4. ^ a b "Latest Published Data". The International Astronomical Union Minor Planet Center. Archived from the original on 5 March 2019. Retrieved 27 May 2024.
    5. ^ Yeomans, Donald K. "HORIZONS Web-Interface for Neptune Barycenter (Major Body=8)". jpl.nasa.gov. JPL Horizons On-Line Ephemeris System. Archived from the original on 7 September 2021. Retrieved 18 July 2014. – Select "Ephemeris Type: Orbital Elements", "Time Span: 2000-01-01 12:00 to 2000-01-02". ("Target Body: Neptune Barycenter" and "Center: Solar System Barycenter (@0)".)
    6. ^ a b c d e f g h Williams, David (27 December 2021). "Planetary Fact Sheet – Metric". Goddard Space Flight Center. Archived from the original on 18 August 2011. Retrieved 11 December 2022.
    7. JPL (Solar System Dynamics). 13 July 2006. Archived
      from the original on 1 November 2013. Retrieved 29 January 2008.
    8. ^ "HORIZONS Web-Interface". NASA. 21 September 2013. Archived from the original on 28 March 2007. Retrieved 4 December 2013.
    9. ^ "Planetary Satellite Physical Parameters". Jet Propulsion Laboratory (Solar System Dynamics). 13 July 2006. Archived from the original on 1 November 2013. Retrieved 29 January 2008.
    10. ^ "JPL Small-Body Database Browser: 225088 Gonggong (2007 OR10)" (20 September 2015 last obs.). Jet Propulsion Laboratory. 10 April 2017. Archived from the original on 10 June 2020. Retrieved 20 February 2020.
    11. ^ "JPL Small-Body Database Browser: (2015 TG387)" (2018-10-17 last obs.). Jet Propulsion Laboratory. Archived from the original on 14 April 2020. Retrieved 13 December 2018.

    Other sources

    1. ^ "Our Local Galactic Neighborhood". interstellar.jpl.nasa.gov. Interstellar Probe Project. NASA. 2000. Archived from the original on 21 November 2013. Retrieved 8 August 2012.
    2. ^ Hurt, R. (8 November 2017). "The Milky Way Galaxy". science.nasa.gov. Retrieved 19 April 2024.
    3. S2CID 54079935
      .
    4. from the original on 28 October 2023. Retrieved 28 September 2023.
    5. ^ .
    6. ^ Greicius, Tony (5 May 2015). "NASA Spacecraft Embarks on Historic Journey Into Interstellar Space". nasa.gov. Archived from the original on 11 June 2020. Retrieved 19 April 2024.
    7. ^ from the original on 7 May 2024. Retrieved 6 May 2024.
    8. .
    9. .
    10. ^ a b "Sun: Facts". science.nasa.gov. 14 November 2017. Archived from the original on 19 April 2024. Retrieved 19 April 2024.
    11. ^ a b "IAU Office of Astronomy for Education". astro4edu.org. IAU Office of Astronomy for Education. Archived from the original on 11 December 2023. Retrieved 11 December 2023.
    12. ^ a b "Solar System: Facts". NASA Science. 13 November 2017. Retrieved 10 July 2025.
    13. S2CID 55944238
      .
    14. ^ a b "Definition of SOLAR SYSTEM". Merriam-Webster. 5 August 2024. Retrieved 10 July 2025.
    15. ^ Boulter, Michael (7 July 2025). "SOLAR SYSTEM Definition und Bedeutung". Collins Englisch Wörterbuch (in German). Retrieved 10 July 2025.
    16. ^ "Features of our Solar System guide for KS3 physics students". BBC Bitesize. 6 June 2022. Retrieved 10 July 2025.
    17. S2CID 56092512
      .
    18. ^ a b c Zabludoff, Ann. "Lecture 13: The Nebular Theory of the origin of the Solar System". NATS 102: The Physical Universe. University of Arizona. Archived from the original on 10 July 2012. Retrieved 27 December 2006.
    19. ^ .
    20. . estimates of disk radii in the Taurus and Ophiuchus star forming regions lie in a wide range between 50 AU and 1000 AU, with a median value of 200 AU.
    21. .
    22. from the original on 9 April 2022. Retrieved 9 April 2022.
    23. .
    24. ^ .
    25. (PDF) from the original on 12 April 2022. Retrieved 10 April 2022.
    26. .
    27. ^ .
    28. .
    29. .
    30. .
    31. .
    32. .
    33. from the original on 10 December 2023. Retrieved 10 December 2023.
    34. ^ .
    35. ^ "Giant red stars may heat frozen worlds into habitable planets – NASA Science". 17 May 2016.
    36. .
    37. ^ "Planetary Nebulas". cfa.harvard.edu. Harvard & Smithsonian Center for Astrophysics. Archived from the original on 6 April 2024. Retrieved 6 April 2024.
    38. from the original on 16 January 2024. Retrieved 16 January 2024.
    39. ^ "The Planets". NASA. 10 July 2023. Retrieved 6 April 2024.
    40. ^ "Kuiper Belt: Facts". NASA. 14 November 2017. Archived from the original on 12 March 2024. Retrieved 6 April 2024.
    41. .
    42. .
    43. ^ a b c Delsanti, Audrey; Jewitt, David (2006). "The Solar System Beyond The Planets" (PDF). Institute for Astronomy, University of Hawaii. Archived from the original (PDF) on 29 January 2007. Retrieved 3 January 2007.
    44. ^ .
    45. ^ "The Sun's Vital Statistics". Stanford Solar Center. Archived from the original on 14 October 2012. Retrieved 29 July 2008, citing Eddy, J. (1979). A New Sun: The Solar Results From Skylab. NASA. p. 37. NASA SP-402. Archived from the original on 30 July 2021. Retrieved 12 July 2017.
    46. ^ Williams, David R. (7 September 2006). "Saturn Fact Sheet". NASA. Archived from the original on 4 August 2011. Retrieved 31 July 2007.
    47. ^ a b Williams, David R. (23 December 2021). "Jupiter Fact Sheet". NASA Goddard Space Flight Center. Archived from the original on 22 January 2018. Retrieved 28 March 2022.
    48. .
    49. . Retrieved 15 July 2025. We note that for all the bodies (except for the Earth, of course), the inclination with respect to the invariable plane is smaller than the inclination with respect to the ecliptic. This is in particular the case for Jupiter and Saturn, for which the inclinations are 0°.3219 and 0°.9254 instead of 1°.3042 and 2°.4859, respectively.
    50. ^ .
    51. .
    52. .
    53. ^ Grossman, Lisa (13 August 2009). "Planet found orbiting its star backwards for first time". New Scientist. Archived from the original on 17 October 2012. Retrieved 10 October 2009.
    54. ^ Nakano, Syuichi (2001). "OAA computing section circular". Oriental Astronomical Association. Archived from the original on 21 September 2019. Retrieved 15 May 2007.
    55. from the original on 15 April 2022. Retrieved 28 March 2022.
    56. .
    57. ^ .
    58. ^ .
    59. .
    60. from the original on 30 July 2022. Retrieved 10 May 2022.
    61. ^ .
    62. .
    63. .
    64. ^ Williams, David R. (23 December 2021). "Neptune Fact Sheet". NASA Goddard Space Flight Center. Archived from the original on 19 November 2016. Retrieved 28 March 2022.
    65. from the original on 20 April 2022. Retrieved 2 April 2022.
    66. .
    67. ^ Boss, Alan (October 2006). "Is it a coincidence that most of the planets fall within the Titius-Bode law's boundaries?". Astronomy. Ask Astro. Vol. 30, no. 10. p. 70. Archived from the original on 16 March 2022. Retrieved 9 April 2022.
    68. ^ Ottewell, Guy (1989). "The Thousand-Yard Model: or, Earth as a Peppercorn". NOAO Educational Outreach Office. Archived from the original on 10 July 2016. Retrieved 10 May 2012.
    69. ^ "Tours of Model Solar Systems". University of Illinois. Archived from the original on 12 April 2011. Retrieved 10 May 2012.
    70. ^ "Luleå är Sedna. I alla fall om vår sol motsvaras av Globen i Stockholm". Norrbotten Kuriren (in Swedish). Archived from the original on 15 July 2010. Retrieved 10 May 2010.
    71. ^ See, for example, Office of Space Science (9 July 2004). "Solar System Scale". NASA Educator Features. Archived from the original on 27 August 2016. Retrieved 2 April 2013.
    72. .
    73. ^ Dyches, Preston; Chou, Felcia (7 April 2015). "The Solar System and Beyond is Awash in Water". NASA. Archived from the original on 10 April 2015. Retrieved 8 April 2015.
    74. ISBN 978-0-8165-2844-8. Archived from the original on 6 April 2023. Retrieved 6 April 2023. Extract of page 658 Archived 15 April 2023 at the Wayback Machine
    75. ^ .
    76. from the original on 7 April 2022. Retrieved 31 March 2022.
    77. .
    78. .
    79. .
    80. ^ "Sun: Facts & Figures". NASA. Archived from the original on 2 January 2008. Retrieved 14 May 2009.
    81. .
    82. .
    83. ^ "What Color is the Sun?". NASA. 25 May 2023. Archived from the original on 26 April 2024. Retrieved 6 April 2024.
    84. ^ "What Color is the Sun?". Stanford Solar Center. Archived from the original on 30 October 2017. Retrieved 23 May 2016.
    85. S2CID 246842719
      .
    86. .
    87. .
    88. .
    89. ^ a b c Steigerwald, Bill (24 May 2005). "Voyager Enters Solar System's Final Frontier". NASA. Archived from the original on 16 May 2020. Retrieved 2 April 2007.
    90. ^ Phillips, Tony (15 February 2001). "The Sun Does a Flip". NASA Science: Share the Science. Archived from the original on 1 April 2022. Retrieved 1 April 2022.
    91. OCLC 961476196. Archived from the original
      on 19 July 2020. Retrieved 9 March 2022.
    92. ^ "A Star with two North Poles". NASA Science: Share the Science. 22 April 2003. Archived from the original on 1 April 2022. Retrieved 1 April 2022.
    93. .
    94. ^ "Inner Solar System". NASA Science: Share the Science. 10 May 2016. Archived from the original on 10 April 2022. Retrieved 2 April 2022.
    95. .
    96. ^ from the original on 12 April 2022. Retrieved 29 March 2022.
    97. .
    98. ^
      PMID 17741171. Archived from the original
      (PDF) on 21 July 2018. Retrieved 25 October 2017.
    99. ^ Talbert, Tricia, ed. (21 March 2012). "MESSENGER Provides New Look at Mercury's Surprising Core and Landscape Curiosities". NASA. Archived from the original on 12 January 2019. Retrieved 20 April 2018.
    100. S2CID 22408219
      .
    101. . The composition of Mercury's exosphere, with its abundant H and He, clearly indicates a strong solar wind source. Once solar wind plasma and particles gain access to the magnetosphere, they predominantly precipitate to the surface, where solar wind species are neutralized, thermalized, and released again into the exosphere. Moreover, bombardment of the surface by solar wind particles, especially energetic ions, contributes to ejection of neutral species from the surface into the exosphere (via "sputtering") as well as other chemical and physical surface modification processes.
    102. ^ a b "How Many Moons Does Each Planet Have? | NASA Space Place – NASA Science for Kids". spaceplace.nasa.gov. Archived from the original on 21 April 2024. Retrieved 21 April 2024.
    103. (PDF) from the original on 4 May 2019. Retrieved 11 August 2023.
    104. ^ Bullock, Mark Alan (1997). The Stability of Climate on Venus (PDF) (PhD thesis). Southwest Research Institute. Archived from the original (PDF) on 14 June 2007. Retrieved 26 December 2006.
    105. ^ Rincon, Paul (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. Archived from the original (PDF) on 14 June 2007. Retrieved 19 November 2006.
    106. . E04S06.
    107. ^ "What are the characteristics of the Solar System that lead to the origins of life?". NASA Science (Big Questions). Archived from the original on 8 April 2010. Retrieved 30 August 2011.
    108. .
    109. ^ Zimmer, Carl (3 October 2013). "Earth's Oxygen: A Mystery Easy to Take for Granted". The New York Times. Archived from the original on 3 October 2013. Retrieved 3 October 2013.
    110. ^ Staff. "Climate Zones". UK Department for Environment, Food and Rural Affairs. Archived from the original on 8 August 2010. Retrieved 24 March 2007.
    111. ^ Carlowicz, Michael; Simmon, Robert (15 July 2019). "Seeing Forests for the Trees and the Carbon: Mapping the World's Forests in Three Dimensions". NASA Earth Observatory. Archived from the original on 31 December 2022. Retrieved 31 December 2022.
    112. ^ Cain, Fraser (1 June 2010). "What Percentage of the Earth's Land Surface is Desert?". Universe Today. Archived from the original on 3 January 2023. Retrieved 3 January 2023.
    113. ^ "Ice Sheet". National Geographic Society. 6 August 2006. Archived from the original on 27 November 2023. Retrieved 3 January 2023.
    114. from the original on 20 April 2022. Retrieved 12 April 2022.
    115. ^ "Facts About Earth – NASA Science". NASA Science. 30 May 2023. Retrieved 11 January 2024.
    116. S2CID 240071005
    117. ^ "The Smell of Moondust". NASA. 30 January 2006. Archived from the original on 8 March 2010. Retrieved 15 March 2010.
    118. .
    119. ^ Norman, M. (21 April 2004). "The Oldest Moon Rocks". Planetary Science Research Discoveries. Hawai'i Institute of Geophysics and Planetology. Archived from the original on 18 April 2007. Retrieved 12 April 2007.
    120. ^ Globus, Ruth (1977). "Chapter 5, Appendix J: Impact Upon Lunar Atmosphere". In Richard D. Johnson & Charles Holbrow (ed.). Space Settlements: A Design Study. NASA. Archived from the original on 31 May 2010. Retrieved 17 March 2010.
    121. .
    122. from the original on 7 April 2022. Retrieved 9 April 2022.
    123. ^ "Polar Caps". Mars Education at Arizona State University. Archived from the original on 28 May 2021. Retrieved 6 January 2022.
    124. ^ Gatling, David C.; Leovy, Conway (2007). "Mars Atmosphere: History and Surface Interactions". In Lucy-Ann McFadden; et al. (eds.). Encyclopaedia of the Solar System. pp. 301–314.
    125. ^ Noever, David (2004). "Modern Martian Marvels: Volcanoes?". NASA Astrobiology Magazine. Archived from the original on 14 March 2020. Retrieved 23 July 2006.
    126. ^ NASA – Mars in a Minute: Is Mars Really Red? Archived 20 July 2014 at the Wayback Machine (Transcript Archived 6 November 2015 at the Wayback Machine) Public Domain This article incorporates text from this source, which is in the public domain.
    127. S2CID 45843366
      .
    128. ^ Philips, Tony (31 January 2001). "The Solar Wind at Mars". Science@NASA. Archived from the original on 18 August 2011. Retrieved 22 April 2022. Public Domain This article incorporates text from this source, which is in the public domain.
    129. ^ Andrews, Robin George (25 July 2020). "Why the 'Super Weird' Moons of Mars Fascinate Scientists – What's the big deal about little Phobos and tinier Deimos?". The New York Times. Archived from the original on 25 July 2020. Retrieved 25 July 2020.
    130. ^ "Phobos". BBC Online. 12 January 2004. Archived from the original on 22 April 2009. Retrieved 19 July 2021.
    131. ^ "Stickney Crater-Phobos". Archived from the original on 3 November 2011. Retrieved 21 April 2024. One of the most striking features of Phobos, aside from its irregular shape, is its giant crater Stickney. Because Phobos is only 28 by 20 kilometers (17 by 12 mi), it must have been nearly shattered from the force of the impact that caused the giant crater. Grooves that extend across the surface from Stickney appear to be surface fractures caused by the impact.
    132. ^ "Deimos". Britannica. 6 June 2023. Archived from the original on 12 November 2018. Retrieved 21 April 2024. It thus appears smoother than Phobos because its craters lie partially buried under this loose material.
    133. ^ "IAU Planet Definition Committee". International Astronomical Union. 2006. Archived from the original on 3 June 2009. Retrieved 1 March 2009.
    134. ^ "Are Kuiper Belt Objects asteroids? Are large Kuiper Belt Objects planets?". Cornell University. Archived from the original on 3 January 2009. Retrieved 1 March 2009.
    135. from the original on 20 April 2022. Retrieved 9 March 2022.
    136. ^ List of asteroids with q<0.3075 AU generated by the JPL Small-Body Database Search Engine Archived 3 March 2016 at the Wayback Machine Retrieved 30 May 2012
    137. .
    138. .
    139. from the original on 1 October 2022. Retrieved 1 October 2022.
    140. ^ a b "Small-Body Database Query". NASA. Archived from the original on 27 September 2021. Retrieved 3 June 2024.
    141. (PDF) from the original on 9 August 2017. Retrieved 30 August 2009.
    142. ^ "NEO Basics – Potentially Hazardous Asteroids (PHAs)". CNEOS NASA/JPL. Archived from the original on 11 November 2021. Retrieved 10 March 2022.
    143. ^ Baalke, Ron. "Near-Earth Object Groups". Jet Propulsion Laboratory. NASA. Archived from the original on 2 February 2002. Retrieved 11 November 2016.
    144. ^ "Discovery Statistics – Cumulative Totals". NASA/JPL CNEOS. 30 December 2024. Archived from the original on 1 January 2025. Retrieved 1 January 2025.
    145. ^ Monastersky, Richard (1 March 1997). "The Call of Catastrophes". Science News Online. Archived from the original on 13 March 2004. Retrieved 2 January 2025.
    146. doi:10.1051/0004-6361:20020834.{{cite journal}}: CS1 maint: multiple names: authors list (link) CS1 maint: numeric names: authors list (link
      )
    147. (PDF) on 21 February 2007. Retrieved 22 March 2007.
    148. .
    149. ^ "Cassini Passes Through Asteroid Belt". NASA. 14 April 2000. Archived from the original on 25 January 2021. Retrieved 1 March 2021.
    150. from the original on 28 September 2021. Retrieved 12 September 2021.
    151. ^ Cook, Jia-Rui C. (29 March 2011). "When Is an Asteroid Not an Asteroid?". NASA/JPL. Archived from the original on 29 June 2011. Retrieved 30 July 2011.
    152. (PDF) from the original on 7 January 2023. Retrieved 4 January 2023.
    153. ^ "Question and answers 2". IAU. Archived from the original on 30 January 2016. Retrieved 31 January 2008. Ceres is (or now we can say it was) the largest asteroid ... There are many other asteroids that can come close to the orbital path of Ceres.
    154. S2CID 133739176
      .
    155. .
    156. ^ Raymond, C.; Castillo-Rogez, J. C.; Park, R. S.; Ermakov, A.; et al. (September 2018). "Dawn Data Reveal Ceres' Complex Crustal Evolution" (PDF). European Planetary Science Congress. Vol. 12. Archived (PDF) from the original on 30 January 2020. Retrieved 19 July 2020.
    157. ^ Krummheuer, Birgit (6 March 2017). "Cryovolcanism on Dwarf Planet Ceres". Max Planck Institute for Solar System Research. Archived from the original on 2 February 2024. Retrieved 22 April 2024.
    158. ^ "Confirmed: Ceres Has a Transient Atmosphere". Universe Today. 6 April 2017. Archived from the original on 15 April 2017. Retrieved 14 April 2017.
    159. ^ from the original on 22 April 2024. Retrieved 22 April 2024.
    160. ^ a b Lakdawalla, Emily; et al. (21 April 2020). "What Is A Planet?". The Planetary Society. Archived from the original on 22 January 2022. Retrieved 3 April 2022.
    161. ^ "A look into Vesta's interior". Max-Planck-Gesellschaft. 6 January 2011. Archived from the original on 5 March 2023. Retrieved 22 April 2024.
    162. .
    163. .
    164. ^ "Athena: A SmallSat Mission to (2) Pallas". Archived from the original on 21 November 2021. Retrieved 7 October 2020.
    165. .
    166. ^ 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. 273–287.
    167. ^ "Trojan Asteroids". Cosmos. Swinburne University of Technology. Archived from the original on 23 June 2017. Retrieved 13 June 2017.
    168. S2CID 205225571
      .
    169. .
    170. .
    171. .
    172. ^ "List of Neptune Trojans". Minor Planet Center. 28 October 2018. Archived from the original on 25 May 2012. Retrieved 28 December 2018.
    173. ^ from the original on 21 December 2019. Retrieved 25 August 2019.
    174. ^ "Gas Giant | Planet Types". Exoplanet Exploration: Planets Beyond our Solar System. 22 October 2020. Archived from the original on 28 November 2020. Retrieved 22 December 2020.
    175. ^ Lissauer, Jack J.; Stevenson, David J. (2006). "Formation of Giant Planets" (PDF). NASA Ames Research Center; California Institute of Technology. Archived from the original (PDF) on 26 March 2009. Retrieved 16 January 2006.
    176. ^ .
    177. .
    178. from the original on 20 April 2022. Retrieved 13 April 2022.
    179. .
    180. .
    181. ^ Pappalardo, R. T. (1999). "Geology of the Icy Galilean Satellites: A Framework for Compositional Studies". Brown University. Archived from the original on 30 September 2007. Retrieved 16 January 2006.
    182. ISBN 0-521-81808-7. Archived from the original
      (PDF) on 26 March 2009.
    183. ^ "In Depth: Saturn". NASA Science: Solar System Exploration. 18 August 2021. Archived from the original on 24 February 2018. Retrieved 31 March 2022.
    184. S2CID 4330204
      .
    185. (PDF) from the original on 25 July 2011. Retrieved 21 April 2024.
    186. ^ a b Williams, Matt (7 August 2015). "The moons of Saturn". phys.org. Archived from the original on 21 April 2024. Retrieved 21 April 2024.
    187. ^ "Calypso". NASA. January 2024. Archived from the original on 17 May 2024. Retrieved 16 May 2024.
    188. ^ "Polydeuces". NASA. January 2024. Retrieved 16 May 2024.
    189. ^ .
    190. ^ (PDF) from the original on 25 February 2014. Retrieved 21 April 2024.
    191. ^ Devitt, Terry (14 October 2008). "New images yield clues to seasons of Uranus". University of Wisconsin–Madison. Archived from the original on 6 April 2024. Retrieved 6 April 2024.
    192. S2CID 250909885
      .
    193. .
    194. .
    195. .
    196. ^ "New Uranus and Neptune Moons". Earth & Planetary Laboratory. Carnegie Institution for Science. 23 February 2024. Archived from the original on 23 February 2024. Retrieved 23 February 2024.
    197. (PDF) from the original on 31 August 2021. Retrieved 31 March 2022.
    198. ^ Vanouplines, Patrick (1995). "Chiron biography". Vrije Universitiet Brussel. Archived from the original on 2 May 2009. Retrieved 23 June 2006.
    199. .
    200. .
    201. ^ Stern, Alan (February 2015). "Journey to the Solar System's Third Zone". American Scientist. Archived from the original on 26 October 2018. Retrieved 26 October 2018.
    202. ^ .
    203. ^
      S2CID 126574999. Archived from the original
      on 7 April 2019.
    204. (PDF) from the original on 28 September 2018. Retrieved 19 October 2011.
    205. (PDF) from the original on 15 March 2016. Retrieved 15 August 2009.
    206. .
    207. (PDF) from the original on 25 August 2014. Retrieved 26 December 2006.
    208. .
    209. .
    210. (PDF) on 7 June 2011. Retrieved 26 December 2006.
    211. ^ "In Depth: Pluto". NASA Science: Solar System Exploration. 6 August 2021. Archived from the original on 31 March 2022. Retrieved 31 March 2022.
    212. ^ (PDF) from the original on 13 November 2012. Retrieved 9 April 2022.
    213. ^ "MPEC 2004-D15 : 2004 DW". Minor Planet Center. 20 February 2004. Archived from the original on 3 March 2016. Retrieved 5 July 2011.
    214. ^ Michael E. Brown (23 March 2009). "S/2005 (90482) 1 needs your help". Mike Brown's Planets (blog). Archived from the original on 28 March 2009. Retrieved 25 March 2009.
    215. OCLC 926914921
      .
    216. ^ Green, Daniel W. E. (22 February 2007). "IAUC 8812: Sats OF 2003 AZ_84, (50000), (55637), (90482)". International Astronomical Union Circular. Archived from the original on 14 March 2012. Retrieved 4 July 2011.
    217. ^ "IAU names fifth dwarf planet Haumea". International Astronomical Union. 17 September 2008. Archived from the original on 25 April 2014. Retrieved 9 April 2022.
    218. S2CID 252620869
      . 225.
    219. ^ "Fourth dwarf planet named Makemake". International Astronomical Union. 19 July 2009. Archived from the original on 30 July 2017. Retrieved 9 April 2022.
    220. Buie, Marc W. (5 April 2008). "Orbit Fit and Astrometric record for 136472". SwRI (Space Science Department). Archived
      from the original on 27 May 2020. Retrieved 15 July 2012.
    221. .
    222. .
    223. (PDF) from the original on 21 January 2022. Retrieved 12 May 2022.
    224. ^ Jewitt, David (2005). "The 1,000 km Scale KBOs". University of Hawaii. Archived from the original on 9 June 2014. Retrieved 16 July 2006.
    225. ^ "List of Centaurs and Scattered-Disk Objects". IAU: Minor Planet Center. Archived from the original on 29 June 2017. Retrieved 2 April 2007.
    226. S2CID 21468196
      .
    227. .
    228. . L1.
    229. ^ .
    230. .
    231. ^ Jewitt, David (2004). "Sedna – 2003 VB12". University of Hawaii. Archived from the original on 16 July 2011. Retrieved 23 June 2006.
    232. ^
      Bibcode:2000A&A...357..268F. Archived from the original
      (PDF) on 8 August 2017. Retrieved 24 August 2008. See Figures 1 and 2.
    233. ^ Hatfield, Miles (3 June 2021). "The Heliopedia". NASA. Archived from the original on 25 March 2022. Retrieved 29 March 2022.
    234. PMID 36874191
      .
    235. from the original on 20 April 2022. Retrieved 9 April 2022.
    236. ^ "Cassini's Big Sky: The View from the Center of Our Solar System". Jet Propulsion Laboratory. 19 November 2009. Archived from the original on 9 April 2022. Retrieved 9 April 2022.
    237. S2CID 239998560
      .
    238. .
    239. ^ Nemiroff, R.; Bonnell, J., eds. (24 June 2002). "The Sun's Heliosphere & Heliopause". Astronomy Picture of the Day. NASA. Retrieved 23 June 2006.
    240. ^ "In Depth: Comets". NASA Science: Solar System Exploration. 19 December 2019. Archived from the original on 31 March 2022. Retrieved 31 March 2022.
    241. .
    242. .
    243. .
    244. from the original on 25 March 2022. Retrieved 10 April 2022.
    245. ^ "Definition of terms in meteor astronomy" (PDF). International Astronomical Union. IAU Commission F1. 30 April 2017. p. 2. Archived (PDF) from the original on 22 December 2021. Retrieved 25 July 2020.
    246. ^ "Meteoroid". National Geographic. 28 May 2010. Archived from the original on 7 October 2015. Retrieved 24 August 2015.
    247. .
    248. .
    249. ^ "ESA scientist discovers a way to shortlist stars that might have planets". ESA Science and Technology. 2003. Archived from the original on 2 May 2013. Retrieved 3 February 2007.
    250. (PDF) from the original on 15 May 2016. Retrieved 9 February 2007.
    251. .
    252. ^ Loeffler, John (1 October 2021). "Our solar system may have a hidden planet beyond Neptune – no, not that one". MSN. Archived from the original on 1 October 2021. Retrieved 7 April 2022.
    253. ^
      S2CID 205013399
      .
    254. ^ a b Arnett, Bill (2006). "The Kuiper Belt and the Oort Cloud". Nine Planets. Archived from the original on 7 August 2019. Retrieved 23 June 2006.
    255. ^ "Oort Cloud". NASA Solar System Exploration. 20 June 2023. Archived from the original on 30 June 2023. Retrieved 1 July 2023.
    256. S2CID 119248548
      .
    257. S2CID 4393431. Archived from the original
      (PDF) on 16 December 2014. Retrieved 20 January 2016.
    258. from the original on 19 October 2021. Retrieved 20 April 2024.
    259. from the original on 9 April 2023. Retrieved 20 April 2024.
    260. .
    261. .
    262. ^ Encrenaz, T.; Bibring, J. P.; Blanc, M.; Barucci, M. A.; Roques, F.; Zarka, P. H. (2004). The Solar System (3rd ed.). Springer. p. 1.
    263. S2CID 195584070
      . A139.
    264. ^ Norman, Neil (May 2020). "10 great comets of recent times". BBC Sky at Night Magazine. Archived from the original on 25 January 2022. Retrieved 10 April 2022.
    265. .
    266. .
    267. . 41.
    268. .
    269. ^ .
    270. .
    271. .
    272. . 13.
    273. .
    274. . L17.
    275. .
    276. ^ from the original on 20 April 2022. Retrieved 8 April 2022.
    277. .
    278. .
    279. .
    280. ^ Leong, Stacy (2002). "Period of the Sun's Orbit around the Galaxy (Cosmic Year)". The Physics Factbook. Archived from the original on 7 January 2019. Retrieved 2 April 2007.
    281. OCLC 56727455
      .
    282. .
    283. from the original on 20 April 2022. Retrieved 1 April 2022.
    284. ^ a b c Mullen, Leslie (18 May 2001). "Galactic Habitable Zones". Astrobiology Magazine. Archived from the original on 7 August 2011. Retrieved 1 June 2020.
    285. from the original on 1 April 2022. Retrieved 1 April 2022.
    286. from the original on 1 April 2022. Retrieved 1 April 2022.
    287. from the original on 30 July 2022. Retrieved 13 May 2022.
    288. .
    289. .
    290. .
    291. .
    292. from the original on 27 November 2021. Retrieved 1 April 2022.
    293. ^ "Christiaan Huygens: Discoverer of Titan". ESA Space Science. The European Space Agency. 8 December 2012. Archived from the original on 6 December 2019. Retrieved 27 October 2010.
    294. .
    295. ^ See, for example:
    296. from the original on 20 April 2022. Retrieved 7 April 2022.
    297. from the original on 15 June 2021. Retrieved 28 June 2021.
    298. (PDF) from the original on 3 February 2022. Retrieved 3 April 2022.
    299. .
    300. .
    301. from the original on 29 November 2021. Retrieved 1 April 2022.
    302. ^ Garner, Rob (10 December 2018). "50th Anniversary of OAO 2: NASA's 1st Successful Stellar Observatory". NASA. Archived from the original on 29 December 2021. Retrieved 20 April 2022.
    303. ^ "Fact Sheet". JPL. Archived from the original on 29 November 2016. Retrieved 3 March 2016.
    304. ^ Woo, Marcus (20 November 2014). "This Is What It Sounded Like When We Landed on a Comet". Wired. Archived from the original on 23 November 2014. Retrieved 20 April 2022.
    305. ^ Marks, Paul (3 December 2014). "Hayabusa 2 probe begins journey to land on an asteroid". New Scientist. Archived from the original on 11 February 2022. Retrieved 20 April 2022.
    306. ^ "NASA's Parker Solar Probe becomes first spacecraft to 'touch' the sun". CNN. 14 December 2021. Archived from the original on 14 December 2021. Retrieved 15 December 2021.
    307. ISSN 0362-4331
      . Retrieved 20 April 2022.
    308. ^ McCartney, Gretchen; Brown, Dwayne; Wendel, JoAnna (7 September 2018). "Legacy of NASA's Dawn, Near the End of its Mission". NASA. Retrieved 8 September 2018.
    309. ^ "Basics of Spaceflight: A Gravity Assist Primer". science.nasa.gov. 20 July 2023. Retrieved 2 May 2024.
    310. ^ "Parker Solar Probe Changed the Game Before it Even Launched – NASA". 4 October 2018. Retrieved 2 May 2024.
    311. .
    312. ^ Foust, Jeff (13 March 2023). "NASA planning to spend up to $1 billion on space station deorbit module". SpaceNews. Retrieved 13 March 2023.
    313. ^ Chang, Kenneth (18 January 2022). "Quiz – Is Pluto A Planet? – Who doesn't love Pluto? It shares a name with the Roman god of the underworld and a Disney dog. But is it a planet? – Interactive". The New York Times. Retrieved 18 January 2022.
    314. ^ Spaceflight, Leonard David (9 January 2019). "A Wild 'Interstellar Probe' Mission Idea Is Gaining Momentum". Space.com. Retrieved 23 September 2019.
    Listen to this article (1 hour and 2 minutes)
    Spoken Wikipedia icon
    Audio help · More spoken articles
    )