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TheSolar System consists of theSun and the objects thatorbit it. The name comes fromSōl, the Latin name for the Sun. Itformed about 4.6 billion years ago when a dense region of amolecular cloud collapsed, creating the Sun and aprotoplanetary disc from which the orbiting bodies assembled. Thefusion of hydrogen into helium inside theSun's core releases energy, which is primarily emitted through its outerphotosphere. This creates a decreasing temperaturegradient across the system. Over 99.86% of the Solar System's mass is located within the Sun.
Themost massive objects that orbit the Sun are the eightplanets. Closest to the Sun in order of increasing distance are the fourterrestrial planets –Mercury,Venus,Earth andMars. These are the planets of theinner Solar System. Earth and Mars are the only planets in the Solar System which orbit within the Sun'shabitable zone, where liquid water can exist on the surface. Beyond thefrost line at about fiveastronomical units (AU), are twogas giants –Jupiter andSaturn – and twoice giants –Uranus andNeptune. These are the planets of theouter Solar System. 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 ninedwarf planets:Ceres,Orcus,Pluto,Haumea,Quaoar,Makemake,Gonggong,Eris, andSedna. Six planets, seven dwarf planets, and other bodies have orbitingnatural satellites, which are commonly called 'moons', and range fromsizes of dwarf planets, like Earth'sMoon, at their largest, to much less massivemoonlets at their smallest. There aresmall Solar System bodies, such asasteroids,comets,centaurs,meteoroids, andinterplanetary dust clouds. Some of these bodies are in theasteroid belt (between Mars's and Jupiter's orbit) and theKuiper belt (just outside Neptune's orbit).
Between the bodies of the Solar System is aninterplanetary medium of dust and particles. The Solar System is constantly flooded by outflowingcharged particles from thesolar wind, forming theheliosphere. At around70–90 AU from the Sun, the solar wind is halted by theinterstellar medium, resulting in theheliopause. This is the boundary tointerstellar space. Further out somewhere beyond2,000 AU from the Sun extends the outermost region of the Solar System, the theorizedOort cloud, the source forlong-period comets, stretching to the edge of the Solar System, the edge of itsHill sphere, at 178,000–227,000 AU (2.81–3.59 ly), where its gravitational potential becomes equal to the galactic potential. The Solar System currently moves through a cloud of interstellar medium called theLocal Cloud. Theclosest star to the Solar System,Proxima Centauri, is 269,000 AU (4.25 ly) away. Both are within theLocal Bubble, a relatively small 1,000 light-years (ly) wide region of theMilky Way. (Full article...)
The cloud is thought to encompass two regions: adisc-shaped inner Oort cloud aligned with thesolar ecliptic (also called itsHills cloud) and aspherical outer Oort cloud enclosing the entireSolar System. Both regions lie well beyond theheliosphere and are ininterstellar space. The innermost portion of the Oort cloud is more than a thousand times farther from the Sun than theKuiper belt, thescattered disc and thedetached objects—three nearer reservoirs oftrans-Neptunian objects. (Full article...)


| Solar System | ||
|---|---|---|
| Celestial mechanics | Comets | ...in fiction |
| Minor planets | Moons | Planetary missions |
| Planets... | Sun | Surface feature nomenclature... |


Solar System:Planets (Definition · Planetary habitability · Terrestrial planets · Gas giants · Rings) · Dwarf planets (Plutoid) · Colonization · Discovery timelineˑExploration · Moons · Planetariums
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Italicized articles are on dwarf planets or major moons.

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