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Portal:Outer space

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The Outer Space Portal

Introduction

The lower half shows a blue planet with patchy white clouds. The upper half has a man in a white spacesuit and maneuvering unit against a black background.
Because of the hazards of a vacuum, astronauts must wear a pressurizedspace suit while off-Earth and outside their spacecraft.

Outer space, or simplyspace, is the expanse that exists beyondEarth's atmosphere and betweencelestial bodies. It contains ultra-lowlevels of particle densities, constituting anear-perfect vacuum of predominantlyhydrogen andheliumplasma, permeated byelectromagnetic radiation,cosmic rays,neutrinos,magnetic fields anddust. The baselinetemperature of outer space, as set by thebackground radiation from theBig Bang, is 2.7 kelvins (−270 °C; −455 °F).

Theplasma between galaxies is thought to account for about half of thebaryonic (ordinary) matter in the universe, having anumber density of less than onehydrogen atom per cubic metre and akinetic temperature of millions ofkelvins. Local concentrations of matter have condensed intostars andgalaxies. Intergalactic space takes up most of the volume of theuniverse, but even galaxies andstar systems consist almost entirely of empty space. Most of the remainingmass-energy in theobservable universe is made up of an unknown form, dubbeddark matter anddark energy.

Outer space does not begin at a definite altitude above Earth's surface. TheKármán line, an altitude of 100 km (62 mi) abovesea level, is conventionally used as the start of outer space in space treaties and for aerospace records keeping. Certain portions of the upperstratosphere and themesosphere are sometimes referred to as "near space". The framework for internationalspace law was established by theOuter Space Treaty, which entered into force on 10 October 1967. This treaty precludes any claims ofnational sovereignty and permits all states to freelyexplore outer space. Despite the drafting ofUN resolutions for the peaceful uses of outer space,anti-satellite weapons have been tested inEarth orbit.

The concept that the space between the Earth and the Moon must be a vacuum was first proposed in the 17th century after scientists discovered thatair pressure decreased with altitude. The immense scale of outer space was grasped in the 20th century when the distance to theAndromeda Galaxy was first measured. Humans began the physical exploration of space later in the same century with the advent of high-altitudeballoon flights. This was followed by crewedrocket flights and, then, crewed Earth orbit, first achieved byYuri Gagarin of theSoviet Union in 1961. The economic cost of putting objects, including humans, into space is very high, limiting humanspaceflight tolow Earth orbit and theMoon. On the other hand,uncrewed spacecraft have reached all of the knownplanets in theSolar System. Outer space represents a challenging environment forhuman exploration because of the hazards ofvacuum andradiation.Microgravity has a negative effect on humanphysiology that causes bothmuscle atrophy andbone loss. (Full article...)

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Ariel as seen by Voyager 2 in 1986

Ariel is the brightest and third most massive of the 28 knownmoons of Uranus. Discovered on 24 October 1851 byWilliam Lassell, it is named for asky spirit in Alexander Pope'sThe Rape of the Lock and Shakespeare'sThe Tempest. Like its parent planet, Ariel orbits on its side, giving it an extreme seasonal cycle. As of 2011, almost all knowledge of Ariel derives from a singleflyby of Uranus performed by the spacecraftVoyager 2 in 1986, which managed to image 35% of the moon's surface. There are no plans at present to return to study the moon in more detail. AfterMiranda, Ariel is the second-smallest of Uranus's five round satellites, and the second-closest to its planet. Among the smallest of the Solar System's 19 known spherical moons (it ranks 14th among them in diameter), Ariel is composed of roughly equal parts ice and rocky material. Like all of Uranus's moons, Ariel probably formed from anaccretion disk that surrounded the planet shortly after its formation, and, like other large moons, it may bedifferentiated, with an inner core of rock surrounded by amantle of ice. Ariel has a complex surface comprising extensive cratered terrain cross-cut by a system ofscarps, canyons and ridges. The surface shows signs of more recent geological activity than other Uranian moons, most likely due totidal heating.

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Juno spacecraft with Jupiter in the background
Depiction of a planet with a rocky landscape orbiting the Alpha Centauri star system.
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