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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...)
Io is the innermost of the fourGalilean moons of the planetJupiter and, with adiameter of 3,642 kilometres (2,263 mi), thefourth-largest moon in theSolar System. It was named after the mythological character ofIo, a priestess ofHera who became one of the lovers ofZeus. With over 400 activevolcanoes, Io is the most geologically active object in the Solar System. This extreme geologic activity is the result of tidal heating from friction generated within Io's interior as it is pulled betweenJupiter and the other Galilean satellites—Europa,Ganymede andCallisto. Several volcanoes produce plumes ofsulfur andsulfur dioxide that climb as high as 500 km (300 mi) above the surface. Io's surface is also dotted with more than 100 mountains that have been uplifted by extensive compression at the base of the moon's silicate crust. Some of these peaks are taller than Earth'sMount Everest. Unlike most satellites in the outer Solar System, which are mostly composed of water-ice, Io is primarily composed of silicate rock surrounding a molten iron or iron sulfide core. Most of Io's surface is characterized by extensive plains coated with sulfur and sulfur dioxide frost. Io's volcanism is responsible for many of the satellite's unique features. Its volcanic plumes and lava flows produce large surface changes and paint the surface in various shades of yellow, red, white, black, and green, largely due toallotropes and compounds of sulfur. Numerous extensive lava flows, several more than 500 km (300 mi) in length, also mark the surface. The materials produced by this volcanism provide material for Io's thin, patchy atmosphere and Jupiter's extensivemagnetosphere. Io's volcanic ejecta also produce a largeplasma torus around Jupiter.




For a full schedule of launches and deep-space rendezvous, see2026 in spaceflight. |
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