• Earth
  • The third planet from the sun in our solar system. Allowed Values: Magnetosheath Magnetosphere Magnetosphere.Magnetotail Magnetosphere.Main Magnetosphere.Polar Magnetosphere.Radiation Belt Near Surface Near Surface.Atmosphere Near Surface.Auroral Region Near Surface.Equatorial Region Near Surface.Ionosphere Near Surface.Ionosphere.D-Region Near Surface.Ionosphere.E-Region Near Surface.Ionosphere.F-Region Near Surface.Ionosphere.Topside Near Surface.Mesosphere Near Surface.Plasmasphere Near Surface.Polar Cap Near Surface.South Atlantic Anomaly Region Near Surface.Stratosphere Near Surface.Thermosphere Near Surface.Troposphere Surface
Abstract from DBPedia
    Earth (otherwise known as the world, in Greek: Γαῖα Gaia, or in Latin: Terra) is the third planet from the Sun, the densest planet in the Solar System, the largest of the Solar System's four terrestrial planets, and the only astronomical object known to harbor life. According to radiometric dating and other sources of evidence, Earth formed about 4.54 billion years ago. Earth gravitationally interacts with other objects in space, especially the Sun and the Moon. During one orbit around the Sun, Earth rotates about its axis 366.26 times, creating 365.26 solar days or one sidereal year. Earth's axis of rotation is tilted 23.4° away from the perpendicular of its orbital plane, producing seasonal variations on the planet's surface within a period of one tropical year (365.24 solar days). The Moon is the Earth's only permanent natural satellite; their gravitational interaction causes ocean tides, stabilizes the orientation of Earth's rotational axis, and gradually slows Earth's rotational rate. Earth's lithosphere is divided into several rigid tectonic plates that migrate across the surface over periods of many millions of years. 71% of Earth's surface is covered with water. The remaining 29% is land mass—consisting of continents and islands—that together has many lakes, rivers, and other sources of water that contribute to the hydrosphere. The majority of Earth's polar regions are covered in ice, including the Antarctic ice sheet and the sea ice of the Arctic ice pack. Earth's interior remains active with a solid iron inner core, a liquid outer core that generates the Earth's magnetic field, and a convecting mantle that drives plate tectonics. Within the first billion years of Earth's history, life appeared in the oceans and began to affect the atmosphere and surface, leading to the proliferation of aerobic and anaerobic organisms. Since then, the combination of Earth's distance from the Sun, physical properties, and geological history have allowed life to evolve and thrive. Life arose on Earth by 3.5 billion years ago, though some geological evidence indicates that life may have arisen as much as 4.1 billion years ago. In the history of the Earth, biodiversity has gone through long durations of expansion but occasionally punctuated by mass extinction events. Over 99% of all species of life that ever lived on Earth are extinct. Estimates of the number of species on Earth today vary widely; most species have not been described. Over 7.3 billion humans live on Earth and depend on its biosphere and minerals for their survival. Humanity has developed diverse societies and cultures; politically, the world is divided into about 200 sovereign states.

    地球(ちきゅう、英: Earth, 羅: Terra)とは、人類など多くの生命体が生存する天体である。太陽系にある惑星の1つ。太陽から3番目に近く、表面に水、空気中に酸素を大量に蓄え、多様な生物が生存することを特徴とする惑星である。


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