The Solar System was formed approximately 4.6 billion years ago and consists of the Sun, planets, dwarf planets and other astronomical objects bound in its orbit. The formation was caused by the collapse of a giant molecular cloud, the mass at the centre collecting to form the Sun and a flat disk of dust around it which the planets and other bodies would eventually be formed from.
Earth, our home planet, is the only planet in its solar system known to harbor life. All of the things we need to survive are provided under a thin layer of atmosphere that separates us from the (almost) uninhabitable void of space.
Mars is a small rocky body once thought to be very Earthlike. Like the other terrestrial planets its surface has been changed by volcanism, impacts from other bodies, movements of its crust, and atmospheric effects such as dust storms.
The vast majority of asteroids in the solar system are found in a region of the solar system out beyond Mars. They form the Asteroid Belt.
The most massive planet in our solar system, with four planet-size moons and many smaller satellites, Jupiter forms a kind of miniature solar system. Jupiter resembles a star in composition.
Mars is a small rocky body once thought to be very Earthlike. Like the other terrestrial planets its surface has been changed by volcanism, impacts from other bodies, movements of its crust, and atmospheric effects such as dust storms.
Once considered one of the blander-looking planets, Uranus has been revealed as a dynamic world with some of the brightest clouds in the outer solar system and 11 rings.
The eighth planet from the sun, Neptune was the first planet located through mathematical predictions rather than through regular observations of the sky.
The Kuiper Belt (sometimes referred to as the Kuiper-Edgeworth Belt) is an area of the outer solar system that is estimated to stretch across 20 astronomical units (AU) of space.
The Oort Cloud is an extended shell of icy objects that exist in the outermost reaches of the solar system. The Oort Cloud is roughly spherical, and is thought to be the origin of most of the long-period comets that have been observed.
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