The Oort cloud is a theoretical cloud of predominantly icy planetesimals proposed to surround the Sun. It is divided into two regions: a disc-shaped inner OortCloud and a spherical outer Oortcloud. The outer limit of the Oort Cloud defines the cosmographic boundary of the Solar System and the extent of the Sun’s Hill sphere. It may be the source of all long-period and Halley-type comets entering the inner Solar System.
About Oort cloud in brief

The cloud is only loosely bound to the solar system, and thus is easily affected by gravitational pull both of passing stars and of the Milky Way itself. These forces occasionally dislodge comets from their orbits within the cloud and send them toward the inner solar System. There are two main classes of comet: short-period comets and long- Period comets. All long- periods comets have very large orbits, on the order of thousands of au, and appear from every direction in the sky. Those relatively rare comets with orbits of about 10,000 au have probably gone through one or more orbits through the Solar system and have had their orbits drawn inward by the gravity of the planets. Some estimates place the outer boundary at between 100,000 and 50,000 au. The region can be subdivided into a sphere-shaped outer Oorting cloud of 20,000–50,000au, and a torus-shaped inward Oort clouds of 2,00,000 – 20,00 au. The outer cloud supplies the long-series comets to inside the orbit of Neptune. It also provides a source of new comets, as the latter’s numbers are gradually depleted as the cloud continues to continue to grow. It was thought it was more massive than previously thought, but better knowledge of its distribution has led to a lower estimate of its size.
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This page is based on the article Oort cloud published in Wikipedia (as of Dec. 06, 2020) and was automatically summarized using artificial intelligence.






