E N C Y C L O P E D I A

 

Solar system

A generic solar system (or planetary system) consists of at least one star and various orbiting objects (such as asteroids, comets, moonss, and planets). The term originated to describe the plantary system around Sol, the Latin name for our sun. The planet Earth is located within our solar system, which is usually just called the Solar system; others being referred to as planetary systems to avoid confusion. This terminology will be used below.

Table of contents
1 Solar system objects
2 Origin and evolution of planetary systems
3 Orbit of the solar system
4 Discovery and exploration of the solar system
5 The solar system and other planetary systems
6 Attributes of Major Planets
7 Other facts
8 See also

Solar system objects

There are a wide variety of objects present in the solar system that fall under various different categories. In recent years many of these categories have been found to be less clear-cut than once thought. This encyclopedia employs the following divisions:

  • The Sun, a spectral class G2 star that contains 99.86% of system's mass.
  • The planets of the solar system are those nine bodies traditionally labelled as such; Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune and Pluto.
    • Sizeable objects that orbit these planets are moonss. For a complete listing, see that article.
    • dust and other small particles that orbit these planets form planetary rings
    • Space debris of artificial origin can be found in orbit around Earth.
    • The planets were originally formed from planetesimals, sub-planetary bodies that accreted together during the first years of the solar system and no longer exist. The name is also sometimes used to refer to asteroids and comets in general, or to asteroids below 10km in diameter
  • Asteroids are objects smaller than planets that lie roughly within the orbit of Jupiter and are composed in significant part by non-volatile minerals. They are subdivided into the near-Earth asteroids, which are further subdivided into Atens, Apolloss, and Amors.
    • Asteroid moons are asteroids that orbit larger asteroids. They are not as clearly distinguished as planetary moons, sometimes being almost as large as their partner.
    • Trojan asteroids are located in either of Jupiter's L4 or L5 points, though the term is also sometimes used for asteroids in any other planetary Lagrange point as well.
    • Meteoroids are asteroids roughly boulder-sized or smaller, all the way down to dust. Dust within the solar system is responsible for the phenomenon of zodiacal light.
  • Comets, which are composed largely of volatile ices and whose orbits are highly eccentric, generally having a periapsis within the orbit of the inner planets and an apoapsis out past Pluto. Short-period comets exist with apoapses closer than this, however, and old comets that have had most of their volatiles driven out by solar warming are often categorized as asteroids. Some comets with hyperbolic orbits may also originate outside the solar system.
  • Centaurss, icy comet-like bodies that have less eccentric orbits that remain in the region between Jupiter and Neptune.
  • Trans-Neptunian objects, icy bodies whose mean orbital radius lies beyond Neptune's. These are further subdivided:
    • Kuiper belt objects, with orbits lying between 30 and 50 AU. Thought to be the origin for short-period comets. Pluto is sometimes classified as a Kuiper belt object in addition to being a planet, and a class of Kuiper belt objects with Pluto-like orbits are called Plutinos. The remaining Kuiper belt objects are classified as Cubewanos in the main belt and scattered disk objects in the outer fringes.
    • Oort cloud objects, currently hypothetical, with orbits lying between 50,000 and 100,000 AU. This region is thought to be the origin of long-period comets.
  • Small quantities of dust are present throughout the solar system, and is responsible for the zodiacal light. Some of the dust is likely interstellar dust from outside the solar system.

Origin and evolution of planetary systems

Planetary systems are generally believed to form as part of the same process which results in star formation; although, some argue that systems are formed by some kind of accidental "stellar near-collison". The more common theory argues that the objects of a planetary system developed from a solar nebula.

Orbit of the solar system

The solar system is part of the Milky Way galaxy, a spiral galaxy with a diameter of about 100,000