Solar system

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AMANDEEP SINGH AMAN SINGH AABID SALIM AVINAAS YOGI ADITYA BASISTA PROJECT ON SOLAR SYSTEM FOR 9 TH – D BOYS

Transcript of Solar system

AMANDEEP SINGHAMAN SINGH AABID SALIM

AVINAAS YOGIADITYA BASISTA

PROJECT ON SOLAR SYSTEM FOR 9TH – D BOYS

SOLAR SYSTEM

The Solar System[a] consists of the Sun and the astronomical objects gravitationally bound in orbit around it, all of whichformed from the collapse of a giant molecular cloud approximately 4.6 billion years ago. Of the many objects that orbit the Sun, most of the mass is contained within eight relatively solitary planets[e] whose orbits are almost circular and lie within a nearly flat disc called the ecliptic plane. The four smaller inner

planets, Mercury, Venus, Earth and Mars, also called theterrestrial planets, are primarily composed of rock and metal. The four outer planets, the gas

giants, are substantially more massive than the terrestrials. The two largest, Jupiter and Saturn, are composed mainly of hydrogen and helium;

the two outermost planets, Uranus and Neptune, are composed largely of ices, such as water, ammonia and methane, and are often referred to

separately as "ice giants".

The Sun, which comprises nearly all the matter in the Solar System, is composed of roughly 98% hydrogen and helium.[10] Jupiter and Saturn, which comprise nearly all the remaining matter, possess atmospheres composed of roughly 99% of those same elements.[11][12] A composition

gradient exists in the Solar System, created by heat and light pressure from the Sun; those objects closer to the Sun, which are more affected by heat and light pressure, are composed of

elements with high melting points. Objects farther from the Sun are composed largely of materials with lower melting points.[13] The boundary in the Solar System beyond which those volatile substances could condense is known as the frost line, and it lies at roughly 4 AU from

the Sun.[14]

The objects of the inner Solar System are composed mostly of rock,[15] the collective name for compounds with high melting points, such as silicates, iron or nickel, that remained solid under almost all conditions in the protoplanetary nebula.[16] Jupiter and Saturn are composed mainly of gases, the astronomical term for materials with extremely low melting points and high vapor

pressure such asmolecular hydrogen, helium, and neon, which were always in the gaseous phase in the nebula.[16] Ices, like water, methane, ammonia, hydrogen sulfide and carbon

dioxide,[15] have melting points up to a few hundred kelvins, while their phase depends on the ambient pressure and temperature.[16] They can be found as ices, liquids, or gases in various

places in the Solar System, while in the nebula they were either in the solid or gaseous phase.[16] Icy substances comprise the majority of the satellites of the giant planets, as well as

most of Uranus and Neptune (the so-called "ice giants") and the numerous small objects that lie beyond Neptune's orbit.[15][17] Together, gases and ices are referred to as volatiles.[18]