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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]
Solar system

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Solar system

  • 1. PROJECT ON SOLAR SYSTEM FOR 9TH – D BOYS
  • 3. 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".
  • 4.
  • 5.
  • 6. 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]