Formation of the Solar System (Cambridge (CIE) IGCSE Physics)

Revision Note

Katie M

Written by: Katie M

Reviewed by: Caroline Carroll

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Formation of the Solar System

  • The 4 inner planets (nearest to the Sun):  

    • are rocky and small

    • have atmospheres (except for Mercury)

  • The 4 outer planets (furthest from the Sun):

    • are gaseous and large

    • are mostly composed of hydrogen and helium gas

The planets in the Solar System

planets-of-our-solar-system, IGCSE & GCSE Physics revision notes

The eight planets can be split into the four inner rocky planets and the four outer gas giants 

  • The differences between the inner and outer planets can be explained using the accretion model for the formation of the Solar System

Distribution of elements in the Solar System

  • The Sun and the planets in the Solar System formed from a cloud of dust and gas (nebula)

    • Gravity pulled this cloud together into a giant ball, which would eventually become the Sun

    • As the nebula collapsed, the Sun became denser and hotter

  • The Solar System then formed around 4.5 billion years ago

    • The planets formed from the remnants of the matter left over from the nebula that formed the Sun

    • The nebula contained many elements that were created during a supernova explosion in the distant past

  • As the early Sun became hotter, gaseous matter was pushed further out into the Solar System than solid matter

A nebula

Nebula, downloadable IGCSE & GCSE Physics revision notes

A nebula is an interstellar cloud of gas and dust 

Formation of the inner planets

  • In the hotter regions, closer to the Sun, the temperature was too high for lighter elements to exist in a solid state

    • Therefore, the inner planets formed from materials with high melting temperatures such as metals (e.g. iron)

    • The original nebula contained only a small proportion of heavy elements, so the inner planets could not grow as significantly as the outer planets

  • As a result, solids in the inner disc were pulled together by gravity to form solid planets

    • This is why the 4 planets nearest to the Sun (Mercury, Venus, Earth and Mars) are rocky and small 

Formation of the outer planets

  • In the cooler regions, further from the Sun, the temperature was low enough for the light molecules to exist in a solid state

    • Therefore, the outer planets formed from materials with low melting temperatures (e.g. hydrogen, helium, water and methane)

    • The original nebula contained a large proportion of light elements, so the outer planets were able to become exceptionally large

  • As a result, gases in the outer disc were pulled together by gravity to form gaseous planets

    • This is why the 4 planets furthest from the Sun (Jupiter, Saturn, Uranus and Neptune) are gaseous and large

Formation of the accretion disc

  • In the nebula, matter accreted

    • This means attractive gravitational forces between particles caused them to join together and grow into larger objects

  • As the cloud collapsed under gravitational forces

    • it began to spin faster

    • it became hotter

    • it formed an accretion disc

  • From the rotating accretion disc, the Sun and the planets emerged

    • The Sun formed at the centre

    • The planets formed in the accretion disc

Formation of the Solar System

6-1-3-accretion-model-cie-igcse-23-rn

The Solar System formed from a nebula with the Sun in the centre, then solid planets closer to the Sun and gaseous planets further away

Examiner Tips and Tricks

When writing about the formation of the Solar System, make sure you can:

  • State where solid and gaseous matter gathered in the Solar System

  • Explain how heavier elements became a part of the nebula

  • Describe the role of gravity in pulling matter together and the formation of an accretion disc

  • Explain the difference between the planets in terms of the accretion model

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Katie M

Author: Katie M

Expertise: Physics

Katie has always been passionate about the sciences, and completed a degree in Astrophysics at Sheffield University. She decided that she wanted to inspire other young people, so moved to Bristol to complete a PGCE in Secondary Science. She particularly loves creating fun and absorbing materials to help students achieve their exam potential.

Caroline Carroll

Author: Caroline Carroll

Expertise: Physics Subject Lead

Caroline graduated from the University of Nottingham with a degree in Chemistry and Molecular Physics. She spent several years working as an Industrial Chemist in the automotive industry before retraining to teach. Caroline has over 12 years of experience teaching GCSE and A-level chemistry and physics. She is passionate about creating high-quality resources to help students achieve their full potential.