Know that microwave radiation of a specific frequency is observed at all points in space around us and is known as cosmic microwave background radiation (CMBR)

6.1 The Earth – Rotation, Tilt and Seasons

1. Rotation

  • Earth rotates once about its axis every 24 h (≈ 86 400 s).
  • Result: the regular alternation of day and night.
  • Linear speed at the equator:


    v = 2πR / T ≈ 2π (6.37 × 10⁶ m) / 86 400 s ≈ 465 m s⁻¹

2. Axial tilt

  • Earth’s axis is tilted 23.5° to the plane of its orbit (the ecliptic).
  • The tilt, together with the orbital motion, causes the Sun’s apparent height in the sky to change over the year – giving the seasons.
  • When the Northern Hemisphere is tilted towards the Sun the days are longer and the Sun appears higher → summer; the opposite gives winter.

3. Seasons – quick exam checklist

  • Identify the season in a given hemisphere by the tilt direction.
  • Remember: the length of a year (orbital period) is 365 days 6 h 9 min ≈ 1 yr.
  • Key point for AO1: “The Earth’s rotation causes day/night, its tilt (23.5°) causes the seasons.”

Suggested diagram: Earth‑Sun geometry showing tilt in summer and winter (labelled 23.5°).


6.2 The Solar System

1. Overview

The Sun is at the centre of a system of eight planets, dwarf planets, moons, asteroids and comets. All objects move in (approximately) elliptical orbits due to the Sun’s gravity.

2. Planets – key facts (core IGCSE content)

#PlanetTypeMean distance from SunOrbital periodNotable feature
1MercuryTerrestrial0.39 AU88 dNo atmosphere, extreme temperature range
2VenusTerrestrial0.72 AU225 dThick CO₂ atmosphere, surface pressure ≈ 92 bar
3EarthTerrestrial1.00 AU365 dLife‑supporting, liquid water
4MarsTerrestrial1.52 AU687 dRed surface, thin CO₂ atmosphere
5JupiterGas giant5.20 AU12 yrLargest planet, strong magnetic field
6SaturnGas giant9.58 AU29 yrProminent ring system
7UranusIce giant19.2 AU84 yrRotates on its side (≈ 98° tilt)
8NeptuneIce giant30.1 AU165 yrStrong winds, dark methane clouds

3. Dwarf planets, moons, asteroids & comets

  • Dwarf planets – bodies that orbit the Sun and are massive enough to be round, but have not cleared their orbital zone. Examples: Pluto, Eris, Ceres.
  • Moons – natural satellites. Earth has one (the Moon); Jupiter has >70, Saturn >80, etc.
  • Asteroids – rocky bodies mainly in the asteroid belt between Mars and Jupiter.
  • Comets – icy bodies from the Kuiper Belt or Oort Cloud that develop a coma and tail when near the Sun.


6.3 Extension (Enrichment) – Cosmic Microwave Background Radiation (CMBR)

This material is not required for the core IGCSE exam but is useful for deeper understanding or extension work.

1. What is the CMBR?

  • A faint, uniform glow of electromagnetic radiation that fills the whole Universe.
  • Observed in every direction – the same at all points in space.
  • Remnant “after‑glow” of the hot, dense early Universe (the Big Bang).

2. Key observational facts

  • Discovered in 1965 by Arno Penzias and Robert Wilson using a horn antenna.
  • Has an almost perfect black‑body spectrum with an average temperature 2.725 K.
  • Peak wavelength (Wien’s law)


    λmax = b/T ≈ 2.898 × 10⁻³ / 2.725 ≈ 1.06 mm

  • Corresponding peak frequency


    νmax ≈ c/λmax ≈ 2.8 × 10¹¹ Hz ≈ 160 GHz

  • Falls in the microwave region of the electromagnetic spectrum (≈ 300 MHz – 300 GHz).
  • Isotropic to about one part in 10⁵; tiny anisotropies map the density fluctuations that later formed galaxies.

3. How is it detected?

  • Ground‑based radio telescopes with very sensitive microwave receivers (e.g., Atacama Cosmology Telescope).
  • High, dry sites or space platforms are chosen to minimise atmospheric absorption.
  • Satellites – COBE, WMAP and Planck – have measured the spectrum and temperature with high precision.

4. Numerical summary (quick revision)

PropertySymbol / ValueUnitsNotes
Average temperatureT = 2.725KCOBE FIRAS measurement
Peak wavelengthλmax ≈ 1.06mmWien’s law λmax=b/T
Peak frequencyνmax ≈ 160GHzc = λν
Temperature anisotropyΔT/T ≈ 10⁻⁵WMAP & Planck maps

5. Using Wien’s law – exam skill (AO2)

Wien’s displacement law for wavelength: λmax = b/T, where b = 2.898 × 10⁻³ m·K.

Example – Find λmax for T = 2.7 K

λmax = (2.898 × 10⁻³ m·K) / 2.7 K

≈ 1.07 × 10⁻³ m = 1.07 mm

Then obtain the frequency: νmax = c/λmax ≈ 3.00 × 10⁸ m s⁻¹ / 1.07 × 10⁻³ m ≈ 2.8 × 10¹¹ Hz (≈ 160 GHz).

6. Why it supports the Big‑Bang model (AO1)

  • The hot‑big‑bang theory predicted a relic radiation field; its discovery confirmed the prediction.
  • The observed black‑body spectrum matches the theoretical Planck curve for 2.7 K.
  • Measured anisotropies provide the seeds for later galaxy formation.

Suggested diagram: Black‑body curve peaking at ~160 GHz with the CMBR spectrum highlighted.


4 Practical Skills linked to Space Physics (AO3)

Activity 1 – Modelling Earth’s tilt and the seasons

  1. Materials: a bright lamp (Sun), a white ball (Earth), a protractor, a marker.
  2. Fix the ball on a stand so it can rotate. Tilt the axis to 23.5°.
  3. Rotate the ball once while keeping the lamp fixed; observe which hemisphere receives more light at different positions.
  4. Record observations and label the four seasons for each hemisphere.
  5. Safety: do not look directly at the lamp when it is on; keep the lamp away from flammable materials.

Activity 2 – Measuring the apparent diameter of the Moon

  1. Use a simple “pinhole camera” (a cardboard box with a small circular hole) and a sheet of white paper as a screen.
  2. During a clear night, point the camera at the Moon and measure the diameter of the projected image with a ruler.
  3. Calculate the Moon’s angular size using θ ≈ (image diameter / distance to screen) (radians) and convert to degrees (1 rad ≈ 57.3°).
  4. Compare your result with the accepted value ≈ 0.5°.
  5. Safety: never look directly at the Sun through the pinhole camera.

Link to assessment objectives

  • AO1 – Knowledge: recall facts about Earth’s rotation, tilt, planetary order, and (if chosen) the CMBR.
  • AO2 – Application: use formulas such as v = 2πr/T for Earth’s equatorial speed, or θ = s/D for angular size.
  • AO3 – Practical/experimental: design, carry out and analyse the two activities above; present results in a simple table or graph.


Exam Revision Checklist (IGCSE 0625 – Space Physics)

  • State that the Earth rotates once every 24 h → day/night.
  • State the axial tilt (23.5°) and explain how it produces the seasons.
  • List the eight planets in order, give one key feature for each, and know the difference between terrestrial and giant planets.
  • Define dwarf planets, moons, asteroids and comets.
  • Be able to calculate:

    • Linear speed at the equator (v = 2πR/T).
    • Orbital speed of the Moon (v = 2πr/T, with r ≈ 3.84 × 10⁸ m, T ≈ 2.36 × 10⁶ s → v ≈ 1.02 km s⁻¹).
    • Peak wavelength of a black‑body using Wien’s law (extension only).

  • Remember the practical safety points when working with bright lamps or the Sun.
  • If you attempt the extension material, be ready to state:

    • What the CMBR is and why it is called “microwave” (λ ≈ 1 mm, ν ≈ 160 GHz).
    • How its discovery supports the Big‑Bang theory.