What shape is the Earth, how big is it, and what is it made of inside?
The shape, size and internal structure of the Earth: the oblate spheroid, the mean diameter of 13000 km, and the crust, mantle, outer core and inner core.
A focused answer to Edexcel GCSE Astronomy statements 1.1 to 1.3, covering why the Earth is an oblate spheroid, how to use its mean diameter of 13000 km, and the four major internal divisions (crust, mantle, outer core and inner core) and their features.
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What this dot point is asking
Edexcel statements 1.1 to 1.3 want you to know the shape of the Earth (an oblate spheroid), to use information about its mean diameter of 13000 km in calculations, and to describe the four major internal divisions of the Earth (crust, mantle, outer core and inner core) and their features.
The shape of the Earth
The difference is small (the equatorial diameter is only about 43 km larger than the polar diameter), so the Earth looks spherical in photographs, but "oblate spheroid" is the precise answer the mark scheme wants. Calling it a perfect sphere is the classic lost mark. The same flattening happens to other rotating bodies, and faster-spinning planets such as Jupiter and Saturn are visibly more oblate.
The size of the Earth
The mean diameter is a single average value used because the Earth is not perfectly round. Questions often ask you to combine it with to get the circumference, or to take a ratio with the Moon's mean diameter of 3500 km (so the Earth is about 3.7 times wider than the Moon) or the Sun's mean diameter of . Working in standard form, .
The internal structure of the Earth
The layers differ in state and composition: rocky crust and mantle outside, metallic iron and nickel cores inside. The boundary between solid inner core and liquid outer core is set by pressure, not just temperature, which is why the deeper inner core is solid even though it is hotter. The liquid outer core, being a moving conductor, is the source of the Earth's magnetic field, which links forward to the magnetosphere in solar astronomy.
How Edexcel examines this
This is naked-eye Paper 1 content and a reliable source of recall and short-calculation marks. The shape question rewards naming the oblate spheroid and linking the equatorial bulge to rotation; do not write "sphere" alone. The diameter is given on the data sheet, so calculations test whether you can use it: expect circumference (), radius (), or a ratio comparing the Earth with the Moon or Sun, sometimes in standard form. The structure question rewards the four divisions in the correct order with their states, especially the liquid outer core and solid inner core. A frequent synoptic link is to the magnetosphere (the moving liquid outer core generates the magnetic field) in Topic 10, so be ready to connect the inner structure to that. Keep the answers precise and ordered, and watch the units (kilometres throughout).
Try this
Q1. State the precise name for the shape of the Earth. [1 mark]
- Cue. An oblate spheroid (flattened at the poles, bulging at the equator).
Q2. Name the four major internal divisions of the Earth in order from the surface. [2 marks]
- Cue. Crust, mantle, outer core, inner core.
Exam-style practice questions
Practice questions written in the style of Pearson Edexcel exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Edexcel 1AS0 20222 marksDescribe the shape of the Earth, and explain why it has this shape rather than being a perfect sphere.Show worked answer →
The Earth is an oblate spheroid, meaning it is a sphere that is slightly flattened at the poles and bulges at the equator (1 mark). It has this shape because the Earth rotates on its axis, and the spin causes a bulge at the equator where the rotation speed is greatest (1 mark). Markers reward naming the shape as an oblate spheroid and linking the equatorial bulge to the Earth's rotation. A common error is to call the Earth a perfect sphere, which loses the mark.
Edexcel 1AS0 20213 marksThe mean diameter of the Earth is 13000 km. Calculate the approximate circumference of the Earth around the equator. Use circumference = pi x diameter.Show worked answer →
Use with the mean diameter (1 mark for the correct method). Substituting gives (1 mark). This works out to (accept about ) (1 mark). Markers reward selecting the right equation, correct substitution of the mean diameter, and a circumference of roughly 41000 km. Working in standard form () is acceptable.
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