Earth & Space - Materials from Earth - The Earth & its Resources - P6G15 |
Teacher's Guide
ES-D2.1 |
Learning outcomes
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1. Discuss with the children what they know about the Earth and what it is made of. |
Earth
Planet Earth was formed about 4.6 billion (4,600 million) years ago - as far as we know - from materials thrown out from the original explosion of the Universe - the Big Bang. We live on the crust of the Earth which is relatively thin (only 6 -70 km thick) like the skin of an orange. Underneath the crust of the Earth is the Mantle - a layer of rock about 3,000 km thick. In places the mantle is so hot the rock has melted to form a thick, treacle-like substance called magma. Underneath the mantle is the outer core - made of metal so hot that it is liquid. As the Earth rotates, this layer moves around very slowly producing the Earth’s magnetic field. At the centre of the Earth is the core. It is solid and made from nickel and iron. It is extremely hot - about 5000 degrees C. (background image) |
Activity
One of the best ways to teach the children about our planet is as follows :-
The children could investigate how the outer core of the Earth moves by half-filling a dish with water. Now make a disc from a margarine tub lid or thick card and use waterproof colours to make a design on it. Float the disc on the water then turn the dish slowly. Watch what happens to the floating disc. Investigate whether the disc turns at the same speed as the dish - slower or faster? What happens if you change the speed of the dish turning? (if the dish cannot be turned easily try placing it on a metal tray or turn a plate upside-down and put the dish on top - watch it does not fall off!) (The water in the dish does not rotate at the same speed as the dish. Water at the edges will be dragged by the dish and so will rotate but water further in slips on the outer water and so does not turn as fast) Extension Would you get the same effect with a thicker liquid? - try half set jelly then set jelly. This is similar to the way the layers of the Earth move at different speeds - the crust and mantle rotate but the inner core of thick viscous liquid moves more slowly. |