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Published byBenedict Crawford Modified over 9 years ago
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Do now! Can you continue the questions on pages 84 and 85?
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Last lesson Chemical and physical weathering
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Chemical weathering Rain is slightly acidic as it contains substances dissolved from the air. It can react with rock, dissolving it.
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Chemical weathering Some rocks are dissolved more by acid rain than others Limestone “pavement”
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Physical weathering Rocks can be weathered by physical changes
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Physical weathering When rocks are hot they expand, and when they cool they contract. Repeated changes cause the rock to crack, often causing rock to peel off. Sometimes called “onion-skin weathering”
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Physical weathering Freeze-thaw weathering is another example You now know all about freeze-thaw weathering
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Today’s lesson Transport of weathered rock Soil Rock cycle
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Transport
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Rock falls to the bottom of rock faces and may be transported away by fast moving streams.
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Abrasion The rocks in the stream bed rub against each other and wear away. This is abrasion.
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Sediment The bits of rock in the stream bed are called sediment.
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Deposit Smaller rock fragments are carried further than large ones, eventually being deposited on the bottom in slow water.
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Let’s try some questions! Stick the sheet in and fill in the gaps. You have 8 minutes!
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What is soil?
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A mixture of stones, smaller rock particles (sand) and humus (remains of dead plants and animals)
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Copy?! Can you copy the table on page 91?
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The Rock Cycle Can you read page 100 very carefully?
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The Rock Cycle Can you copy the diagram on page 100?
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