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Do now! Can you complete the experiment sheet we did last lesson? Interesti ng scientist
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Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Dec 16, 2015

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Mariano Rake
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Page 1: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Do now!Can you complete the experiment sheet we

did last lesson?Interesting scientist

Page 2: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Last lesson

• Investigating the suitability of rocks for different purposes

Page 3: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Which rock would make the best statue?

What did you decide?

Page 4: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Today’s lesson

• Three main rock types

Page 5: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Three main rock types

Igneous

Page 6: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Three main rock types

Sedimentary

Page 7: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Three main rock types

Metamorphic

Page 8: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

From the latin “ignis” meaning fire

Page 9: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Formed by the cooling of lava or magma

What’s the difference?

Page 10: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Made from crystals

Page 11: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Quick cooling forms small crystals, slow cooling forms large crystals

Page 12: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Basalt is formed by quickly cooling lava

Page 13: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Pumice is formed from lava that contains a lot of gas. It can float!

Page 14: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Obsidian is like dark glass formed when molten silica cools quickly!

Page 15: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Igneous rocks

Granite is made from magma that cools slowly underground

Page 16: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Page 17: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Sediments like sand and mud build up at the bottom of oceans and rivers

Page 18: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Over millions of years pressure from successive layers forms these into sedimentary rocks

Page 19: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Layers!

Page 20: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Animals and plants can be trapped in the sediments and can form fossils

Page 21: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Sandstone is made from sand grains stuck together

Page 22: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Limestone is made from the mineral calcite which came from the beds of evaporated seas and lakes and from sea animal shells.

Page 23: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Conglomerate rocks are made up of large sediments like pebbles. The sediment is cemented together with dissolved minerals.

Page 24: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Sedimentary rocks

Shale are formed from clay and mud that is compacted together by pressure.

Page 25: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

Page 26: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

Metamorphic rocks are rocks that have "morphed" into another kind of rock.

Page 27: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

These rocks were once igneous or sedimentary rocks. The rocks are under tons of pressure, which causes heat build up, and this causes them to change.

Page 28: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

These often also contain thin layers and crystals but are much harder than sedimentary rocks

Page 29: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

Marble is limestone that has been metamorphised

Page 30: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

Slate is metamorphised shale

Page 31: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Metamorphic rocks

Anthracite coal

Page 32: Do now! Can you complete the experiment sheet we did last lesson? Interesting scientist.

Brain-map

Mr Porter is now going to put these slides on a loop so you can brain map them!