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Igneous, Metamorphic and sedimentary rocks

Igneous, Metamorphic and sedimentary rocks

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Physics

8th Grade

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Created by

Helen SMITH

Used 183+ times

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15 Slides • 15 Questions

1

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Types of rocks & how they form. ​

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  • Igneous rocks (from the Latin word for fire) form when hot, molten rock crystallizes and solidifies.

  • The rock melts deep within the Earth's crust at active plate boundaries or hot spots, and rises toward the surface.

  • Under the ground the molten rock is called magma - intrusive rocks are formed when magma solidifies below the surface

  • When the molten rock erupts it is called lava - extrusive rocks form from lava

Igneous rocks

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  • As the magma or lava cools crystals form

  • The appearance of the rock depends on the types of minerals present in the molten rock (shown are fluorite, misolite, bismuth and quartz) and the size of the crystals

  • Larger crystals form when the rock cools slowly, small crystals when it cools more quickly.

Crystals

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  • lava erupts at 1000 °C or more.

  • Since it is erupting into air (or the sea for underwater volcanoes) it cools down relatively quickly - hours to days

  • Therefore the minerals which crystalise as the rock cools are relatively small since they don't have time to grow bigger

  • For example, basalt is an extrusive rock with tiny crystals, generally only visible with a loupe (magnifying glass).

  • Basalt formed from underwater eruptions will generally cool quicker and have smaller crystals than basalt that cools on the ground

Extrusive rocks

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Frothy rocks

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​Pumice

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​Scoria

  • violent eruptions can occur which shoot out lava filled with gases.

  • The lava cools quickly, while it is still in the air, and traps the gases inside, producing rocks full of holes.

  • Two examples of this type of rock are pumice - a pale-coloured rock which can float on water; and scoria - a darker heavier rock, which contains iron and is generally found close to the volcano crater.

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  • Obsidian is a smooth, black glassy rock which forms when lava cools almost instantly.

  • It cools so quickly no crystals form

  • Very tiny air bubbles trapped in the rock can give it a coloured sheen.

Obsidian

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  • Magma that doesn't make it to the surface cools very slowly underground, forming intrusive rocks, sometimes called plutonic rock (from Pluto - Roman god of the underworld)

  • These can be exposed when the ground surface is eroded away

  • Large bodies of intrusive rock are called batholiths.

  • Intrusive rocks can have large crystals, which are visible by eye

Intrusive rock

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  • granite is a common intrusive rock made up of white, pink, grey, black and clear crystals

  • The 3 minerals it contains are quartz (clear to white or grey), feldspar (white or pink) and mica (black)

Granite

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Multiple Choice

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Formed by melting rock:

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magma

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sediments

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sedimentary rock

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intrusive igneous

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Multiple Choice

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Formed by cooling & solidification of magma
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Sedimentary

2

Metamorphic

3

Extrusive Igneous

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Intrusive Igneous

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Multiple Choice

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Formed by cooling & solidification of lava
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Sedimentary

2

Metamorphic

3

Extrusive Igneous

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Intrusive Igneous

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Multiple Choice

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Has large crystals because of slow cooling
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sedimentary rock

2

metamorphic rock

3

intrusive igneous rock

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extrusive igneous rock

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  • Are rocks formed from sediments

  • Sediments form when weathered rock is eroded by the wind, running water, the sea or glaciers and deposited in a new location.

  • Sediments buried under further layers of deposition are tightly packed by compaction

  • Chemicals dissolved in water can seep into the sediments, crystallising and gluing them together in a process called cementation.

  • Many sedimentary rocks form in this way.

Sedimentary rock

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  1. Deposition

  2. Compaction

  3. & 4. Cementation

Sedimentary rock formation

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Types of sedimentary rock

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​conglomerate

​sandstone

​siltstone and shale

  • Clasts move downhill due to erosion under the influence of gravity, getting smaller & smoother.

  • As running water slows down, larger pebbles and gravel fall out first, then sand and finally fine mud particles.

  • Conglomerate contains larger pebbles and cemented together with smaller grains.

  • Sandstone is formed from grains of sand.

  • Siltstone and shale from fine grains deposited from slow moving water.

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  • Limestone is a sedimentary rock that is formed from deposits of the remains of sea organisms such as shellfish and corals.

  • Coal forms from the remains of dead plants that are covered by water before they can decay and then buried by other sediments.

  • The weight of the sediments above compacts the plant material

  • Over millions of years compacting increases the temperature of the sediment and squeezes out the water, forming coal.

Organic sediments

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  • Plant and animals remains can also be deposited in sediment layers

  • When the organic materials are replaced by minerals, or decay leaving a void, this is called fossilisation.

  • Trace fossils occur when tracks and burrows are preserved

Fossils

Canowindra fish fossils

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Star-shaped holes from a soft-bodied sea creature

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Dinosaur trackways Winton QLD (credit: Chris Whitelaw)

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Multiple Choice

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Formed by weathering & erosion
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magma

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sediments

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sedimentary rock

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intrusive igneous

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Multiple Choice

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Formed by compacting & cementing of sediments
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Sedimentary

2

Metamorphic

3

Extrusive Igneous

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Intrusive Igneous

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  • Igneous and sedimentary rocks which are buried deep below the Earth’s surface experience huge pressures from the weight of rock and sediments above them.

  • Temperature increases by ~25°C every kilometre below the surface, so these rocks can also experience high temperatures.

  • This produces changes in composition and appearance of the minerals, in a process called metamorphism and the rocks are called metamorphic rocks.

Metamorphic rock

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  • Marble forms from limestone under heat and pressure.

  • Metamorphic rocks that are mainly the result of great pressure on the parent rock are characterised by parallel bands of different coloured minerals or flat, leaf-like layers. For example,

  • Slate forms from shale; because it is heavy and naturally forms a flat, smooth surface it is traditionally used in pool tables

  • Gneiss is formed from granite

Types of metamorphic rock

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Multiple Choice

Scientists divide rocks into groups based on how they form. The major groups of rocks are:

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sedimentary and igneous

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sedimentary, igneous and metamorphic

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metamorphic and sedimentary

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Multiple Choice

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Formed by heat and pressure
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Sedimentary

2

Metamorphic

3

Extrusive Igneous

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Intrusive Igneous

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Multiple Choice

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Has wavy bands.
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sedimentary rock

2

metamorphic rock

3

extrusive igneous rock

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intrusive igneous rock

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Multiple Choice

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A fossil can be formed when

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organic materials are replaced by minerals

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bones are preserved in sedimentary layers

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organic remains are metamorphosed by heat and pressure

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lava flows over plants or animals encasing them in rock.

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Multiple Choice

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Has small or no crystals because of rapid cooling
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sedimentary

2

metamorphic

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extrusive igneous

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intrusive igneous

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Multiple Choice

If heat and pressure inside the Earth cause a rock to melt, the material that formed would be
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Metamorphic

2

Magma

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Sedimentary

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Igneous

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Multiple Choice

You find a rock in which the grains are arranged in parallel bands of white and black crystals.  The rock is probably a(n)
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Igneous rock

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Sedimentary rock

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Metamorphic rock

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Extrusive rock

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Dropdown

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Fossils can only form in​ ​

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Labelling

The processes which form sedimentary rock are:

Drag labels to their correct position on the image
Deposition
Cementation
Compaction
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Types of rocks & how they form. ​

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