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The Story of Rocks How did all of these rocks get here?

The Story of Rocks How did all of these rocks get here?

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Page 1: The Story of Rocks How did all of these rocks get here?

The Story of RocksThe Story of RocksHow did all of these

rocks get here?

Page 2: The Story of Rocks How did all of these rocks get here?

Rock typesRock typesRock types are based on the way the rocks formed!

• Igneous

• Sedimentary

• Metamorphic

Rock types are based on the way the rocks formed!

• Igneous

• Sedimentary

• Metamorphic

Page 3: The Story of Rocks How did all of these rocks get here?

IgneousIgneousIgneousIgneousThese rocks are formed from molten or These rocks are formed from molten or liquid rock.liquid rock.

Magma = liquid rock inside the EarthMagma = liquid rock inside the Earth

Lava = liquid rock on the surface.Lava = liquid rock on the surface.

Page 4: The Story of Rocks How did all of these rocks get here?

SedimentarySedimentaryThese rocks are made of small fragments of These rocks are made of small fragments of rock cemented togetherrock cemented together

The small fragments are broken down from The small fragments are broken down from larger rocks by wind, water, and other forces and larger rocks by wind, water, and other forces and carried away.carried away.

Later they are deposited, buried deeper and Later they are deposited, buried deeper and deeper until they are compacted into rock.deeper until they are compacted into rock.

Page 5: The Story of Rocks How did all of these rocks get here?

MetamorphicMetamorphicThese rocks start as igneous or These rocks start as igneous or sedimentary rocks.sedimentary rocks.

Rocks are changed by:Rocks are changed by:

1) heat1) heat

2) pressure2) pressure

3) chemical processes3) chemical processes

Page 6: The Story of Rocks How did all of these rocks get here?
Page 7: The Story of Rocks How did all of these rocks get here?
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SedimentaryRocks

MetamorphicRock

MagmaIgneous

Rock

Sediments

Rock CycleRock Cycle

Page 9: The Story of Rocks How did all of these rocks get here?

SedimentaryRocks

MetamorphicRock

MagmaIgneous

Rock

Sediments

Rock CycleRock Cycle

Page 10: The Story of Rocks How did all of these rocks get here?
Page 11: The Story of Rocks How did all of these rocks get here?
Page 12: The Story of Rocks How did all of these rocks get here?
Page 13: The Story of Rocks How did all of these rocks get here?
Page 14: The Story of Rocks How did all of these rocks get here?

Igneous Rocks

Page 15: The Story of Rocks How did all of these rocks get here?

Igneous RocksIgneous RocksThe main property of igneous rocks that allows us to identify which type of igneous rock that we have is – Texture

The texture is based on how large the crystals.

Crystal size depends on how fast the rock cooled (i.e. cooling rate)

Page 16: The Story of Rocks How did all of these rocks get here?

Igneous Rocks

Page 17: The Story of Rocks How did all of these rocks get here?

Igneous Rocks

Page 18: The Story of Rocks How did all of these rocks get here?

Igneous RocksIgneous Rocks

Page 19: The Story of Rocks How did all of these rocks get here?

Igneous RocksIgneous Rocks

Page 20: The Story of Rocks How did all of these rocks get here?

Igneous RocksIgneous Rocks

Page 21: The Story of Rocks How did all of these rocks get here?

Igneous RocksIgneous Rocks

Page 22: The Story of Rocks How did all of these rocks get here?

Igneous Rocks

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Page 24: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks

Page 25: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary RocksThe main property that allows us to group sedimentary rocks is the source of sediments.

Sediments can be:

1. Clastic

2. Chemical

3. Organic

The main property that allows us to group sedimentary rocks is the source of sediments.

Sediments can be:

1. Clastic

2. Chemical

3. Organic

Page 26: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Clastic – These sediments are composed of

fragments that can be up to a meter in diameter or so small that the fragments cannot be seen with the naked eye.

• Clastic – These sediments are composed of fragments that can be up to a meter in diameter or so small that the fragments cannot be seen with the naked eye.

Page 27: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary RocksChemical – These fragments were dissolved in water and usually form at the bottoms of rivers, lakes, seas, and oceans

Chemical – These fragments were dissolved in water and usually form at the bottoms of rivers, lakes, seas, and oceans

Page 28: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary RocksOrganic – These fragments are from organic material like animals and plantsOrganic – These fragments are from organic material like animals and plants

Page 29: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Common sedimentary features:

– Stratification (layering)– Ripple marks (from waves)– Cross bedding (different direction of beds)– Mud cracks (dried mud)– fossils (lithified animals and plants)– concretions

• Common sedimentary features:– Stratification (layering)– Ripple marks (from waves)– Cross bedding (different direction of beds)– Mud cracks (dried mud)– fossils (lithified animals and plants)– concretions

Page 30: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Stratification• Stratification

Page 31: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Ripple marks• Ripple marks

Page 32: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Cross bedding• Cross bedding

Page 33: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Mud Cracks• Mud Cracks

Page 34: The Story of Rocks How did all of these rocks get here?

Sedimentary RocksSedimentary Rocks• Fossils• Fossils

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Page 36: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic Rocks

Page 37: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic RocksMetamorphic rocks began their life as an igneous or sedimentary rock but underwent a physical change to become a new type of rock.

What causes the changes?1. Heat2 Pressure3. Chemicals

Page 38: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic RocksThere are two basic types of metamorphism:

1. Contact Metamorphism

2. Regional metamorphism

Page 39: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic RocksContact Metamorphism

Occurs when rocks near a magma chamber are exposed to high levels of heat but not melted

Page 40: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic RocksRegional Metamorphism

Occurs when rocks are exposed to tectonic pressure or heat.

Page 41: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic Rocks

Page 42: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic RocksHow do we classify metamorphic rocks since they have a wide range of compositions and origins?

Foliation!!

Definition: Visible parallel bands

(not layers)

Metamorphic rocks are foliated or unfoliated

Page 43: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic Rocks

Foliation occurs because the mineral grains are squished by the intense heat or pressure

Page 44: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic Rocks

Page 45: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic Rocks

Page 46: The Story of Rocks How did all of these rocks get here?

Metamorphic RocksMetamorphic RocksUnfoliated

Page 47: The Story of Rocks How did all of these rocks get here?
Page 48: The Story of Rocks How did all of these rocks get here?