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Page 1: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

The Rock CycleThinking about relationships among the

major rock groups (Igneous, Sedimentary, and Metamorphic)

Page 2: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

Also see figure 1.12 on page 16 of the student textbook.

Page 3: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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Major Rock Groups• Igneous

– Formed from a melt (i.e. molten rock)– Plutonic (i.e. intrusive): slow cooling and crystallization

from a magma.– Volcanic (i.e. extrusion): quick cooling at the surface (lava).

• Sedimentary– Formed at the Earth’s surface.– Clastic (mineral fragments or grains, clays)– Chemical (crystalline chemical/biochemical precipitates)

• Metamorphic– Changed by pressure, temperature and hot chemical fluids.

Page 4: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

Fig. 2.9

MAGMA

Page 5: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Crystallization

IGNEOUS

Page 6: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

IGNEOUS

Plutonic

Crystallization

Page 7: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

Crystallization

Page 8: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

Uplift

Crystallization

Weathering

Page 9: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

Uplift

Crystallization

Weathering SEDIMENT

Page 10: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

Uplift

Crystallization

WeatheringErosion

Transport

Deposition

Page 11: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

Uplift

Crystallization

WeatheringErosion

Transport

Deposition

Lithification

Page 12: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

Remember

• Lithification =– Sediment turns to sedimentary rock by the processes of

compaction and cementation.

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased P&T

Crystallization

WeatheringErosion

Transport

Deposition

Lithification

Page 14: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

Remember

• Note that the process of melting is not involved or associated with metamorphism.

• Note that the grade of metamorphism could be increased (e.g., low-grade metamorphic rocks to high-grade metamorphic rocks) as the conditions of metamorphism are increased.

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased P&T

MeltingCrystallization

WeatheringErosion

Transport

Deposition

Can you see

any shortcuts?

Lithification

Page 16: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased P&T

MeltingCrystallization

WeatheringErosion

Transport

Deposition

Lithification

Page 17: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

• The rock cycle demonstrates the relationships among the three major rock groups.

• It is powered by the interior heat of the Earth as well as Earth’s momentum and the energy from the sun.

• It involves processes on Earth’s surface as well as the Earth’s interior.

• It connects the “hydrologic cycle” with the “tectonic cycle”.

In Conclusion…

Page 18: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)
Page 19: The Rock Cycle Thinking about relationships among the major rock groups (Igneous, Sedimentary, and Metamorphic)

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased P&T

MeltingCrystallization

WeatheringErosion

Transport

Deposition

Lithification


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