Transcript

The Rock CycleRelationships among the major rock

groups

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Major Rock Groups• Igneous

– Formed from molten rock– Plutonic (intrusive):slow cooling and crystallization deep

w/in Earth’s crust– Volcanic (extrusion): quick cooling at the surface

• Sedimentary– Formed at the Earth’s surface– Clastic (Mineral Fragments or grains, clays)– Chemical (crystalline chemical/biochemical precipitate– Organic (remains of past organisms, typically shell-

bearing)• Metamorphic

– Changed by pressure, temperature and fluids.– Foliated visible bands– Nonfoliated no banding pattern

Fig. 2.9

MAGMA

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MAGMA

Crystallization

IGNEOUS

5

MAGMA

IGNEOUS

Plutonic

Crystallization

6

MAGMA

Volcanic

IGNEOUS

Plutonic

Crystallization

7

MAGMA

Volcanic

IGNEOUS

Plutonic

Uplift

Crystallization

Weathering

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

Uplift

Crystallization

Weathering SEDIMENT

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

Uplift

Crystallization

WeatheringErosion

Transport

Deposition

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

Uplift

Crystallization

WeatheringErosion

Transport

Deposition

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased Pressure & Temp

Crystallization

WeatheringErosion

Transport

Deposition

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased Pressure & Temp

MeltingCrystallization

WeatheringErosion

Transport

DepositionCan you see

any shortcuts?

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased P&T

MeltingCrystallization

WeatheringErosion

Transport

Deposition

• 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 the Earth’s surface as well as the Earth’s interior

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

In Conclusion…

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MAGMA

Volcanic

IGNEOUS

Plutonic

SEDIMENT

SEDIMENTARY

METAMORPHIC

UpliftBurial

Increased P&T

MeltingCrystallization

WeatheringErosion

Transport

Deposition

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