1. explain how internal energy of the earth causes matter to cycle through the magma and the solid...
TRANSCRIPT
Explain how internal energy of the Earth causes matter to cycle through the magma and the solid earth.
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D21
Igneous Formed from melted or molten rock
There are two types of igneous rock Plutonic or Intrusive
◦ This forms from magma which undergoes slow cooling and crystallization below the surface
Volcanic or Extrusive ◦ This forms from lava which undergoes quick
cooling at the surface
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Major Rock Groups
Sedimentary These rocks form from small pieces of
materials which collect, and over time become cemented together as rock
These are formed at the Earth’s surface
Two Types Clastic
◦ These form from mineral fragments or clays Chemical
◦ These form from crystals or biochemical precipitates
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Major Rock Groups
Metamorphic◦ These types of rocks have been changed by
pressure, temperature and fluids.
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Major Rock Groups
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MAGMA
Volcanic
IGNEOUS
Plutonic
SEDIMENT
Uplift
Crystallization
Cooling
Weathering SEDIMENT
Erosion & Transport & Pressure
WaterWindIce
Gravity
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MAGMA
Volcanic
IGNEOUS
Plutonic
SEDIMENT
SEDIMENTARY
Uplift
WeatheringErosion
Transport
Deposition
Lithification=
Cementation +
Compaction
Crystallization
Cooling
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MAGMA
Volcanic
IGNEOUS
Plutonic
SEDIMENT
SEDIMENTARY
METAMORPHIC
UpliftBurial
Increased P&T
Crystallization
Cooling
WeatheringErosion
Transport
Deposition
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MAGMA
Volcanic
IGNEOUS
Plutonic
SEDIMENT
SEDIMENTARY
METAMORPHIC
UpliftBurial
Increased P&T
MeltingCrystallization
Cooling
WeatheringErosion
Transport
DepositionCan you see
any shortcuts?
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MAGMA
Volcanic
IGNEOUS
Plutonic
SEDIMENT
SEDIMENTARY
METAMORPHIC
UpliftBurial
Increased P&T
Melting
Crystallization
Cooling
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
• It involves processes on the Earth’s surface as well as the Earth’s interior
In Conclusion…
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MAGMA
Volcanic
IGNEOUS
Plutonic
SEDIMENT
SEDIMENTARY
METAMORPHIC
UpliftBurial
Increased P&T
Melting
Crystallization
Cooling
WeatheringErosion
Transport
Deposition