Ch. 3 The Rock Cyclenewburyparkhighschool.net/stillwagon/geoscp/Notes/03 rock cycle New.pdf• After...
Transcript of Ch. 3 The Rock Cyclenewburyparkhighschool.net/stillwagon/geoscp/Notes/03 rock cycle New.pdf• After...
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Ch. 3 The Rock Cycle
Columns of rock called
hoodoos dot Bryce
Canyon National Park.
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Magma - molten material deep
beneath Earth’s surface.
Lava - magma that reaches the surface.
***The melting of any rock type leads to the
production of magma.
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Formation• Igneous Rocks form when Magma or lava Cools.
• Cooling can occur either
below or above the surface!
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Formation of Igneous Rocks
Intrusive - magma hardens
beneath Earth’s surface (granite). Cools slowly
Have large crystals/grains
Extrusive - formed when lava
hardens at surface (pumice, rhyolite). Cools quickly
Have no/small crystals/grains
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Weathering - rocks broken down by water,
air & living things.
Sediments -weathered pieces
of Earth elements. Erosion - sediments are transported by
water, wind or gravity.
produces
Are moved by
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• Formed from particles or sediments that have been
transported & deposited by wind, water, ice, gravity.
• Over time, these particles become pressed or cemented together to form
rocks.
• Ex: sandstone
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Clastic
Clastic vs Chemical Sedimentary Rocks
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• After weathering and Erosion occur sediments must be deposited!
• Deposition - an agent of erosion (water, wind, ice, or gravity) loses
energy & drops sediments.
Formation of Sedimentary Rocks 1. Weathering, Erosion & Deposition
2. Compaction & Cementation
• Compaction - process that squeezes sediments by the weight of
overlying materials driving out water.
• Cementation – Solidification of sediments by the deposition of
dissolved minerals which act like a “glue.”
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• Formed when chemical reactions, heat, and/or pressure change
existing rocks into new rocks.
(physical & chemical properties usually quite different from original.)
meta- means change, morph means form.
(Ex: marble, schist, gneiss (pronounced “nice”)
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Agents of Metamorphism Heat - provides energy needed to drive chemical reactions.
Pressure - causes a more compact rock with greater density.
How does this happen ?
Contact metamorphism:
magma moves into rock
• Occurs near a body of magma
• Changes are driven by a rise in
temperature
Regional metamorphism:
large-scale deformation• Direct pressures occur during
mountain building
• Produces greatest volume of
metamorphic rock.
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Energy That Drives the Rock
Cycle Processes driven by heat from Earth’s
interior are responsible for forming
both igneous & metamorphic rocks.
Weathering & erosion are external
processes powered by energy from the
Sun, produce sedimentary rocks.
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IGNEOUS ROCKS
SEDIMENTS
SEDIMENTARY
ROCKS
METAMORPHIC
ROCKS
MAGMA
Weathering and erosionHeat and pressureMeltingCooling
Compaction,
cementation, and
lithification