title: 18.3 intrusive activity page #: 108 date: 5/16/2013
TRANSCRIPT
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Title: 18.3 Intrusive ActivityPage #: 108
Date: 5/16/2013
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• Students will be able to compare and contrast features formed from magma that solidifies near the surface of Earth with those that solidify deep underground.
• Students will be able to classify different types of intrusive rock bodies.
• Students will be able to describe how geologic processes result in intrusive rocks that appear at Earth’s surface.
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Igneous Rock: Rock formed by solidification of magma.
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Intrusive Activity
Pg. 514
Intrusive Activity: Main Idea: Magma that
solidifies below ground forms geologic features different from those formed by magma that cools at the surface.
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• Intrusive Activity
• Pg. 514
• Plutons: Not all magma emerges at surface of Earth.– Most volcanism happens below
Earth’s surface.– When magma cools minerals begin
to crystallize.– Crystallized magma forms intrusive
igneous rock bodies.
• Igneous Rock Bodies: – May be only a few cm thick and 100s
of meters long.– May be huge – 100s of km^3.
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Intrusive Activity
Pg. 515
Plutons: Huge intrusive igneous rocks 100s km^3 large.• Plutons may be uplifted at Earth’s
surface.
Batholith: Largest plutons. • Irregularly shaped.• Coarse grained igneous rocks 100
km^2+• Usually granite.• Take millions of years to form.
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Batholiths form within the earth.
Uplifting may expose batholithsTo Earth’s surface.
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Intrusive Activity
Pg. 515
Stocks: Smaller batholiths.
Both Batholiths and Stocks form between 5 and 30 km below Earth’s surface.
Both Batholiths and Stocks cut across older rocks.
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Stocks are smaller batholiths.
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Intrusive Activity
Pg. 515
Laccoliths: Lens-shaped pluton with a round top and flat bottom.• Form when rising magma causes
overlying rock to bend.• Largest is 16 km wide.
Sills: Parallel intrusions to rock layers.• May be only a few cm thick, or 100s
of meters thick.• Effects: 1) Lifts overlying rock up.
2) Metmorphoses surrounding rock.
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Laccoliths also form within the earth.Laccoliths are round on top and flat on bottom.
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Intrusive Activity
Pg. 516
Dikes: A pluton that cuts across pre-existing rock.• Form when magma invades cracks in
surrounding rocks.• Can be large or small.
Textures: Dikes and sills usually • Coarse-grained – Large crystals,
result from slow cooling deep in Earth’s surface.
• Fine-grained – Form close to Earth’s surface.
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Dikes cut across PRE-EXISTING rock. So they are always younger.
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Intrusive Activity
Pg. 517
Plutons and Tectonics: Plutons form from mountain
building.Convergent boundaries:Continental – Continental – Collision
forces crust down into the mantle where is melts, intrudes into overlying rock and cools – Forms batholiths.
Oceanic – Oceanic – When magma from a suducted plate does not rise all the way to the Earth’s surface. Example: Sierra Nevada Batholith in California and Yosemite National Park.
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When two plates converge and mountains crumple up, they also push material Into the mantle, where it melts. Melted material may cool to form plutons (Mountain Roots.)