title: 18.3 intrusive activity page #: 108 date: 5/16/2013

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Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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Page 1: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

Title: 18.3 Intrusive ActivityPage #: 108

Date: 5/16/2013

Page 2: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

• 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.

Page 3: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

Igneous Rock: Rock formed by solidification of magma.

Page 4: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.

Page 5: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

• 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.

Page 6: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013
Page 7: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.

Page 8: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.

Page 10: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.

Page 12: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.

Page 14: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.

Page 16: Title: 18.3 Intrusive Activity Page #: 108 Date: 5/16/2013

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.)