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Chapter 6 Rocks Chapter 6 Rocks 6.2 Igneous Rocks 6.2 Igneous Rocks
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Chapter 6 Rocks 6.2 Igneous Rocks.

Jan 08, 2018

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Antony Fox
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Page 1: Chapter 6 Rocks 6.2 Igneous Rocks.

Chapter 6 RocksChapter 6 Rocks

6.2 Igneous Rocks6.2 Igneous Rocks

Page 2: Chapter 6 Rocks 6.2 Igneous Rocks.
Page 3: Chapter 6 Rocks 6.2 Igneous Rocks.

Igneous Rock FormationIgneous Rock Formation• Form from the cooling

of molten rock – Extrusive (volcanic)-

form at or near the surface from lava

– Intrusive (plutonic) – form under the surface from magma

Page 4: Chapter 6 Rocks 6.2 Igneous Rocks.

Igneous Rock FormationIgneous Rock Formation• Igneous rocks are

classified by mineral composition (mafic or felsic) and texture

• Texture – is the size, shape

and arrangement of grains (crystals)

Page 5: Chapter 6 Rocks 6.2 Igneous Rocks.

TextureTexture

• Grain or crystal size depends on:– Rate of cooling

• Fast = small• Slow = large

– Dissolved gasses• More = larger

– Order of solidification

Page 6: Chapter 6 Rocks 6.2 Igneous Rocks.

The Starting MaterialThe Starting Material• Magma is Classified as

Felsic, Mafic or and intermediate

• Felsic – Light colored– High silica magma with

abundance of quartz and feldspar.

– Thick slow flowing in molten state.

– Most intrusive rocks. – Acidic

Page 7: Chapter 6 Rocks 6.2 Igneous Rocks.

The Starting MaterialThe Starting Material• Mafic

– Dark colored, – Low silica

ferromagnesian magma

– More fluid than felsic magma.

– Most extrusive igneous rocks.

Page 8: Chapter 6 Rocks 6.2 Igneous Rocks.

Underground MagmaUnderground Magma• Magma can cool slow

or fast depending on where cooling occurs– Intrusive rocks cool

very slowly underground

– Result of slow cooling• Coarse (large) grains

Page 9: Chapter 6 Rocks 6.2 Igneous Rocks.

INTRUSIVE – large grains

GRANITE GABBRO

Page 10: Chapter 6 Rocks 6.2 Igneous Rocks.

At the SurfaceAt the Surface• Magma pouring onto

the surface is called lava– Extrusive igneous

rocks cool rapidly– Microscopic grains

or none at all

Page 11: Chapter 6 Rocks 6.2 Igneous Rocks.

EXTRUSIVE – fine grains

BASALT OBSIDIAN

Page 12: Chapter 6 Rocks 6.2 Igneous Rocks.

At the SurfaceAt the Surface• Porphyry

– Rocks that cool both underground and at the surface

– Results in large and small grains

Page 13: Chapter 6 Rocks 6.2 Igneous Rocks.

PORPHYRY – large grains embedded in fine grains

RHYOLITE PORPHYRY

Page 14: Chapter 6 Rocks 6.2 Igneous Rocks.

Igneous familiesIgneous families

• Grouped according to mineral composition

• Texture is determined where it cools – intrusive or extrusive– Each family can have coarse grained, fine

grained or glassy textures– Also can have vesicles

• Vesicles are gas cavities within the rock

Page 15: Chapter 6 Rocks 6.2 Igneous Rocks.

Igneous FamiliesIgneous Families• Granite family

– Felsic magma– Light colored– Quartz and Feldspar

• Coarse– Granite

• Fine– Rhyolite

• Glassy– Pumice and

Obsidian

• Gabbro Family– Mafic magma– Dark colored– Pyroxene and Olivine

• Coarse– Gabbro

• Fine– Basalt

• Vesicular– Scoria

Page 16: Chapter 6 Rocks 6.2 Igneous Rocks.

Igneous FamiliesIgneous Families• Diorite family

– Intermediate• Coarse

– Diorite• Fine

– Andesite

Page 17: Chapter 6 Rocks 6.2 Igneous Rocks.

IGNEOUS INTRUSIONSIGNEOUS INTRUSIONS• PLUTONS – A ROCK MASS THAT FORMS

WHEN MAGMA COOLS UNDER GROUND– DIKES– SILLS– LACOLITHS– VOLCANIC NECKS– BATHOLITHS – LARGEST OF ALL

PLUTONS, FORM THE CORES OF MOST MOUNTAINS

Page 18: Chapter 6 Rocks 6.2 Igneous Rocks.

Laccolith Volcanic neck

Sill Batholith

Stock

Dike

Page 19: Chapter 6 Rocks 6.2 Igneous Rocks.

DIKE

Page 20: Chapter 6 Rocks 6.2 Igneous Rocks.

SILL

Page 21: Chapter 6 Rocks 6.2 Igneous Rocks.

LACOLITH

Page 22: Chapter 6 Rocks 6.2 Igneous Rocks.

VOLCANIC NECK

Page 23: Chapter 6 Rocks 6.2 Igneous Rocks.

BATHOLITH