Earth Science/Geology Mr. Traeger. The Rock Cycle The rock cycle is directly related to the theory of ___________, the idea that the Earth’s tectonic.

Earth Science/GeologyEarth Science/Geology

Mr. TraegerMr. Traeger

The Rock CycleThe Rock Cycle

The rock cycle is directly related to the theory of ___________, the idea that the Earth’s tectonic plates are continuously moving.

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary Ro

ck

The Rock CycleThe Rock Cycle

The rock cycle is directly related to the theory of plate tectonics, the idea that the Earth’s tectonic plates are continuously moving.

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary Ro

ck

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary Ro

ck

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary Ro

ck

4

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary Ro

ck

4

5

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary Ro

ck

4

54

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1 2

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1 2

3

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1 2

33

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1 2

33

4

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1 2

33

4

3

Number Process

1 Heating (melting)

2 Cooling and solidification (Crystallization)

3 Heat and Pressure

4 Weathering and Erosion

5 Cementation and Compaction (Lithification)

Igneous Rocks

Sediments

Metamorphic Rock

Magma/Lava Sedimentary

Rock

4

54

1

1 2

33

4

31

Igneous Rocks: Basics

_____________ rocks form when ____________ or ___________ cools, crystallizes, and solidifies.

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Igneous Rocks: Basics

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

______________ is magma that reaches the surface of the Earth.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are _______________ and ______________.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

________________ igneous rocks form deep within the Earth. These rocks are also referred to as __________________.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

Intrusive igneous rocks form deep within the Earth. These rocks are also referred to as plutonic.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

Intrusive igneous rocks form deep within the Earth. These rocks are also referred to as plutonic.

________________ igneous rocks form at the surface of the Earth. These rocks are also referred to as __________________.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

Intrusive igneous rocks form deep within the Earth. These rocks are also referred to as plutonic.

Extrusive igneous rocks form at the surface of the Earth. These rocks are also referred to as volcanic.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

Intrusive igneous rocks form deep within the Earth. These rocks are also referred to as plutonic.

Extrusive igneous rocks form at the surface of the Earth. These rocks are also referred to as volcanic.

The process where orderly patterns form when __________ cools is called _____________________.

Igneous Rocks: Basics

Igneous rocks form when magma or lava cools, crystallizes, and solidifies.

Lava is magma that reaches the surface of the Earth.

Two basic types of igneous rocks are intrusive and extrusive.

Intrusive igneous rocks form deep within the Earth. These rocks are also referred to as plutonic.

Extrusive igneous rocks form at the surface of the Earth. These rocks are also referred to as volcanic.

The process where orderly patterns form when magma cools is called crystallization.

Texture

_____________ cooling forms ___________, coarse textured crystals.

Slow cooling forms visible, coarse textured crystals.

Texture

Slow cooling forms visible, coarse textured crystals.

_____________ cooling forms ___________, fine textured crystals.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main ___________ found in _____________.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by __________ and ___________.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

____________ is the most important characteristic for determining where an igneous rock formed. The rate of cooling determines this.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

Texture is the most important characteristic for determining where an igneous rock formed. The rate of cooling determines this.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

Texture is the most important characteristic for determining where an igneous rock formed. The rate of cooling determines this.

An igneous rock is _______________ if it has a fine-grained texture.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

Texture is the most important characteristic for determining where an igneous rock formed. The rate of cooling determines this.

An igneous rock is aphanitic if it has a fine-grained texture.

Texture

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

Texture is the most important characteristic for determining where an igneous rock formed. The rate of cooling determines this.

An igneous rock is aphanitic if it has a fine-grained texture.

Texture

Gas bubbles trapped in solidifying lava are known as _____________.

Slow cooling forms visible, coarse textured crystals.

Fast cooling forms invisible, fine textured crystals.

Silicon, oxygen, aluminum, sodium, potassium, calcium, iron, and magnesium are the main elements found in minerals.

Igneous rocks are usually classified by composition and texture.

Texture is the most important characteristic for determining where an igneous rock formed. The rate of cooling determines this.

An igneous rock is aphanitic if it has a fine-grained texture.

Texture

Gas bubbles trapped in solidifying lava are known as vesicles.

Texture

An igneous rock is _______________ if it has a coarse-grained texture.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

An igneous rock with very large crystals embedded within smaller crystals has a _________________ texture.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

An igneous rock with very large crystals embedded within smaller crystals has a porphyritic texture.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

An igneous rock with very large crystals embedded within smaller crystals has a porphyritic texture.

Very rapid cooling can form a ___________ texture, as in obsidian.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

An igneous rock with very large crystals embedded within smaller crystals has a porphyritic texture.

Very rapid cooling can form a glassy texture, as in obsidian.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

An igneous rock with very large crystals embedded within smaller crystals has a porphyritic texture.

Very rapid cooling can form a glassy texture, as in obsidian.

The ________________ of an igneous rock will influence ___________.

Texture

An igneous rock is phaneritic if it has a coarse-grained texture.

An igneous rock with very large crystals embedded within smaller crystals has a porphyritic texture.

Very rapid cooling can form a glassy texture, as in obsidian.

The composition of an igneous rock will influence texture.

Composition

Igneous rocks have varying ______________ content.

Composition

Igneous rocks have varying mineral content.

Composition

Igneous rocks have varying mineral content.

A scientist named ____________ found that minerals with higher melting points ______________ before minerals with lower melting points. This is the basis for ____________ ____________ __________.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

A _______________ reaction series occurs when each mineral has a different crystal structure.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

A discontinuous reaction series occurs when each mineral has a different crystal structure.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

A discontinuous reaction series occurs when each mineral has a different crystal structure.

A _______________ reaction series is when calcium-rich crystals react with sodium ions to become more sodium rich.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

A discontinuous reaction series occurs when each mineral has a different crystal structure.

A continuous reaction series is when calcium-rich crystals react with sodium ions to become more sodium rich.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

A discontinuous reaction series occurs when each mineral has a different crystal structure.

A continuous reaction series is when calcium-rich crystals react with sodium ions to become more sodium rich.

__________________ ___________________ is the process of creating more than one rock type from the same magma. This proves that a single magma form many different types of igneous rocks.

Composition

Igneous rocks have varying mineral content.

A scientist named Norman L. Bowen found that minerals with higher melting points crystallized before minerals with lower melting points. This is the basis for Bowen’s Reaction Series.

A discontinuous reaction series occurs when each mineral has a different crystal structure.

A continuous reaction series is when calcium-rich crystals react with sodium ions to become more sodium rich.

Magmatic differentiation is the process of creating more than one rock type from the same magma. This proves that a single magma form many different types of igneous rocks.

Classification

Light colored rocks such as granite are known as ______________. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Intermediate colored rocks such as diorite have moderate amounts of the minerals biotite, amphibole, and pyroxene.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Intermediate colored rocks such as diorite have moderate amounts of the minerals biotite, amphibole, and pyroxene.

Dark colored rocks rich in iron and magnesium such as gabbro are known as _____________. These rocks are rich in the minerals plagioclase, biotite, amphibole, pyroxene, and olivine.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Intermediate colored rocks such as diorite have moderate amounts of the minerals biotite, amphibole, and pyroxene.

Dark colored rocks rich in iron and magnesium such as gabbro are known as mafic. These rocks are rich in the minerals plagioclase, biotite, amphibole, pyroxene, and olivine.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Intermediate colored rocks such as diorite have moderate amounts of the minerals biotite, amphibole, and pyroxene.

Dark colored rocks rich in iron and magnesium such as gabbro are known as mafic. These rocks are rich in the minerals plagioclase, biotite, amphibole, pyroxene, and olivine.

Extremely dark rocks such as peridotite/dunite with low contents of silica and high contents of iron and magnesium are known as _____________________.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Intermediate colored rocks such as diorite have moderate amounts of the minerals biotite, amphibole, and pyroxene.

Dark colored rocks rich in iron and magnesium such as gabbro are known as mafic. These rocks are rich in the minerals plagioclase, biotite, amphibole, pyroxene, and olivine.

Extremely dark rocks such as peridotite/dunite with low contents of silica and high contents of iron and magnesium are known as ultramafic.

Classification

Light colored rocks such as granite are known as felsic. These rocks are rich in the minerals quartz and orthoclase/plagioclase feldspar.

Intermediate colored rocks such as diorite have moderate amounts of the minerals biotite, amphibole, and pyroxene.

Dark colored rocks rich in iron and magnesium such as gabbro are known as mafic. These rocks are rich in the minerals plagioclase, biotite, amphibole, pyroxene, and olivine.

Extremely dark rocks such as peridotite/dunite with low contents of silica and high contents of iron and magnesium are known as ultramafic.

The following chart, reproduced from the course textbook on page 62, is how igneous rocks are classified.

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) Peridotite

Aphanitic (fine-grained) Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) granite Peridotite

Aphanitic (fine-grained) Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) granite diorite Peridotite

Aphanitic (fine-grained) Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) granite diorite gabbro Peridotite

Aphanitic (fine-grained) Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) granite diorite gabbro Peridotite

Aphanitic (fine-grained) rhyolite Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) granite diorite gabbro Peridotite

Aphanitic (fine-grained) rhyolite andesite Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Classification

Granitic (Felsic) Andesitic(Intermediate)

Basaltic(Mafic)

Ultramafic

Phaneritic (coarse-grained) granite diorite gabbro Peridotite

Aphanitic (fine-grained) rhyolite andesite basalt Komatite

Major Mineral Composition QuartzK-FeldsparNa-Feldspar

AmphiboleIntermediate plagioclase

Ca-FeldsparPyroxene

OlivinePyroxene

Minor Mineral Composition MuscoviteBiotiteAmphibole

PyroxeneAmphiboleBiotite

OlivineAmphibole

Ca-Feldspar

Rock ColorBased on % dark minerals

Light-colored< 15% dark minerals

Medium-colored15-40% dark minerals

Dark grey to black> 40% dark minerals

Dark-green to black~ 100% dark minerals

Formation of Sedimentary Rock

Although Earth’s crust is primarily _______________ rock, most of the crust’s surface is covered by ___________________ rock.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through _____________________ and ___________________________ of layers of sediment.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Most sedimentary rocks form in __________________ environments.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Most sedimentary rocks form in aquatic environments.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Most sedimentary rocks form in aquatic environments.

______________________ is when rock fragments settle in a particular area.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Most sedimentary rocks form in aquatic environments.

Deposition is when rock fragments settle in a particular area.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Most sedimentary rocks form in aquatic environments.

Deposition is when rock fragments settle in a particular area.

In a stream, __________________ is first to be deposited, then _______________, then ____________________.

Formation of Sedimentary Rock

Although Earth’s crust is primarily igneous rock, most of the crust’s surface is covered by Sedimentary rock.

In most simple terms, sedimentary rocks occur through cementation and compaction of layers of sediment.

Most sedimentary rocks form in aquatic environments.

Deposition is when rock fragments settle in a particular area.

In a stream, boulders are first to be deposited, then gravel, then sand/silt.

Formation of Sedimentary Rock

Rock particles become ________________ when they bump in to each other in a stream.

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

_________________ rock

_________________ rock

__________________ rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Common examples are: Common examples are:

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

Clastic rock _________________ rock

__________________ rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Common examples are: Common examples are:

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

Clastic rock _________________ rock

__________________ rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Sandstone and Shale

Common examples are: Common examples are:

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

Clastic rock Chemical Evaporite rock __________________ rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Sandstone and Shale

Common examples are: Common examples are:

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

Clastic rock Chemical Evaporite rock __________________ rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Sandstone and Shale

Common examples are: Salt and Tufa

Common examples are:

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

Clastic rock Chemical Evaporite rock Organic or Bioclastic rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Sandstone and Shale

Common examples are: Salt and Tufa

Common examples are:

Formation of Sedimentary Rock

Rock particles become rounded when they bump in to each other in a stream.

Sedimentary rocks are broken down into 3 groups.

Clastic rock Chemical Evaporite rock Organic or Bioclastic rock

Fragments of other rocks that are cemented and compacted together create this type of rock.

Rocks that are formed when minerals dissolved in water precipitate, or fall out of solution, form this type of rock.

Rocks that are formed from sediments consisting of the remains of plants and animals.

Common examples are: Sandstone and Shale

Common examples are: Salt and Tufa

Common examples are: Chalk, Fossiliferous Limestone, Bituminous Coal

Features of Sedimentary Rock

The single most characteristic feature of sedimentary rocks is __________________ the arrangement of visible layers.

Features of Sedimentary Rock

The single most characteristic feature of sedimentary rocks is stratification, the arrangement of visible layers.

Features of Sedimentary Rock

The single most characteristic feature of sedimentary rocks is stratification, the arrangement of visible layers.

The ______________ layers of sedimentary rock are always on the bottom of a column. The _______________ layers are always on the top of a column.

Features of Sedimentary Rock

The single most characteristic feature of sedimentary rocks is stratification, the arrangement of visible layers.

The oldest layers of sedimentary rock are always on the bottom of a column. The youngest layers are always on the top of a column.

Features of Sedimentary Rock

The single most characteristic feature of sedimentary rocks is stratification, the arrangement of visible layers.

The oldest layers of sedimentary rock are always on the bottom of a column. The youngest layers are always on the top of a column.

Some sedimentary rocks contain ___________________. These could be the remains, impression, or any other evidence of a plant or animal preserved in rock. See Chapter 29 for details.

Features of Sedimentary Rock

The single most characteristic feature of sedimentary rocks is stratification, the arrangement of visible layers.

The oldest layers of sedimentary rock are always on the bottom of a column. The youngest layers are always on the top of a column.

Some sedimentary rocks contain fossils. These could be the remains, impression, or any other evidence of a plant or animal preserved in rock. See Chapter 29 for details.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called _______________ rocks. The _________________ rocks can be igneous, sedimentary, or metamorphic.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by ___________________, ___________________, and __________________ ________________ is called metamorphism.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

There are two basic types of metamorphism: _____________ and _____________.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

There are two basic types of metamorphism: regional and local.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

There are two basic types of metamorphism: regional and local.

_________________ metamorphism can occur during mountain-building events. The intense ___________ and _____________ from overlying and compressing rock causes the chemical composition, texture, and/or internal structure of the rock to change.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

There are two basic types of metamorphism: regional and local.

Regional metamorphism can occur during mountain-building events. The intense heat and pressure from overlying and compressing rock causes the chemical composition, texture, and/or internal structure of the rock to change.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

There are two basic types of metamorphism: regional and local.

Regional metamorphism can occur during mountain-building events. The intense heat and pressure from overlying and compressing rock causes the chemical composition, texture, and/or internal structure of the rock to change.

Metamorphic rocks are ____________ dense than the parent rocks.

Metamorphic Rock Processes

Metamorphic rocks are formed from preexisting rocks called parent rocks. The parent rocks can be igneous, sedimentary, or metamorphic.

A change in a rock’s structure by heat, pressure, and chemical activity is called metamorphism.

There are two basic types of metamorphism: regional and local.

Regional metamorphism can occur during mountain-building events. The intense heat and pressure from overlying and compressing rock causes the chemical composition, texture, and/or internal structure of the rock to change.

Metamorphic rocks are more dense than the parent rocks.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of _____________, _________________, and _________________ ________________.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Two types of local metamorphism are called _____________ and ______________.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Two types of local metamorphism are called contact and deformational.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Two types of local metamorphism are called contact and deformational.

________________ metamorphism occurs when hot magma comes in contact with rock, thereby heating and changing it.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Two types of local metamorphism are called contact and deformational.

Contact metamorphism occurs when hot magma comes in contact with rock, thereby heating and changing it.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Two types of local metamorphism are called contact and deformational.

Contact metamorphism occurs when hot magma comes in contact with rock, thereby heating and changing it.

________________ metamorphism occurs at low temperatures and high pressure caused by stress and friction near earthquake faults. The altered rocks have the same mineral composition, but show changes in structure and texture.

Metamorphic Rock Processes

The degree of metamorphism is determined by the amount of heat, pressure, and chemical activity.

Two types of local metamorphism are called contact and deformational.

Contact metamorphism occurs when hot magma comes in contact with rock, thereby heating and changing it.

Deformational metamorphism occurs at low temperatures and high pressure caused by stress and friction near earthquake faults. The altered rocks have the same mineral composition, but show changes in structure and texture.

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

____________________ is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic rocks are either ________________ or _______ ________________.

______________________ rocks _______ ________________ rocks

Rocks that form alternating bands of minerals or split along parallel layers

Rocks that appear shiny, crystalline, or deformed, but do not have layering.

Common examples are: Common examples are:

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic rocks are either foliated or non-foliated.

______________________ rocks _______ ________________ rocks

Rocks that form alternating bands of minerals or split along parallel layers

Rocks that appear shiny, crystalline, or deformed, but do not have layering.

Common examples are: Common examples are:

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic rocks are either foliated or non-foliated.

Foliated rocks _______ ________________ rocks

Rocks that form alternating bands of minerals or split along parallel layers

Rocks that appear shiny, crystalline, or deformed, but do not have layering.

Common examples are: Common examples are:

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic rocks are either foliated or non-foliated.

Foliated rocks _______ ________________ rocks

Rocks that form alternating bands of minerals or split along parallel layers

Rocks that appear shiny, crystalline, or deformed, but do not have layering.

Common examples are: Slate, Schist, Phyllite, Gneiss

Common examples are:

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic rocks are either foliated or non-foliated.

Foliated rocks Non-foliated rocks

Rocks that form alternating bands of minerals or split along parallel layers

Rocks that appear shiny, crystalline, or deformed, but do not have layering.

Common examples are: Slate, Schist, Phyllite, Gneiss

Common examples are:

Metamorphic Rock Descriptions

The descriptions and identifications of metamorphic rocks are often based on the parent rock, mineral content, and texture.

Foliation is the tendency of a rock to form bands of minerals or split along parallel layers.

Metamorphic rocks are either foliated or non-foliated.

Foliated rocks Non-foliated rocks

Rocks that form alternating bands of minerals or split along parallel layers

Rocks that appear shiny, crystalline, or deformed, but do not have layering.

Common examples are: Slate, Schist, Phyllite, Gneiss

Common examples are: Marble, Quartzite