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Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

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Page 1: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Table of Contents

Chapter 6 Volcanoes

Chapter Preview

6.1 Volcanoes and Plate Tectonics

6.2 Volcanic Eruptions

6.3 Volcanic Landforms

6.4 California Geology

Page 2: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

1. Igneous rocks form when

a. sediment is compacted and cemented.

b. rocks are changed by heat and pressure.

c. sediment is heated and cooled.

d. lava and magma cool and harden.

Chapter 6 Volcanoes

Page 3: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

1. Igneous rocks form when

a. sediment is compacted and cemented.

b. rocks are changed by heat and pressure.

c. sediment is heated and cooled.

d. lava and magma cool and harden.

Chapter 6 Volcanoes

Page 4: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

2. Melted material that erupts from a volcano is called

a. magma.

b. sediment.

c. lava.

d. mica.

Chapter 6 Volcanoes

Page 5: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

2. Melted material that erupts from a volcano is called

a. magma.

b. sediment.

c. lava.

d. mica.

Chapter 6 Volcanoes

Page 6: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

3. Why do volcanoes erupt?

a. They are hot and fiery.

b. They form beneath the ocean floor.

c. Gases in magma expand as it rises to the surface.

d. Lava is a pure liquid.

Chapter 6 Volcanoes

Page 7: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

3. Why do volcanoes erupt?

a. They are hot and fiery.

b. They form beneath the ocean floor.

c. Gases in magma expand as it rises to the surface.

d. Lava is a pure liquid.

Chapter 6 Volcanoes

Page 8: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

4. Which of these does NOT rapidly change Earth’s

land surface?

a. earthquakes

b. mountain building

c. landslides

d. volcanic eruptions

Chapter 6 Volcanoes

Page 9: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Chapter Preview Questions

4. Which of these does NOT rapidly change Earth’s

land surface?

a. earthquakes

b. mountain building

c. landslides

d. volcanic eruptions

Chapter 6 Volcanoes

Page 10: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

You know that if you want to open a bottle of soda, you must do so carefully. Otherwise, the soda might spray out of the bottle as soon as you loosen the cap. What causes the soda to rush out with such force? How is this similar to what happens when a volcano erupts? Explain.

What causes volcanoes, and how do they change

Earth’s surface?

Chapter 6 Volcanoes

Page 11: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Use Clues to Determine Meaning

Chapter 6 Volcanoes

Some volcanoes result from hot spots in Earthís mantle. A hot spot is an area where material from within the mantle rises and then melts. A volcano forms above a hot spot when the hot material erupts through the crust and reaches the surface.A hot spot in the ocean oor can gradually form a series of volcanic mountains. For example, the Hawaiian Islands formed one by one over millions of years as the Pacific plate drifted over a hot spot.

Example

Unfamiliar wordsHot spot isthe subject ofthe sentence.

Definition,follows boldface

Explanation

Page 12: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Apply It!

Review the clues to the meaning of hot spot. Then complete the following.

1. What clue tells you that hot spot might be followed by a definition?

The term is in boldface and is the subject of the sentence.

2. What example helps you understand hot spots?

The Hawaiian Islands formed one by one over millions of years as thePacific plate drifted over a hot spot

Chapter 6 Volcanoes

Page 13: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

End of Chapter Preview

Chapter 6 Volcanoes

Page 14: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Describe what happens along a fault beneath Earth’s surface when an earthquake occurs?

Page 15: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

How do volcanoes change the land?

Page 16: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Volcanoes

Page 17: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Section 1:Volcanoes and Plate

TectonicsWhere are most of Earth’s volcanoes found?

How do hot spot volcanoes form?

Chapter 6 Volcanoes

Page 18: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

A volcanovolcano is a weak spot in the crust where molten material, or magma, comes to the surface.

Page 19: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

MagmaMagma is molten material that has not reached the surface and is still underground.

Page 20: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

LavaLava is molten material, or magma, that has reached the surface.

Page 21: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Ring of FireRing of Fire is a major volcanic belt that rims or circles the Pacific Ocean.

Page 22: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Island ArcIsland Arc is a string of islands formed by weak spots or hot spotshot spots in the crust where magma burns through.

Page 23: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Volcanoes and Plate Boundaries

Volcanic belts form along the boundaries of Earth’s plates.

Chapter 6 Volcanoes

Page 24: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Volcanoes and Plate BoundariesVolcanoes often form where two oceanic plates collide or where an oceanic plate collides with a continental plate. In both situations, an oceanic plate sinks through a trench. Rock above the plate melts to form magma, which then erupts to the surface as lava.

Chapter 6 Volcanoes

Page 25: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Hot Spot Volcanoes

A volcano forms above a hot spot when magma erupts through the crust and reaches the surface.

Chapter 6 Volcanoes

Page 26: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

More on Volcanoes

Click the PHSchool.com button for an activityabout volcanoes.

Chapter 6 Volcanoes

Page 27: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

End of Section:Volcanoes and Plate Tectonics

Chapter 6 Volcanoes

Page 28: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

What causes volcanoes to form at a spreading boundary?

Page 29: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Where are most of Earth’s volcanoes found? Explain.

Page 30: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Describe the order of parts through which magma travels

as it moves to the surface.

Page 31: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Which is more likely to be dangerous – a volcano that

erupts frequently or a volcano that has been inactive for a

hundred years? Why?

Page 32: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Section 2:Volcanic Eruptions

What happens when a volcano erupts?

What are the two types of volcanic eruptions?

What are a volcano’s stages of activity?

Chapter 6 Volcanoes

Page 33: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Volcanic Eruptions

Page 34: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Reaches Earth’s Surface

When a volcano erupts, the force of the expanding gases pushes magma from the magma chambermagma chamber through the pipepipe until it flows or explodes out of the ventvent.

Chapter 6 Volcanoes

Page 35: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

Magma chamberMagma chamber is a pocket beneath a volcano where magma is collected or stored.

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Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

PipePipe is a long tube inside a volcano that connects the magma chamber to the Earth’s surface.

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Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

VentVent is an opening through which molten rock and gas leave the volcano.

Page 38: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

Lava flowLava flow is the area covered by lava as it pours out of a vent.

Page 39: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

CraterCrater is a bowl-shaped area that may form at the top of a volcano.

Page 40: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

PahoehoePahoehoe is a very thin, fast moving lava. Pahoehoe contains low amounts of silica, which gives it it’s thinness. When Pahoehoe hardens, it forms wrinkle and rope-like rock formations. Pahoehoe is hotter than Aa.

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Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

AaAa is a very thick, slow moving lava. Aa contains high amounts of silica, which gives it it’s thickness. When aa hardens, it forms a rough surface consisting of jagged (sharp) lava chunks.

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Magma Reaches Earth’s Surface

Chapter 6 Volcanoes

Pyroclastic flowPyroclastic flow is an explosive eruption that includes hot gases, cinders (volcanic ash), and bombs (volcanic rocks).

Page 43: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Composite Volcano Eruption Activity

Click the Active Art button to open a browser window and access Active Art about composite volcano eruption.

Chapter 6 Volcanoes

Page 44: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Composition

Magma varies in composition and is classified according to the amount of silica it contains. The graphs show the average composition of the two types of magma. Use the graphs to answer the questions.

Chapter 6 Volcanoes

Page 45: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Composition

Silica, other oxides, and other solids.

Reading Graphs:

Study both graphs. What materials make up both types of magma?

Chapter 6 Volcanoes

Page 46: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Composition

Rhyolite-forming magma; about 70 percent.

Reading Graphs:

Which type of magma has more silica? About how much silica does this type of magma contain?

Chapter 6 Volcanoes

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Magma Composition

About 60 percent

Estimating:

A third type of magma has a silica content that is halfway between that of the other two types. About how much silica does this type of magma contain?

Chapter 6 Volcanoes

Page 48: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Magma Composition

Rhyolite-forming magma would have higher viscosity because it is higher in silica.

Predicting:

What type of magma would have a higher viscosity? Explain.

Chapter 6 Volcanoes

Page 49: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Kinds of Volcanic Eruptions

Within the last 150 years, major volcanic eruptions have greatly affected the land and people around them.

Chapter 6 Volcanoes

Page 50: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Deadly Eruptions

Page 51: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Stages of Volcanic Activity

Chapter 6 Volcanoes

ActiveActive volcanoes are considered “live” meaning that it is erupting, or has shown signs that it may erupt in the near future

Lassen PeakLassen PeakMount ShastaMount Shasta

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Stages of Volcanic Activity

Chapter 6 Volcanoes

DormantDormant volcanoes are considered “asleep” or “sleeping bears” meaning that they may become active in the future

Long Valley Long Valley CratersCraters

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Stages of Volcanic Activity

Chapter 6 Volcanoes

ExtinctExtinct volcanoes are considered “dead” meaning that it is unlikely that they will erupt again

AucklandAuckland

St. LuciaSt. Lucia

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End of Section:Volcanic Eruptions

Chapter 6 Volcanoes

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Section 3: Volcanic Landforms

What landforms do lava and ash create?

How does magma that hardens beneath the surface create landforms?

Chapter 6 Volcanoes

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Types of Volcanoes

Page 57: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Landforms From Lava and Ash

Volcanic eruptions create landforms made of lava, ash, and other materials. These landforms include composite composite volcanoesvolcanoes, shield volcanoesshield volcanoes, cinder cone volcanoescinder cone volcanoes, and lava plateauslava plateaus.

Chapter 6 Volcanoes

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Landforms From Lava and Ash

Composite VolcanoesComposite Volcanoes have quiet eruptions that alternate with explosive eruptions, forming layers of lava and ash.

Chapter 6 Volcanoes

Mayon, PhilippinesCotopaxi, Ecuador

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Landforms From Lava and Ash

Shield VolcanoesShield Volcanoes have quiet eruptions and have gentle slopes, which are not steep.

Chapter 6 Volcanoes

Mauna Loa, Hawaii Erta Ale, Ethiopia

Page 60: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Landforms From Lava and Ash

Cinder Cone VolcanoesCinder Cone Volcanoes have explosive eruptions of ash, cinders, and bombs that form a cone-shaped hill.

Chapter 6 Volcanoes

Mount Etna, ItalySP Crater, Arizona

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Landforms From Lava and Ash

Lava PlateausLava Plateaus are formed from runny lava (pahoehoe) that cools in flat sheets of rock. Over time these layers form high plateaus.

Chapter 6 Volcanoes

Steamboat Rock, Washington Hawaii

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Landforms From Lava and Ash

CalderasCalderas are formed when a magma chamber is emptied after an eruption and the volcano mountain collapses into the empty space creating a crater.

Chapter 6 Volcanoes

Aniakchak, Alaska Crater Lake, Oregon

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Landforms From Lava and Ash

A calderacaldera forms when an volcano’s magma chamber empties and the roof of the chamber collapses. The result is a large, bowl-shaped calderacaldera.

Chapter 6 Volcanoes

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Landforms From Magma

Features formed by magma include volcanic necksvolcanic necks, dikesdikes, and sillssills, as well as batholithsbatholiths and dome mountainsdome mountains.

Chapter 6 Volcanoes

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Landforms From Magma

BatholithsBatholiths

Chapter 6 Volcanoes

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Landforms From Magma

Volcanic NecksVolcanic Necks

Chapter 6 Volcanoes

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Landforms From Magma

DikesDikes

Chapter 6 Volcanoes

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Landforms From Magma

SillsSills

Chapter 6 Volcanoes

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Batholiths

A batholithbatholith is a mass of rock formed when a large body of magma cools inside the crust. Several large batholithsbatholiths form the core of mountain ranges in western North America. Half Dome in Yosemite National Park, California, is part of the Sierra Nevada batholithbatholith.

Chapter 6 Volcanoes

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Links on Volcanic Effects

Click the SciLinks button for links on volcanic effects.

Chapter 6 Volcanoes

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End of Section:Volcanic Landforms

Chapter 6 Volcanoes

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Section 4:California Geology

How does plate tectonics help to explain features of California’s geology?

Chapter 6 Volcanoes

Page 73: Table of Contents Chapter 6 Volcanoes Chapter Preview 6.1 Volcanoes and Plate Tectonics 6.2 Volcanic Eruptions 6.3 Volcanic Landforms 6.4 California Geology

Plate Tectonics and California

The movements of three plates have shaped the geologic features of California over millions of years.

Chapter 6 Volcanoes

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Plate Tectonics and California

Many geologic processes worked together to form California’s landscape

of volcanoes, faults, mountain ranges, and basins.

Chapter 6 Volcanoes

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End of Section: California Geology

Chapter 6 Volcanoes

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Chapter 6 Volcanoes

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QuickTake Quiz

Click to start quiz.

Chapter 6 Volcanoes